Desarrollos metodológicos y aplicaciones hacia el cálculo de la peligrosidad sísmica en el ecuador continental y estudio de riesgo sísmico en la ciudad de Quito

En el presente trabajo de tesis se desarrolla, en primer lugar, un estudio de peligrosidad sísmica en Ecuador continental, siguiendo una metodología probabilista zonificada. El estudio se plantea a escala regional y presenta como principales aportaciones: 1) la elaboración de un Estado del Arte sobre Tectónica y Geología de Ecuador, concluyendo con la identificación de las principales fuentes sísmicas; 2) La confección de un Catálogo Sísmico de proyecto, recopilando información de distintas agencias, que ha sido homogeneizado a magnitud momento, Mw, depurado de réplicas y premonitores y corregido por la falta de completitud para la estimación de tasas en diferentes rangos de magnitud; 3) la propuesta de un nueva zonificación sísmica, definiendo las zonas sismogenéticas en tres regímenes tectónicos: cortical, subducción interfase y subducción in-slab; 4) la caracterización sísmica de cada zona estimando los parámetros de recurrencia y Magnitud Máxima (Mmax), considerando para este último parámetro una distribución de valores posibles en función de la sismicidad y tectónica, tras un exhaustivo análisis de los datos existentes; 5) la generación de mapas de peligrosidad sísmica de Ecuador continental en términos de aceleración pico (PGA) y espectral SA (T= 1s) , en ambos casos para periodos de retorno (PR) de 475, 975 y 2475 años; 6) La estimación de espectros de peligrosidad uniforme (UHS) y sismos de control mediante desagregación de la peligrosidad, para PR de 475 y 2475 años en 4 capitales de provincia: Quito, Esmeraldas, Guayaquil y Loja. Una segunda parte del trabajo se destina al cálculo del riesgo sísmico en el Barrio Mariscal Sucre de Quito, lo que supone incidir ya a una escala municipal. Como principales contribuciones de este trabajo se destacan: 1) definición del escenario sísmico que más contribuye a la peligrosidad en Quito, que actuará como input de cálculo del riesgo; 2) caracterización de la acción sísmica asociada a ese escenario, incluyendo resultados de microzonación y efecto local en la zona de estudio; 3) Elaboración de una Base de Datos partiendo de información catastral e identificación de las tipologías dominantes; 4) Asignación de clases de vulnerabilidad y obtención de porcentajes de daño esperado en cada clase ante la acción sísmica definida previamente, con la consiguiente representación de mapas de vulnerabilidad y daño; 5) mapas de indicadores globales del riesgo sísmico; 6) Base de datos georreferenciada con toda la información generada en el estudio. Cabe destacar que el trabajo, aunque no formula nuevos métodos, si plantea una metodología integral de cálculo del riesgo sísmico, incorporando avances en cada fase abordada, desde la estimación de la peligrosidad o la definición de escenarios sísmicos con carácter hibrido (probabilista-determinista), hasta la asignación de vulnerabilidades y estimación de escenarios de daño. Esta tesis trata de presentar contribuciones hacia el mejor conocimiento de la peligrosidad sísmica en Ecuador y el riesgo sísmico en Quito, siendo uno de los primeros estudios de tesis que se desarrolla sobre estos temas en el país. El trabajo puede servir de ejemplo y punto de partida para estudios futuros; además de ser replicable en otras ciudades y municipios de Ecuador. -------------------- ABSTRACT: ------------------ This thesis first develops a study of seismic hazard in mainland Ecuador, following a zoned, probabilistic methodology. The study considers a regional scale and presents as main contributions: 1) The development of a State of Art on the Tectonics and Geology of Ecuador, concluding with the identification of the main seismic sources; 2) The creation of a Seismic Catalog project, collecting information from different agencies, which has been homogenized to Moment magnitude, Mw, purged from aftershocks and premonitories and corrected for the lack of completeness to estimate rates in different maggnitude ranges; 3) The proposal of a new seismic zoning, defining the seismogenic zones in three tectonic regimes: cortical, subduction interface and subduction in-slab; 4) The seismic characterization of each zone, estimating the parameters of recurrence and Maximum Magnitude (Mmax), considering the latter as a distribution of possible values, depending on the seismicity and tectonics, and after a thorough analysis of the existing data; 5) Seismic hazard maps of continental Ecuador in terms of peak ground acceleration (PGA) and spectral SA(T=1), and return periods (PR) of 475, 975 and 2475 years; 6) Uniform hazard spectra (UHS) and control earthquakes obtained by hazard disaggregation, for PR 475 and 2475 years in four provincial capitals: Quito, Esmeraldas, Guayaquil and Loja. The second section focuses on the calculation of seismic risk in the Quito Mariscal Sucre parish, which is already supposed to be influencing at a municipal level. The main contributions here are the: 1) Definition of the seismic scenario that contributes most to the hazard in Quito, which acts as an input in the risk calculation; 2) Characterization of the seismic action associated with that scenario, including results of micro-zoning and local effect in the study area; 3) Development of a database, based on cadastral data and identification of key typologies; 4) Allocation of vulnerability classes and obtaining percentages of damage expected in each class faced with the seismic action previously defined, with the consequent representation of maps of vulnerability and damage; 5) Global maps of seismic risk indicators; 6) Geo-referenced database with all the information generated in the study. It should be noted that although new methods are not prescribed, this study does set a comprehensive methodology for the calculation of seismic risk, incorporating advances in each phase approached, from the hazard estimation, or definition of seismic scenarios applying a hybrid (deterministic-probabilistic) method, to the allocation of vulnerabilities and estimation of damage scenarios. This thesis aims to present contributions leading to a better understanding of seismic hazard in Ecuador and seismic risk in Quito, and is one of the first studies in the country to develop such themes. This study can serve as an example and starting point for future studies, which could replicate this methodology in other cities and municipalities.

Materialidad poética: arquitectura suiza en el entorno de los Grisones 1992-2004

El entorno alpino de los Grisones ha sido un laboratorio donde experimentar un método arquitectónico procedente de diversas fuentes durante los años 70 en la ETHZ. Este método ha producido durante las últimas tres décadas un discurso teórico propiamente suizo alemán. La tradición continúa siendo un valor cultural para la comunidad alpina de los Grisones, que apuesta por seguir relacionando la arquitectura con su historia y su paisaje. La especificidad de cada entorno suizo alemán es un hecho obvio pero, por encima de sus rasgos característicos, hay un denominador común que les da unidad en silencio: se trata de una idea de la construcción. El fenómeno de los Grisones es territorial en su localización concreta, pero comparte el trasfondo teórico del resto de la arquitectura suizo alemana reciente. La tesis recorre transversalmente las condiciones que han dado lugar a esa trayectoria común hasta la actualidad, en que la arquitectura suizo alemana se halla precisamente en un momento de cambio generacional. La obra de Peter Märkli constituye en esta tesis un paradigma de la voluntad suizo alemana por formar parte de la continuidad cultural de la arquitectura, como una actitud de resistencia compartida frente al mundo globalizado. La tesis se articula a partir de ocho proyectos recientes, realizados por arquitectos suizo alemanes en el entorno del territorio alpino de los Grisones. Estos proyectos condensan la trayectoria arquitectónica suizo alemana durante el siglo XX, así como el fenómeno arquitectónico que ha tenido lugar en el entorno de los Grisones durante las últimas tres décadas. La tesis analiza a través de cada pareja de proyectos los episodios teóricos, artísticos y filosóficos más relevantes que se sintetizan en estas obras, así como sus referentes arquitectónicos y la dimensión trascendente de los materiales en los que la cultura suiza hunde sus raíces: la madera, la piedra y el hormigón. Las vanguardias pictóricas, el Movimiento Moderno y las corrientes humanistas y regionalistas que se fueron sucediendo durante el pasado siglo, configuran el escenario en el que tomó cuerpo la sensibilidad arquitectónica suizo alemana reciente, que emerge a través de la compleja red de relaciones establecidas entre el panorama suizo y el internacional. El mismo bagaje teórico subyace al territorio suizo alemán a nivel general, por lo que asociarlo a través de esta tesis a proyectos realizados en un entorno característico, permite acceder a una realización concreta de ese debate en un entorno tan particular como son los Grisones. La aproximación a los proyectos es de carácter fenomenológico: la experiencia directa de los mismos ha sido el sustrato fundamental del enfoque de la tesis. El trabajo de campo no se limitó a visitar los proyectos que vertebran la tesis, sino que trató de abarcar las obras más relevantes de la producción suizo alemana reciente en los Grisones, con el fin de adquirir cierto grado de sensibilidad perceptiva hacia la singularidad de su identidad territorial. La tesis hace especial hincapié en las obras de Peter Märkli y Peter Zumthor, representantes de los dos extremos del discurso suizo alemán reciente, respecto a la materialidad y al carácter de la secuencia espacial, sistemático o fluido respectivamente, pero que asimismo comparten el clasicismo formalista que subyace al fenómeno suizo alemán. Los dos proyectos que establecen el periodo 1992-2004 explorado por esta investigación constituyen dos hitos fundamentales. El Museo de La Congiunta en Giornico de Peter Märkli se construyó en 1992 y se erige a partir de entonces como un icono arquitectónico de la condensación típicamente suizo alemana de base reductiva. Este paradigma de síntesis conceptual y constructiva comenzó a forjarse en la década de 1930 de la mano del Konkrete Kunst formulado por Max Bill, que es la única manifestación artística genuinamente suiza del siglo XX y que desarrolló pictóricamente los valores de precisión, rigor, racionalismo y abstracción afines a la sensibilidad suizo alemana. En segundo lugar, el proyecto para la rehabilitación de la Villa Garbald y la construcción de la Torre Roccolo en Castasegna llevado a cabo por Miller & Maranta en 2004, supuso la consumación de la Analoge Architektur, que fue la primera corriente arquitectónica propiamente suiza, desarrollada durante la década de 1980 por Miroslav Sik. La Deutscher Tendenza es un periodo de la trayectoria suizo alemana reciente poco conocido, representado por una figura tan relevante como es Peter Zumthor. Las obras que proyectó Zumthor entre 1979 y 1985 forman parte de un periodo en que el arquitecto se encontraba profundamente influido por el neorracionalismo italiano, como ilustra la escuela de Churwalden de 1983. La arquitectura suizo alemana reciente exploró sistemáticamente los sistemas compositivos de las vanguardias pictóricas y del Movimiento Moderno, por encima de su formalismo concreto. La segunda fase de la obra de Zumthor entre 1985 y 1996 se caracteriza por la transfiguración del plano libre del sistema compositivo neoplasticista desarrollado por De Stijl, plano que adquirió grosor hasta convertirse en la caja articuladora de la fluidez de la secuencia espacial. El formalismo de Zumthor en esta fase implica la prioridad del esquema compositivo, compuesto por un perímetro regular en el que se reúnen las cajas que, como las superficies de color de las composiciones de Mondrian, articulan el espacio a su alrededor. La Residencia de Masans de Zumthor de 1993 es un proyecto canónico de este sistema compositivo, que culmina en el esquema radial de las Termas de Vals de 1996. La imagen poética se convirtió en el lenguaje propio del pensamiento de la arquitectura suizo alemana, que permitía una reflexión no verbal, a partir de unos pocos arquetipos fundamentales. Los arquitectos del Ticino buscaron en la Tendenza italiana durante la década de 1970 una alternativa al insostenible modelo territorial que estaba destruyendo su paisaje cultural. Algunos de estos arquitectos comenzaron a dar clase durante esa década en la ETHZ, por lo que transmitieron sus inquietudes al alumnado e introdujeron a Aldo Rossi en la facultad, que era uno de los máximos representantes de la Tendenza. El método analógico de Rossi, basado en la psicología analítica de Carl Jung, fue una influencia fundamental en la ETHZ durante los años 70. Rossi partía de una teoría afín al colectivo intelectual suizo que los arquitectos de la ETHZ pronto comprendieron que debían independizar del contexto italiano, desarrollando su propio método a partir de 1985 con la Analoge Architektur. El valor de la preexistencia de acuerdo a este método incipiente se hallaba en su papel articulador de la continuidad cultural de una comunidad, que Miroslav Sik definió a partir de su concepto de Altneue (literalmente, lo Nuevo-Viejo). La fusión entre lo nuevo y lo viejo era la base de la espontaneidad con la que habían crecido los asentamientos históricamente. Sik consideraba que la continuidad dependía de la comprensión de los patrones preexistentes, con el objeto de mantener su vigencia mediante la incorporación de estrategias contemporáneas, que renovarían su significado sin perder su esencia. La Casa Gugalun en Versam de Zumthor de 1994 supone una aproximación a escala doméstica a este planteamiento. La arquitectura suizo alemana reciente a menudo busca en sus referentes plásticos una manera de explorar ámbitos poco accesibles para la disciplina arquitectónica. El pensamiento arquitectónico basado en la imagen poética se implementa a partir de la tectónica de la construcción, que es el medio para comunicar una idea vertebradora del proyecto de principio a fin. La construcción como medio introduce el concepto clave de la apariencia de la arquitectura, estrechamente relacionado con la filosofía idealista de Friedrich Schiller. La apariencia debe expresar el sentido conceptual de la obra, que los arquitectos suizo alemanes denominan idea, por lo que la construcción no tiene un valor por sí misma, sino en cuanto a la apariencia. La Capilla de Oberrealta de Christian Kerez de 1993 puede ser considerada una obra escultórica en el paisaje, más próxima a las artes plásticas que a la arquitectura. La tensión que surge entre la figura ideal y la pieza sometida a una sutil deformación confiere un carácter dinámico a la composición, que intensifica el efecto perceptivo, de acuerdo a la teoría del pensamiento visual de Rudolph Arnheim. La deformación al servicio de la psicología de la percepción es un fenómeno que caracteriza la arquitectura suizo alemana reciente. El concepto de Forme Forte (forma fuerte) fue introducido por Martin Steinmann para caracterizar el objeto arquitectónico denominado internacionalmente Swiss Box. Este concepto se caracteriza por una predilección por lo monolítico, lo unitario y lo arquetípico. La condición más sustancial de una Forme Forte es, sin embargo, la de configurar un elemento estructurador del entorno. Tanto la base morfológica de una Forme Forte, como su capacidad para estructurar el lugar, se corresponden con los conceptos de arquetipo y monumento de la teoría de Rossi. La tesis explora el sentido de la deformación en la producción suizo alemana reciente, a partir de la Escuela de Paspels de Valerio Olgiati de 1998 y la Torre Roccolo de Villa Garbald de Miller&Maranta de 1998. La teoría tectónica de Gottfried Semper y la razón de la forma de Adolf Loos constituyen el sustrato teórico, que relaciona la actividad existencial de habitar con la materialidad de la arquitectura suizo alemana reciente. La teoría tectónica de Semper fundamenta las revisiones posteriores de los sistemas constructivos tradicionales suizo alemanes. Esta influencia sirvió como base a la vanguardia suiza de la Neues Bauen, que desarrolló un racionalismo funcionalista durante las décadas de 1920 y 1930, que constituye una gramática de base no simbólica. Esta gramática constituye el fundamento de la transición del orden clásico a la materialidad como instrumento compositivo durante la segunda mitad del siglo XX, consolidando el concepto de la base material de la forma. La revisión de la tradición regionalista y racionalista llevada a cabo por la generación de arquitectos suizo alemanes de la década de 1950 y 1960, constituyó una investigación lingüística sustancial. Rudolph Olgiati es la figura determinante de este periodo. La revisión de esta investigación se codificó en clave estructuralista durante los años 70 en la ETHZ, influenciada por la presencia de Roland Barthes como profesor invitado. Esta revisión constituyó la base de la articulación tectónica propiamente suizo alemana todavía vigente, como ilustra expresamente la obra de Burkhalter&Sumi en esta tesis. La obra de Gion Caminada en Vrin entre 1995 y 2002 aporta una intensa investigación sobre el Strickbau, que implementa una y otra vez variaciones sobre un sistema tradicional, ilustrando las infinitas posibilidades que ofrece un lenguaje, paradójicamente limitado por los medios disponibles en un entorno alpino aislado. Para terminar Jürg Conzett es el ingeniero con el que han desarrollado sus proyectos la mayoría de los arquitectos en el entorno de los Grisones, formado durante 8 años con Zumthor y colaborador habitual de Caminada entre otros. Conzett es el referente que relaciona la ingeniería con la arquitectura en el ámbito de esta tesis, imprescindible en el contexto de esta investigación. ABSTRACT The Alpine setting of Grisons has been a laboratory for architectural experimentation with an approach forged in the 1970s from various sources in the Swiss Federal Institute of Technology in Zurich (ETHZ). This method has produced a uniquely German-Swiss theoretical discourse over the past three decades. Tradition continues to be a cultural value for Grisons, a region committed to continue linking its architecture with the region’s history and landscape. The specificity of the German-Swiss environment is obvious, but beyond its characteristic features, there is a common denominator that gives these settings a silent unity: it is an idea of building. The phenomenon of Grisons is geographic in its specific location, but it shares the theoretical basis of the rest of the new German-Swiss architecture. This thesis transversely delves into the conditions that have shaped this common path up to the present, just as German-Swiss architecture is going through a time of generational change. In this thesis, Märkli Peter's work constitutes a paradigm of the German-Swiss will to uphold the cultural and architectural continuity of the region, exemplifying an attitude of shared resistance to the globalized world. The thesis is structured around eight recent projects carried out by German-Swiss architects in the Alpine region of Grisons. These projects represent the trajectory of twentieth century German-Swiss architectural history, as well as the architectural phenomenon that has taken place in the environs of Grisons over the past three decades. Through these projects the thesis analyzes the most relevant theoretical, artistic and philosophical references that are synthesized in the works, as well as their architectural references and the transcendental dimension of the materials in which Swiss culture is rooted: wood, stone and concrete. The artistic avant-garde, together with Modernism and the humanistic and regional movements that occurred during the last century, set the stage for present-day German-Swiss architectural sensitivity, which emerges from a complex web of relationships established between the Swiss and international panorama. This same theoretical background and experience underlies all of the German-Swiss territory in general, so associating it through this thesis to a particular context allows the description of a specific embodiment of this debate, within the unique environment of Grisons. The methodological approach to analyzing the projects was phenomenological: direct experience is the main substrate underpinning the focus of the thesis. Field work was not limited to visiting the projects featured in the thesis, but rather encompassed the most important works of recent German-Swiss construction in the Grisons in order to gain some degree of perceptual sensitivity to the uniqueness of its territorial identity. The present paper puts special emphasis on the works of Peter Märkli and Peter Zumthor, who share the formal classicist perspective of the German-Swiss context but stand on opposite sides of the philosophical spectrum with regard to the notion of materiality and the nature of space, which they conceive as systematic or fluid, respectively. The two projects that establish the boundaries of the time period 1992–2004 explored by this research represent two key milestones. The Museum La Congiunta in Giornico, by Peter Märkli, was built in 1992 and quickly established itself as an architectural icon of German-Swiss reductionism. This paradigm of conceptual and constructive synthesis began to take shape in the 1930s under the banner of Konkrete Kunst (Concrete Art), led by Max Bill. The only genuinely Swiss artistic movement of the twentieth century, Konkrete Kunst was characterized by the artistic values of precision, rigor, rationalism and abstraction, sentiments that were very close to the German-Swiss tradition. Secondly, the project for the rehabilitation of Villa Garbald and the construction of the Roccolo Tower in Castasegna, conducted by Miller&Maranta in 2004, represented the consummation of the Analoge Architektur, which was the first truly Swiss architectural movement, spearheaded in the 1980s by Miroslav Sik. The Deutscher Tendenza is a little-known period of recent German-Swiss history, represented by the important figure of Peter Zumthor. The projects that Zumthor led between 1979 and 1985 are part of a period when Italian Neo-Rationalism exercised a profound influence on the architect, as illustrated by the Churwalden School, circa 1983. Recent German-Swiss architecture systematically explored the compositional systems of the artistic avant-garde and Modernism, beyond its specific formal aspects. The second phase of Zumthor's work, between 1985 and 1996, is characterized by the transfiguration of the free plane, neoplastic compositional system developed by De Stijl, a plane that thickened until it became the box articulating fluidity from the spatial sequence. Zumthor's formalism in this phase prioritizes the compositional scheme, consisting of a regular perimeter in which the boxes that -like Mondrian’s colored surfaces- arrange the space around it. Zumthor’s Masans Residence, circa 1993, is a canonical project of this compositional system, which culminates in the radial pattern of the Therme Vals, circa 1996. The poetic image became the appropriate language of thought for German-Swiss architecture, which invited a nonverbal reflection inspired by a few fundamental archetypes. The architects of Ticino sought, through the Italian Tendenza of the 1970s, an alternative to the unsustainable territorial model that was destroying their cultural landscape. Some of these architects began to teach during that decade at ETHZ, and naturally they transmitted their unease to their students. These architects also introduced Aldo Rossi, one of the leading representatives of the Tendenza, to the school. Rossi’s analogue method, based on the analytical psychology of Carl Jung, was a major influence on the ETHZ during the 1970s. Rossi’s theoretical grounding was very much in tune with Swiss intellectualism, and it did not take long for architects from ETHZ to realize that they should break away from the Italian context, developing their own method from 1985 on with the Analoge Architektur. The value of the pre-existing conformity of this emerging method, stemmed from its role in facilitating the cultural continuity of a community, which Miroslav Sik defined in his concept of Altneue (literally, Old-new). This fusion of old and new was the basis for the spontaneity with which settlements had historically grown. Sik considered that continuity depended on understanding the existing patterns and sustaining their relevance through the incorporation of contemporary strategies, which would renew their meaning without losing their essence. Zumthor’s Gugalun House in Versam, circa 1994, is a domestic-scale approach to this philosophy. Modern German-Swiss architecture often looks to its references in visual art for a way to explore areas that are normally inaccessible to the architectural discipline. Architectural thinking based on the poetic image is achieved through a building’s tectonics, which communicate the core idea of a project from start to finish. The understanding of construction as a medium introduces the key concept of the appearance in architecture, closely related to the idealistic philosophy of Friedrich Schiller. The appearance should express the conceptual meaning of the work, which German-Swiss architects call the idea, so that the building does not have value in and of itself, but only in terms of its appearance. The Oberrealta Chapel by Christian Kerez, circa 1993, can be considered a sculpture in the landscape, closer to the visual arts than to architecture. The tension that arises between the ideal figure and the piece subjected to a subtle deformation confers a dynamic character onto the composition, intensifying the perceptual effect, according to Rudolf Arnheim’s theory of visual thought. The deformation in the service of the psychology of perception is a phenomenon that characterizes recent German-Swiss architecture. Martin Steinmann introduced the Forme Forte (Strong Form) concept to describe the architectural object known internationally as the Swiss Box. This concept is characterized by a predilection for all things monolithic, unitary and archetypal. The most substantial condition of a Forme Forte, however, is the configuration of a structuring element in the environment. Both the morphological basis of a Forme Forte and its ability to frame the place, correspond to the concepts of archetype and monument put forward by Rossi’s theory. The present thesis explores the sense of deformation in recent German-Swiss production, based on the School of Paspels by Valerio Olgiati, circa 1998 and the Roccolo Tower in Villa Garbald, by Miller&Maranta, circa 1998. Gottfried Semper’s tectonic theory and Adolf Loos’s reason for form constitute the theoretical foundation that links the existential activity of dwelling to the materiality of recent German-Swiss architecture. Semper’s tectonic theory laid the foundation for subsequent revisions of the German-Swiss traditional building systems. This influence was the basis for the Swiss avant-garde of Neues Bauen, which developed a functional rationalism during the 1920s and 30s that served as a non-symbolic grammatical foundation for the transition from classical order to materiality as a compositional tool. During the second half of the twentieth century, this architectural grammar helped consolidate the concept of the material base of the form. The revision of the regionalist and rationalist tradition, carried out by the generation of German-Swiss architects of the 1950s and 60s, constituted a substantial linguistic investigation. Rudolph Olgiati is the key figure of this period. The research was codified in terms of structuralism in the 1970s in ETHZ and influenced by the presence of Roland Barthes as a visiting professor. This revision was the basis of the uniquely German-Swiss tectonic design still in use today, as specifically illustrated by the work of Burkhalter & Sumi in this thesis. Gion Caminada's work in Vrin between 1995 and 2002 offers an extensive study on the Strickbau, which implements variations on a traditional system again and again, illustrating the endless possibilities of a language that paradoxically seems limited by the available resources in a remote Alpine setting. Finally, Jürg Conzett is the engineer with whom most architects in the Grisons region have developed their projects. Trained under Zumthor for 8 years, and a regular collaborator of Caminada, among others, Conzett is the reference point linking engineering with architecture in this thesis, essential in the context of this research.

Amino acid epimerization dating of coastal neotectonic processes in southeastern Iberian Peninsula: the region between Aguas and Antas river mouths

The coastal area between the mouths of the Aguas and Antas Rivers presents a deformed system of raised marine deposits, some of which have been strongly affected by active tectonics. The use of amino acid epimerization dating of Glycymeris shells from raised coastal deposits allowed determining the age of these marine deposits, all of them linked to highstand sea levels in the Mediterranean realm, with ages between MIS 11 and MIS 1. These results allowed corroborating the age of some previously studied sites, and using new sampling sites, the general aminostratigraphy for the Quaternary raised marine deposits on the Mediterranean coast was confirmed. The main deformation event took place after MIS 11 and continued until MIS 5, and was linked to the activity of the Palomares Faul

Active materiality : the agency of matter from the phenomenological perspective = Materialidad activa : la operatividad de la materia desde el punto de vista fenomenológico

The role of matter has remained central to the making and the thinking of architecture, yet many attempts to capture its essence have been trapped in a dialectic tension between form and materiality, between material consistency and immaterial modes of perception, between static states and dynamic processes, between the real and the virtual, thus advancing an increasing awareness of the perplexing complexity of the material world. Within that complexity, the notion of agency – emerging from and within ecological, politico-economic and socio-cultural processes – calls for a reconceptualization of matter, and consequently processes of materialisation, offering a new understanding of context and space, approached as a field of dynamic relationships. In this context, cutting across boundaries between architectural discourse and practice as well as across the vast trans-disciplinary territory, this dissertation aims to illustrate a variety of design methodologies that have derived from the relational approach. More specifically, the intention is to offer new insights into spatial epistemologies embedded within the notion of atmosphere – commonly associated with the so-called New Phenomenology – and to reflect upon its implications for architectural production. In what follows, the intended argumentation has a twofold dimension. First, through a scrutiny of the notion of atmosphere, the aim is to explore ways of thinking and shaping reality through relations, thus acknowledging the aforementioned complexity of the material universe disclosed through human and non-human as well as material and immaterial forces. Secondly, despite the fact that concerns for atmospherics have flourished over the last few decades, the objective is to reveal that the conceptual foundations and procedures for the production of atmosphere might be found beneath the surface of contemporary debates. Hence, in order to unfold and illustrate previously advocated assumptions, an archaeological approach is adopted, tracing a particular projective genealogy, one that builds upon an atmospheric awareness. Accordingly, in tracing such an atmospheric awareness the study explores the notoriously ambiguous nature and the twofold dimension of atmosphere – meteorological and aesthetic – and the heterogeneity of meanings embedded in them. In this context, the notion of atmosphere is presented as parallactic. It transgresses the formal and material boundaries of bodies. It calls for a reevaluation of perceptual experience, opening a new gap that exposes the orthodox space-bodyenvironment relationships to questioning. It offers to architecture an expanded domain in which to manifest itself, defining architectural space as a contingent construction and field of engagement, and presenting matter as a locus of production/performance/action. Consequently, it is such an expanded or relational dimension that constitutes the foundation of what in the context of this study is to be referred to as affective tectonics. Namely, a tectonics that represents processual and experiential multiplicity of convergent time and space, body and environment, the material and the immaterial; a tectonics in which matter neither appears as an inert and passive substance, nor is limited to the traditionally regarded tectonic significance or expressive values, but is presented as an active element charged with inherent potential and vitality. By defining such a relational materialism, the intention is to expand the spectrum of material attributes revealing the intrinsic relationships between the physical properties of materials and their performative, transformative and affective capacities, including effects of interference and haptic dynamics – i.e. protocols of transmission and interaction. The expression that encapsulates its essence is: ACTIVE MATERIALITY RESUMEN El significado de la materia ha estado desde siempre ligado al pensamiento y el quehacer arquitectónico. Sin embargo, muchos intentos de capturar su esencia se han visto sumergidos en una tensión dialéctica entre la forma y la materialidad, entre la consistencia material y los modos inmateriales de la percepción, entre los estados estáticos y los procesos dinámicos, entre lo real y lo virtual, revelando una creciente conciencia de la desconcertante complejidad del mundo material. En esta complejidad, la noción de la operatividad o capacidad agencial– que emerge desde y dentro de los procesos ecológicos, políticos y socio-culturales– requiere de una reconceptualización de la materia y los procesos inherentes a la materialización, ofreciendo una nueva visión del contexto y el espacio, entendidos como un campo relacional dinámico. Oscilando entre el discurso arquitectónico y la práctica arquitectónica, y atravesando un extenso territorio trans-disciplinar, el objetivo de la presente tesis es ilustrar la variedad de metodologías proyectuales que emergieron desde este enfoque relacional. Concretamente, la intención es indagar en las epistemologías espaciales vinculadas a la noción de la atmósfera– generalmente asociada a la llamada Nueva Fenomenología–, reflexionando sobre su impacto en la producción arquitectónica. A continuación, el estudio ofrece una doble línea argumental. Primero, a través del análisis crítico de la noción de atmósfera, el objetivo es explorar maneras de pensar y dar forma a la realidad a través de las relaciones, reconociendo la mencionada complejidad del universo material revelado a través de fuerzas humanas y no-humanas, materiales e inmateriales. Segundo, a pesar de que el interés por las atmósferas ha florecido en las últimas décadas, la intención es demostrar que las bases conceptuales y los protocolos proyectuales de la creación de atmósferas se pueden encontrar bajo la superficie de los debates contemporáneos. Para corroborar e ilustrar estas hipótesis se propone una metodología de carácter arqueológico, trazando una particular genealogía de proyectos– la que se basa en una conciencia atmosférica. Asimismo, al definir esta conciencia atmosférica, el estudio explora tanto la naturaleza notoriamente ambigua y la dimensión dual de la atmósfera– meteorológica y estética–, como la heterogeneidad de significados derivados de ellas. En este contexto, la atmósfera se entiende como un concepto detonante, ya que sobrepasa los limites formales y materiales de los cuerpos, llevando a la re-evaluación de la experiencia perceptiva y abriendo a preguntas la ortodoxa relación espacio- cuerpo-ambiente. En consecuencia, la noción de la atmósfera ofrece a la arquitectura una dimensión expandida donde manifestarse, definiendo el espacio como una construcción contingente, performativa y afectiva, y presentando la materia como locus de producción/ actuación/ acción. Es precisamente esta dimensión expandida relacional la que constituye una base para lo que en el contexto del presente estudio se define como una tectónica afectiva. Es decir, una tectónica que representa una multiplicidad procesual y experiencial derivada de la convergencia entre el tiempo y el espacio, el cuerpo y el entorno, lo material y lo inmaterial; una tectónica en la que la materia no aparece como una substancia pasiva e inerte, ni es limitada al significado considerado tradicionalmente constructivo o a sus valores expresivos, sino que se presenta como elemento activo cargado de un potencial y vitalidad inherentes. A través de la definición de este tipo de materialismo afectivo, la intención es expandir el espectro de los atributos materiales, revelando las relaciones intrínsecas entre las propiedades físicas de los materiales y sus capacidades performativas, transformativas y afectivas, incluyendo efectos de interferencias y dinámicas hápticas– o dicho de otro modo, protocolos de transmisión e interacción. Una expresión que encapsula su esencia vendría a ser: MATERIALIDAD ACTIVA

High-precision 40Ar/39Ar geochronology and the advent of North America’s Late Cretaceous terrestrial fauna

A densely sampled, diverse new fauna from the uppermost Cedar Mountain Formation, Utah, indicates that the basic pattern of faunal composition for the Late Cretaceous of North America was already established by the Albian-Cenomanian boundary. Multiple, concordant 40Ar/39Ar determinations from a volcanic ash associated with the fauna have an average age of 98.39 ± 0.07 million years. The fauna of the Cedar Mountain Formation records the first global appearance of hadrosaurid dinosaurs, advanced lizard (e.g., Helodermatidae), and mammal (e.g., Marsupialia) groups, and the first North American appearance of other taxa such as tyrannosaurids, pachycephalosaurs, and snakes. Although the origin of many groups is unclear, combined biostratigraphic and phylogenetic evidence suggests an Old World, specifically Asian, origin for some of the taxa, an hypothesis that is consistent with existing evidence from tectonics and marine invertebrates. Large-bodied herbivores are mainly represented by low-level browsers, ornithopod dinosaurs, whose radiations have been hypothesized to be related to the initial diversification of angiosperm plants. Diversity at the largest body sizes (>106 g) is low, in contrast to both preceding and succeeding faunas; sauropods, which underwent demise in the Northern hemisphere coincident with the radiation of angiosperms, apparently went temporarily unreplaced by other megaherbivores. Morphologic and taxonomic diversity among small, omnivorous mammals, multituberculates, is also low. A later apparent increase in diversity occurred during the Campanian, coincident with the appearance of major fruit types among angiosperms, suggesting the possibility of adaptive response to new resources.

Oceanic minerals: Their origin, nature of their environment, and significance

The chemical and isotopic compositions of oceanic biogenic and authigenic minerals contain invaluable information on the evolution of seawater, hence on the history of interaction between tectonics, climate, ocean circulation, and the evolution of life. Important advances and greater understanding of (a) key minor and trace element cycles with various residence times, (b) isotopic sources and sinks and fractionation behaviors, and (c) potential diagenetic problems, as well as developments in high-precision instrumentation, recently have been achieved. These advances provided new compelling evidence that neither gradualism nor uniformitarianism can explain many of the new important discoveries obtained from the chemistry and isotopic compositions of oceanic minerals. Presently, the best-developed geochemical proxies in biogenic carbonates are 18O/16O and Sr/Ca ratios (possibly Mg/Ca) for temperature; 87Sr/86Sr for input sources, Cd/Ca and Ba/Ca ratios for phosphate and alkalinity concentrations, respectively, thus also for ocean circulation; 13C/12C for ocean productivity; B isotopes for seawater pH;, U, Th isotopes, and 14C for dating; and Sr and Mn concentrations for diagenesis. The oceanic authigenic minerals most widely used for chemical paleoceanography are barite, evaporite sulfates, and hydrogenous ferromanganese nodules. Marine barite is an effective alternative monitor of seawater 87Sr/86Sr, especially where carbonates are diagenetically altered or absent. It also provides a high-resolution record of seawater sulfate S isotopes, (evaporite sulfates only carry an episodic record), with new insights on factors affecting the S and C cycles and atmospheric oxygen. High-resolution studies of Sr, Nd, and Pb isotopes of well-dated ferromanganese nodules contain invaluable records on climate driven changes in oceanic circulation.

Caracterização geocronológica (U-Pb), geoquímica e isotópica (Sr, Nd, Hf) do complexo Rio Capivari no terreno Embu

O Complexo Rio Capivari (CRC) é constituído por ortognaisses migmatíticos de composições graníticas a tonalíticas e anfibolitos subordinados (magmas toleíticos) em lascas tectônicas no Terreno Embu. As composições dos gnaisses do CRC são predominantemente cálcio-alcalinas a álcali-cálcicas. Idades U-Pb em núcleos de zircão com zoneamento oscilatório indicam cristalização magmática dos protólitos em três períodos principais 2.4, 2.2-2.1 e 2.0 Ga. Idades metamórficas foram reconhecidas em bordas de zircão totalmente escuras nas imagens de catodoluminescência e variam entre 620-590 Ma. A suíte sideriana (2.4 Ga) apresenta caráter juvenil, como evidenciado pelos valores positivos de \'\'épsilon\'\'IND.Nd\' (+3.8) e \'\'épsilon\'\'IND.Hf\' (+0.3 a +4.8) e pela ausência de núcleos de zircão herdado, comumente encontrados em rochas que sofreram retrabalhamento crustal. A suíte de idades riacianas (2.2-2.1 Ga) apresenta idades modelos TDM arqueanas (2.6-3.3 Ga), valores negativos de \'\'épsilon\'\'IND.Nd\' (-12.0 a -4.0) e negativos a levemente positivos de \'\'épsilon\'\'IND.Hf\' (-7.8 a +0.5). Portanto, tais rochas derivam de retrabalhamento de reservatórios crustais antigos. A suíte de idade orosiriana (2.0 Ga) apresenta fontes mais antigas e retrabalhadas com valores altamente negativos de \'\'épsilon\'\'IND.Nd\' (-10.4) e \'\'épsilon\'\'IND.Hf\' (-1.2 a -13.6), sugerindo prolongada residência crustal com idades modelo \'T IND.DM\' e \'T IND.Hf\' >3.3 Ga. As assinaturas de elementos traços em rocha total e a química de zircão sugerem fontes máficas para o gnaisse sideriano. Reservatórios de crosta média, mas de profundidades variáveis, parecem ser a principal fonte dos gnaisses riacianos e orosirianos. Análises em diagramas tectônicos discriminantes baseados em elementos traços de rocha total com elevadas razões \'La/Yb IND.(N)\' (>10), Nb/Yb (>2) e Th/Yb (>1), somados aos valores de \'Y IND.2\'\'O IND.3\' (<3000 ppm), U/Yb (>0.5) e Nb/Yb (0.01-0.10) da química de zircão, sugerem que ambas as suítes de idades foram geradas em ambientes de arco magmático continental, mas com um gap de 200-300 Ma entre o gnaisse sideriano e os gnaisses riacianos sem dados ou informações geológicas. Perfis multielementos (elementos traços) comparativos entre representação de amostras típicas de arco continental associado à subducção de crosta oceânica (margem andina) e amostras de arcos de ilha (Ilhas Mariana) confirmam afinidade com ambiente de arco continental para o CRC, associado à subducção de placa oceânica, principalmente para o gnaisse sideriano. Apesar de pouco representativo, devido ao número de amostras (n=1), uma acresção juvenil em 2.4 Ga colabora para uma dinâmica contínua da evolução da crosta continental. O papel desempenhado pelo CRC na evolução geral do Terreno Embu permanece enigmático. Os dados isotópicos de \'\'épsilon\'\'IND.Nd(590)\' e \'ANTPOT.87 Sr\'/\'ANTPOT.88 Sr IND.(i)\' do CRC (-27.3 a -19.7 e 0.704 a 0.722, respectivamente) indicam evolução temporal não compatível com o requerido para as fontes dos granitos ediacaranos do Terreno Embu, que exigem a participação de reservatórios mais primitivos (\'\'épsilon\'\'IND.Nd(590)\' -13 a -7) e empobrecidos em Rb (\'ANTPOT.87 Sr\'/\'ANTPOT.88 Sr IND.(i)\' \'\'QUASE IGUAL A\' 0,710).

Geologia e petrologia da ilha de São Sebastião (Estado de São Paulo)

A ilha de São Sebastião consta principalmente de rochas alcalinas que formam um maciço de 300 km2 aproximadamente, constituindo o terceiro em área no Brasil. Apresenta-se em um "stock" alongado segundo NE-SW, encaixado em estruturas de gnais. As formações geológicas encontradas consistem em 1 - Granitos e Gnais (ARQUEANO), 2 - Eruptivas básicas (RÉTICO), 3 - Eruptivas alcalinas (JURÁSSICO) e 4 - Depósitos recentes (HOLOCENO). O método de estudo empregado foi o petrográfico e a coluna geológica estabelecida em base de dados petrográficos, tectônicos e fisiográficos. O arqueano é determinado por definição dos seus tipos petrográficos (1- gnais facoidal, 2- oligoclásio-gnais, 3- hornblenda-gnais, 4- biotita-gnais e 5- microlina-granito) idênticos aos concorrentes no considerado arqueano do Brasil meridional. O triássico (rético) é conferido às rochas básicas (diabásios e basaltos) pela sua semelhança tectônica e petrográfica com as congêneres que cortam de maneira semelhante o arqueano no continente. A "mise-en-place" das eruptivas alcalinas (1- Nordmarkito, 2- Biotita-pulaskito, 3- Pulaskito, 4- Nefelina-sienito, 5- Foiaito, 6- Essexito-foiaito, 7- Essexito e 8- Teralito) pode ser considerada jurássica devido suas relações com as eruptivas básicas referidas réticas, pois na praia do Bonete (foto 14) observa-se um dique de nordmarkito cortando outro de diabásio. As eruptivas quartzo-dioríticas (quartzo-microdiorito e quartzo-andesito) cortam as alcalinas no cume do Zabumba, indicando sua idade mais moderna que estas. Além deste fato, preenchem linhas de fraturas tectônicas recentes, como as falhas ao longo do canal de São Sebastião, indicando que a topografia deveria ser a mesma que a atual para permitir rios efusivos ao nível do canal ou que pelo menos toda a zona de extrusão estivesse, como hoje está, em superfície. Os depósitos aluviais marinhos e continentais são considerados recentes, (holocênicos) pelo favor da topografia onde se dispõe, ocupando o fundo os vales e os bordos do atual modelado costeiro, idade esta conferida em base fisiográfica. A tectônica que afetou a ilha de São Sebastião participa da que atuou em todo o litoral meridional brasileiro. Pode-se distinguir duas fases distintas: na primeira ocorreram as erupções básicas e as alcalinas subsidiárias e na segunda deram-se os falhamentos escalonados em blocos basculados para NW, com as fraturas de tensão preenchidas pelas eruptivas quartzo-dioríticas. Toda a atividade tectônica foi regulada pela direção NE-SW privilegiada da estrutura do arqueano, correspondente a antigos eixos dos dobramentos laurencianos e huronianos. A geomorfologia da ilha consta de uma antiga superfície de erosão rematada até a senilidade, - o peneplano cretáceo, hoje reduzida às cristas culminares do maciço alcalino e às satélites das estruturas gnáissicas, desnivelada pelo falhamento em blocos e ligeiramente adernada para NW devido ao basculamento. Ao lado desta topografia vestigial existe o modelado atual da ilha caracterizado por uma juventude do estágio evolutivo. Esta escultura foi inaugurada com os últimos levantamentos epirogênicos que ascenderam as eruptivas alcalinas plutônicas a mais de 1.300 m sobre o nível do mar. O modelado costeiro apresenta uma costa típica de submergência com esculturas em rias, no estágio da juventude. A presença de terraceamentos marinhos de abrasão, atualmente elevados cerca de 20 a 30 m, lembra as oscilações epirogênicas ou eustáticas do litoral.

Brachiopod assemblages from the Early-Middle Jurassic transition in the Eastern Subbetic (SE Spain): Systematic and palaeobiogeographic implications and palaeoenvironmental significance

New data on brachiopod assemblages recorded in the Eastern Subbetic area (Alicante, SE Spain) and attributed to the Early Bajocian (Humphriesianum Zone and/or immediately older) are provided. Eleven species have been distinguished and reported for the first time in the Subbetic domain of the Betic Cordillera. The description of the morphological evidences on each analysed taxa, especially in relation to their internal morphology, brings new implications in the systematics of the Middle Jurassic brachiopods. The analysis of faunistic affinity between the recorded assemblages and those from other palaeogeographic domains, shows that the Subbetic brachiopod fauna has a clear Mediterranean affinity, as proved by the different species belonging to the genera Striirhynchia, Septocrurella, Mondegia?, Karadagithyris, Linguithyris, Papodina?, Viallithyris?, and Zugmayeria?. It is also evidenced that the Early-Middle Jurassic transition in the Eastern Subbetic accounted, in qualitative terms, a remarkable interval of faunistic renewal in the brachiopod assemblages, strongly influenced by a complex tectonic and stratigraphic framework controlled by a period of intense extensional tectonics, globally framed in the evolution of the Atlantic Ocean.

Tectonic control on the sedimentary record of the central Moldavidian Basin (Eastern Carpathians, Romania)

The sedimentary record of the Tarcău and Vrancea Nappes, belonging to the flysch accretionary zone of the Eastern Carpathians (Eastern Carpathian Outer Flysch), registered Cretaceous-Miocene events during the evolution of the Moldavidian Basin. Our biostratigraphic data indicate that the deposits studied are younger than previously reported. The comparison of sedimentary record studied with the Late Cretaceous-Early Miocene global eustatic curve indicates that eustatic factor played a secondary role, after the tectonic one. Four main stages of different processes influenced by tectonics are recognized in the sedimentary record: (1) Campanian-Maastrichtian-earliest Paleocene; (2) latest Ypresian-Lutetian; (3) late Chattian-earliest Aquitanian, and (4) late Aquitanian-early Burdigalian. The late Chattian- earliest Aquitanian and late Aquitanian-early Burdigalian records indicate a high tectonic influence. The first event was related to the foredeep stage of the sedimentary domain studied, and the second one to the deformation stage of the same domain. The sedimentary records of tectonic influence recognized during these stages are useful tools for geodynamic reconstructions. The stratigraphic correlation of Tarcău and Vrancea sedimentary records are used

Tasas de deformación GPS en la cuenca del Bajo Segura (Cordillera Bética oriental)

En este trabajo hemos cuantificado las tasas de deformación actual de la cuenca del Bajo Segura (NE del corredor de cizalla de la Bética oriental), a partir del análisis de una red GPS con 11 vértices geodésicos. Se han analizado los datos de cuatro campañas GPS entre junio de 1999 y enero de 2013, que han sido procesados con la versión 6.2 del software GIPSY-OASIS. Este software utiliza la técnica de posicionamiento puntual de precisión conocido por las siglas PPP. Se observa un acortamiento ~N-S en toda la cuenca de mayor magnitud en el sur, en la zona de falla del Bajo Segura, con valores que varían de oeste a este entre 0,73 y 0,24 mm/año. En el borde septentrional de la cuenca, en la zona de falla de Crevillente, los valores de acortamiento N-S son menores. Sin embargo, en esta falla se ha observado un movimiento lateral sinistrorso que, en la componente E-O, varía entre 0,44 y 0,75 mm/año.

Paleogene evolution of the External Betic Zone and geodynamic implications

Interdisciplinary studies combining field data (geological and tectonic mapping, lithostratigraphic reconstructions, lithofacies characterization, correlations and sampling) and laboratory analyses (biostratigraphy, chronostratigraphy, clay mineralogy and sandstone petrography) of eight Senonian-Paleogene successions from the Sierra de La Pila and Sierra de El Carche areas (Murcia province, SE Spain) belonging to the External Betic Zone are presented. Field evidence of tectonic activity (slumps, olistostromes, syn-genetic folds, lateral variability, changes in thicknesses, para- and unconformity boundaries, stratigraphic gaps, shallowing upward trends to emersion, etc.) was found in several Paleogene intervals. The results enable a better reconstruction of the stratigraphic architecture and chronostratigraphy of the Paleogene record, highlighting in particular: facies evolution, discontinuities, depositional sequences (Middle-Upper Maastrichtian, Upper Paleocene-Middle Eocene, Oligocene-Lower Aquitanian), environmental evolution (homogeneous conditions during the Late Cretaceous and successive realm diversification from platform to slope to basin) and correlations, along the Prebetic to Subbetic transition, which is a key sector to understand the northeastward variations of the South Iberian margin. A conclusive paleogeographic and geodynamic evolutionary model for the study area is proposed, hypothesizing that Paleogene compressive tectonics affected the eastern External Betic Zone. In addition, correlations with successions from the western External Betic Zone evidenced asynchronous deformation from east to west along the internalmost External Betic Zone. Moreover, a comparison with the external Tunisian Tell enables the recognition of similar sedimentarytectonic events, imposing new constraints in the Paleogene geodynamic reconstruction throughout the western Tethys.

An insight into the breakup of Gondwana: Identifying events through low-temperature thermochronology from the basement rocks of Madagascar

Fission track analysis was applied to the Precambrian suites of Madagascar in order to identify the lower-temperature cooling histories and their relationships to the Phanerozoic events that affected the island. Apatite ages range from 431 to 68 Ma, and zircon ages range from 452 to 238 Ma. Thermochronologically, the island can be divided into a southern, central, and northern region each with a subdivision on an east-west basis. The southern region is sharply separated from the central region by strongly contrasting apparent apatite ages over the northwest-southeast striking Ranotsara Shear Zone (RSZ). The change in apparent ages over the RSZ is indicative of later reactivation along younger brittle faults. The central region has the oldest ages of the island and has a diffuse contact to the third region northward. Along the entire western margin of the Precambrian basement initial Paleozoic exhumation was followed by heating (burial by sediments) during Jurassic and Cretaceous times. A decrease in ages along the eastern margin from 119 to 68 Ma coincides with the predicted positions of the Marion hot spot after effects of erosion are considered. On the other hand, these ages may represent progressive opening of the margin in a southward direction together with associated denudation of the rift shoulder. The eastern part of the central region has remained very stable since at least Devonian times, undergoing only long-term very slow exhumation at rates of 1–5 m/Myr.