Tectonica do Complexo Varginha na regiao de Sao Joao da Boa Vista (SP)

Migmatites, high-grade gneisses and granitoids represent the most important Precambrian rocks of Sao Joao da Boa Vista region. Structures are interpreted as due to low-angle oblique non-coaxial ductile shear, developed under conditions of amphibolite facies. Transcurrent ductile shear zones and associated drags modify the foliation and lineations orientations. A first phase of migmatization related to anatexis seems to be developed before or early during the thermo-tectonic process. A second one is syntectonic, and represents the main regional phase. Joints and faults represent the brittle features, the faults marked by cataclastic rocks and intense retrometamorphism along the main zones. -from English summary

Megaestruturacao pre-cambriana do territorio brasileiro baseada em dados geofisicos e geologicos

Crustal discontinuities may be seen as A-type collision sutures with triple junction arrays. Shear belts developed at the block borders due to oblique plate convergence. A consistent litho-structural zoning may be observed along the border zones of the blocks: the known high-grade terrains are exposed along the upper block border and pass to distal granite-greenstone terrains; in the lower block, granite-greenstone terrains form the older basement, and supracrustals occur as a metavolcano-sedimentary belt near or adjacent to the suture. This regional litho-structural framework may be related to diachronous collisions of sialic masses which lead to their amalgamation into an extensive continental mass. -from English summary

Paraná Basin: Mineral resource potentials in Brazil, Uruguay, and Paraguay

The Paraná Basin is a Western Gondwanan cratonic basin that is better defined as the Paraná depositional site, since it has a diverse history as a basin. Sedimentation started in the Ordovician-Silurian, followed by extensive marine Devonian deposition. A Late Paleozoic/ Triassic facies cycle wedge was clearly built during Pangean time. The Early Cretaceous was characterized by extensive basaltic lava flows immediately before the break-up of Pangea. Following these rifting and drifting processes, the basin's structural framework was totally rebuilt, generating new depositional sites in the Late Cretaceous to Tertiary. Based on more recent data, at least two different basins may be defined during the evolution of what was once considered a unique basin. Nevertheless, even if considered as a single basin, the sedimentary pile of the Paraná Basin has considerable economic potential, until now exploited only rudimentarily, except for its groundwater resources. Aggregates, limestones, clays, industrial sands, gems, dimension stones, hydrocarbons, coal, peat, and uranium are some of the potential mineral resources of this basin. Copyright © 1997 by V. H. Winston & Son, Inc. All rights reserved.

Modelagem gravimétrica da Bacia de Taubaté-vale do Rio Paraíba do Sul, leste do estado de São Paulo

This paper presents the gravity survey refinement of the Paraíba do Sul river valley, east region of São Paulo state, by acquisition of 646 gravity stations. Further than the traditional Free-Air and Bouguer corrections, it was necessary to apply the Terrain Correction due the proximity of the Mantiqueira and Mar mountain ranges. An enhanced understanding of Taubaté Basin structural framework was the main objetive of this work. As result, we present the Bouguer Gravity Map of the east region of São Paulo State and the Residual Bouguer Gravity Map generated by Upward Continuation and High-pass filtering. The 2D Gravity Modeling was applied in 4 sections, using bi-dimensional models for the bodies that produced the anomalies (Talwani Method). After integrating the gravity data with the interpretation of 11 seismic sections, it was possible to delineate the Taubate Basin structural framework, which shows an utmost sedimentary thickness of 800 m in the depocenters. It was also interpreted an ultramaphic alkaline plug in the subsurface of Caçapava city.

Molecular model of shikimate kinase from Mycobacterium tuberculosis

Tuberculosis (TB) resurged in the late 1980s and now kills approximately 3 million people a year. The reemergence of tuberculosis as a public health threat has created a need to develop new anti-mycobacterial agents. The shikimate pathway is an attractive target for herbicides and anti-microbial agents development because it is essential in algae, higher plants, bacteria, and fungi, but absent from mammals. Homologs to enzymes in the shikimate pathway have been identified in the genome sequence of Mycobacterium tuberculosis. Among them, the shikimate kinase I encoding gene (aroK) was proposed to be present by sequence homology. Accordingly, to pave the way for structural and functional efforts towards anti-mycobacterial agents development, here we describe the molecular modeling of M. tuberculosis shikimate kinase that should provide a structural framework on which the design of specific inhibitors may be based. © 2002 Elsevier Science (USA). All rights reserved.

Análise, modelagem e interpretação de dados gravimétricos no lineamento Guapiara - região sudeste do estado de São Paulo

Pós-graduação em Geologia Regional - IGCE

Inter-relação entre geologia/relevo/solo/vegetação e atuação dos processos morfodinâmicos da unidade de paisagem serra do Japi: uma contribuição à conservação

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Mapeamento do relevo do embasamento de bacias sedimentares através da inversão gravimétrica vinculada

Apresentamos três novos métodos estáveis de inversão gravimétrica para estimar o relevo de uma interface arbitrária separando dois meios. Para a garantia da estabilidade da solução, introduzimos informações a priori sobre a interface a ser mapeada, através da minimização de um (ou mais) funcional estabilizante. Portanto, estes três métodos se diferenciam pelos tipos de informação físico-geológica incorporados. No primeiro método, denominado suavidade global, as profundidades da interface são estimadas em pontos discretos, presumindo-se o conhecimento a priori sobre o contraste de densidade entre os meios. Para a estabilização do problema inverso introduzimos dois vínculos: (a) proximidade entre as profundidades estimadas e verdadeiras da interface em alguns pontos fornecidas por furos de sondagem; e (b) proximidade entre as profundidades estimadas em pontos adjacentes. A combinação destes dois vínculos impõe uma suavidade uniforme a toda interface estimada, minimizando, simultaneamente em alguns pontos, os desajustes entre as profundidades conhecidas pelas sondagens e as estimadas nos mesmos pontos. O segundo método, denominado suavidade ponderada, estima as profundidades da interface em pontos discretos, admitindo o conhecimento a priori do contraste de densidade. Neste método, incorpora-se a informação geológica que a interface é suave, exceto em regiões de descontinuidades produzidas por falhas, ou seja, a interface é predominantemente suave porém localmente descontínua. Para a incorporação desta informação, desenvolvemos um processo iterativo em que três tipos de vínculos são impostos aos parâmetros: (a) ponderação da proximidade entre as profundidades estimadas em pontos adjacentes; (b) limites inferior e superior para as profundidades; e (c) proximidade entre todas as profundidades estimadas e um valor numérico conhecido. Inicializando com a solução estimada pelo método da suavidade global, este segundo método, iterativamente, acentua as feições geométricas presentes na solução inicial; ou seja, regiões suaves da interface tendem a tornar-se mais suaves e regiões abruptas tendem a tornar-se mais abruptas. Para tanto, este método atribui diferentes pesos ao vínculo de proximidade entre as profundidades adjacentes. Estes pesos são automaticamente atualizados de modo a acentuar as descontinuidades sutilmente detectadas pela solução da suavidade global. Os vínculos (b) e (c) são usados para compensar a perda da estabilidade, devida à introdução de pesos próximos a zero em alguns dos vínculos de proximidade entre parâmetros adjacentes, e incorporar a informação a priori que a região mais profunda da interface apresenta-se plana e horizontal. O vínculo (b) impõe, de modo estrito, que qualquer profundidade estimada é não negativa e menor que o valor de máxima profundidade da interface conhecido a priori; o vínculo (c) impõe que todas as profundidades estimadas são próximas a um valor que deliberadamente viola a profundidade máxima da interface. O compromisso entre os vínculos conflitantes (b) e (c) resulta na tendenciosidade da solução final em acentuar descontinuidades verticais e apresentar uma estimativa suave e achatada da região mais profunda. O terceiro método, denominado mínimo momento de inércia, estima os contrastes de densidade de uma região da subsuperfície discretizada em volumes elementares prismáticos. Este método incorpora a informação geológica que a interface a ser mapeada delimita uma fonte anômala que apresenta dimensões horizontais maiores que sua maior dimensão vertical, com bordas mergulhando verticalmente ou em direção ao centro de massa e que toda a massa (ou deficiência de massa) anômala está concentrada, de modo compacto, em torno de um nível de referência. Conceitualmente, estas informações são introduzidas pela minimização do momento de inércia das fontes em relação ao nível de referência conhecido a priori. Esta minimização é efetuada em um subespaço de parâmetros consistindo de fontes compactas e apresentando bordas mergulhando verticalmente ou em direção ao centro de massa. Efetivamente, estas informações são introduzidas através de um processo iterativo inicializando com uma solução cujo momento de inércia é próximo a zero, acrescentando, em cada iteração, uma contribuição com mínimo momento de inércia em relação ao nível de referência, de modo que a nova estimativa obedeça a limites mínimo e máximo do contraste de densidade, e minimize, simultaneamente, os desajustes entre os dados gravimétricos observados e ajustados. Adicionalmente, o processo iterativo tende a "congelar" as estimativas em um dos limites (mínimo ou máximo). O resultado final é uma fonte anômala compactada em torno do nível de referência cuja distribuição de constraste de densidade tende ao limite superior (em valor absoluto) estabelecido a priori. Estes três métodos foram aplicados a dados sintéticos e reais produzidos pelo relevo do embasamento de bacias sedimentares. A suavidade global produziu uma boa reconstrução do arcabouço de bacias que violam a condição de suavidade, tanto em dados sintéticos como em dados da Bacia do Recôncavo. Este método, apresenta a menor resolução quando comparado com os outros dois métodos. A suavidade ponderada produziu uma melhoria na resolução de relevos de embasamentos que apresentam falhamentos com grandes rejeitos e altos ângulos de mergulho, indicando uma grande potencialidade na interpretação do arcabouço de bacias extensionais, como mostramos em testes com dados sintéticos e dados do Steptoe Valley, Nevada, EUA, e da Bacia do Recôncavo. No método do mínimo momento de inércia, tomou-se como nível de referência o nível médio do terreno. As aplicações a dados sintéticos e às anomalias Bouguer do Graben de San Jacinto, California, EUA, e da Bacia do Recôncavo mostraram que, em comparação com os métodos da suavidade global e ponderada, este método estima com excelente resolução falhamentos com pequenos rejeitos sem impor a restrição da interface apresentar poucas descontinuidades locais, como no método da suavidade ponderada.

Mapeamento de uma interface separando dois meios homogêneos através da reconstituição gravimétrica compacta: aplicação a dados do LEPLAC-IV

O problema do mapeamento de uma interface separando dois meios homogêneos tem sido tradicionalmente resolvido através da continuação para baixo da anomalia gravimétrica observada. Este procedimento requer a utilização de um filtro passa-baixa ou de um parâmetro de amortecimento, que tendem a diminuir a resolução do relevo estimado da interface. Além disso, o uso da continuação para baixo implica supor (desnecessariamente) que a interface é uma superfície harmônica. Desta forma, a utilização da continuação para baixo é restrita a interfaces que apresentam um relevo suave relativamente à sua profundidade média. As restrições impostas pela continuação para baixo do campo gravimétrico são reduzidas na técnica de inversão proposta para este estudo, cujo objetivo é mapear a interface crosta-manto baseada na incorporação de informações a priori sobre o mínimo momento de inércia da fonte causadora, em relação a um eixo de concentração de massa pré-estabelecido e coincidente com o topo da fonte anômala. Além da introdução de informações sobre o mínimo momento, foi incluída também a possibilidade de haver variação lateral e em profundidade de densidade em setores previamente estabelecidos, o que permite estender a aplicação desta técnica a situações geológicas mais complexas que envolvam a reconstituição de corpos justapostos, que sejam de diferentes naturezas, tais como aqueles presentes em zonas de transição crustal. O método de inversão apresentado foi avaliado em testes usando dados sintéticos e os resultados obtidos mostraram a eficiência desta técnica em recuperar corpos alongados horizontalmente, que apresentem como topo ou base, interfaces arbitrárias a serem mapeadas. Foi também constatada a eficácia do método em reconstituir corpos que comportem variação lateral de densidade que pudessem retratar situações em que se deseja investigar a natureza do embasamento em regiões de transição crustal. Com base nos resultados destes testes, a técnica foi então empregada na inversão gravimétrica de cinco perfis do LEPLAC IV que cruzam a região oceânica adjacente à margem continental sudeste brasileira. Os resultados desta aplicação permitiram inferir a natureza dos corpos que constituem o arcabouço estrutural da região onde encontram-se inseridas a Dorsal de São Paulo e a Zona de Fratura de Porto Alegre, assim como mapear a Moho subjacente.

Interpretação tectono-estratigráfica do reservatório Quissamã (Eo-meso-albiano) nos campos de Pampo, Bicudo e Bonito, Bacia de Campos

Hydrocarbon accumulations occur in marine carbonate reservoirs of Quissamã Formation (early to midlle Albian), southwest Campos Basin. We investigated Pampo, Bicudo and Bonito fields, in order to understand the tectono-structural framework of oncolite/bioclast coarse-grained calcarenite reservoir and the calcilutite-marl-shale sealing interval (Late Albian to Turonian). The database of eleven wells from those fields allowed to elaborate structural sections correlating the Macaé Group – both Quissamã reservoir and Outeiro seal, the latter corresponding to the tectonic deepening phase of basin evolution. Based on density and electric logs, it was prepared structural sections of the carbonate reservoirs with consequent identification of porous zones and oil-water contacts. An extensive 3-D seismic database (~300 Km2) allowed to map three reflectors which represent the limiting units of Macaé Group

Análise das respostas de atributos sísmicos dos carbonatos barremiano, albiano e neógeno no campo de Bonito, bacia de Campos - RJ

The Bonito oil field, located on southwest of Campos Basin-RJ, has been explored since 1982. The main reservoir is composed by calcarenites of Quissamã Formation (Macaé Group) from Albian, but two other carbonate levels are present on the field, firsts is Coqueiros Formation (Aptian) and the second Siri Member (Oligo-Miocene). In this context and considering that carbonates reservoirs are a challenge for exploratory geoscientists, since the difficulty on recognize the effective reservoir distribution. This work aim to characterize the geophysical/geological facies based on seismic attributes responses, related to reservoir geometrical distribution, for the tree carbonates intervals on Bonito oil Field. A tree dimensional interpretation of the levels has been developed, based on well cross correlation and a 3D seismic interpretation, resulting on the stratigraphic and structural framework of the field, which showed a NE-SW fault trend controlling the Aptian carbonates reservoirs, and halocnetics structures showing a structural trap on Albian carbonates reservoirs. The definition of the structural/ stratigraphic framework possibly the seismic attributes calculations over the reservoir intervals. To select the best response in comparison with the reservoir distribution, obtained by seismic interpretation, the attributes response were compared with isopachs maps of each carbonate stratigraphic level. The attributes Maximum Amplitude, Maximum Magnitude and Rms Amplitude showed a good answer to reservoir distribution. The Rms Amplitude also showed a good correlation with physical rock properties, like RHOB bulk density, for the Albian and Aptian carbonates, as consequence it is possible make a characterization of reservoir distribution based on seismic attribute answer

Purchasing Organization and Design: A Literature Review

This paper presents the results of a comprehensive literature review of the organization of purchasing covering the period from 1967 to 2009. The review provides a structured overview of prior research topics and findings and identifies gaps in the existing literature that may be addressed in future research. The intention of the review is to a) synthesize prior research, b) provide researchers with a structural framework on which future research on the organization of purchasing may be oriented, and c) suggest promising areas for future research.

(Table 1) Magnetic susceptibility readings in the western part of the Sør Rondane Montains

The Sør Rondane Mountains (SRM) in eastern Dronning Maud Land (DML) are located in an area, where two apparent Pan-African (650-520 Ma) orogenic mobile belts appear to intersect, the East African-Antarctic Orogen and the Kuunga Orogen. Hence, a better understanding of the tectonic structure of the Sør Rondane region is an important key for unravelling the complex geodynamic evolution of the eastern DML and adjacent regions of East Antarctica during the Late Neoproterozoic/Early Palaeozoic amalgamation of Gondwana. The SRM were recently (2011-2012) aerogeophysically investigated with a 5 km flight line spacing, covering a total area of ~140,000 km². The aeromagnetic data are correlated with ground-based magnetic susceptibility measurements and geological field data and allow to project tectonic terranes and individual structures into ice-covered areas. Magnetic anomalies and basement foliation trends are collinear in areas dominated by simple shear deformation, whereas an area of large-scale refolding correlates with a subdued small-scale broken magnetic anomaly pattern. The latter area can be regarded as a distinct tectonic domain, the central Sør Rondane corridor. It magnetically separates the SRM into an eastern, a central, and a western portion. This subdivision is presumably related to late Pan-African extensional tectonics and suggests that such a tectonic regime may play a larger role than previously assumed. Voluminous late Pan-African granitoids, which are mainly undeformed, correlate with positive magnetic anomalies between +30 and +80 nT, while a strong magnetic high (+680 nT) near the granitic intrusion at Dufekfjellet is caused by a highly magnetised enigmatic body. The recently discovered prominent magnetic anomaly province of southeastern DML continues into the southern part of the Sør Rondane region, where only a few outcrops are exposed. Findings at these westernmost nunataks of the SRM indicate that the subdued magnetic anomaly pattern of this southeastern DML province is most likely caused by the predominance of metasedimentary rocks of yet unknown age.

Dinámicas de ocupación urbana del Anillo Verde metropolitano, desde sus orígenes en el Plan General del Área Metropolitana de Madrid de 1963 hasta el Plan General de Ordenación Urbana de 1997

El Anillo Verde metropolitano, definido por el Plan General de Ordenación Urbana del Área Metropolitana de Madrid en 1963 siguiendo los modelos planteados por la cultura urbanística internacional, como armadura de la estructura urbana del AMM, espacio protagonista dentro del sistema de espacios libres, lugar de uso público destinado al recreo y contacto con la naturaleza de la población madrileña, se convierte en realidad en una reserva de suelo que va entrando en juego motivado por las alianzas entre el poder institucional y la clase social dominante actuando al margen del planeamiento, poniendo en evidencia la escasez de recursos legales y culturales disponibles para la salvaguarda de los intereses comunes y, donde los condicionantes geográficos y naturales del territorio madrileño han influido decisivamente en la especialización funcional y espacial del Área Metropolitana de Madrid. Así pues considerando esta idea como HIPÓTESIS, el objetivo de la TESIS sería demostrarla, para lo cual se hace necesario primero, acotar espacial y temporalmente el objeto de estudio, es decir, del Anillo Verde metropolitano1, segundo, contextualizar histórica y disciplinarmente los presupuestos teóricos que conformaban la idea del Anillo Verde, tercero, reconocer, localizar y documentar las piezas que han ido materializando la ocupación urbana del Anillo Verde, clasificándolas según parámetros temporales, funcionales, urbanísticos y, formales, lo que permite analizar la geografía, uso, instrumentación y forma de su transformación a escala general metropolitana y, cuarto, profundizar a modo de comprobación a escala municipal y urbana en dos escenarios representativos del conjunto metropolitano: el municipio de Pozuelo de Alarcón y el distrito de Hortaleza-Barajas. El contenido del documento se divide en tres bloques, el bloque I, se centra en las bases teóricas, el bloque II sitúa el hilo argumental de la tesis a escala metropolitana y el bloque III comprueba el fenómeno a escala municipal y urbana. De esta forma, se comienza por la comprensión del significado del concepto del Anillo Verde, que va más allá de la dimensión instrumental asignada de límite y contención urbana frente al crecimiento de la ciudad industrial de principios del siglo XX, basada en la descentralización de la ciudad tradicional, para adquirir un significado más complejo, como gran espacio de reserva y salvaguarda de valores naturales y culturales que se expresaban en su territorio y que permitirían alcanzar el equilibrio entre la ciudad y sus habitantes, es decir, entre el hombre y el espacio que habita. Se hace un recorrido por las principales corrientes urbanísticas que se van nutriendo de distintas disciplinas (economía, sociología, geografía, biología, ecología) para plantear teorías que permitieran materializar un nuevo orden urbano según principios de equidad social, económica y ambiental, en una secuencia donde Europa y Estados Unidos realizaban un constante intercambio -el movimiento de la Ciudad Jardín o el Regionalismo, que dieron paso a propuestas como el Greater London o el Gran Berlín, donde la figura del Anillo Verde tenía un papel protagonista, y del que también participaría nuestro país y la ciudad de Madrid, con modelos regionales como el Plan Besteiro y urbanos como el Plan Bidagor, antecedentes directos del Plan General de Ordenación Urbana del Área Metropolitana de Madrid de 1963 que pone en marcha la ordenación del crecimiento metropolitano de Madrid. El hilo argumental de la tesis se organiza en una doble aproximación: un acercamiento a escala metropolitana a partir del reconocimiento del modelo de ciudad definido en los distintos planes generales que acompañaron el desarrollo metropolitano (municipio de Madrid y de los siete términos municipales que rodeaban a este y que tenían suelo destinado a Anillo Verde), haciendo referencia además a las relaciones con el planeamiento regional, concretando en una escala de aproximación municipal que avanza hasta la interpretación urbana detallada. El primer acercamiento tiene lugar en el bloque II y se organiza en tres capítulos. El capítulo 4 se dedica al punto obligado de partida de la geografía local, describiendo las características biofísicas de los terrenos que formaban parte del Anillo Verde, que han marcado históricamente la forma de aprovechamiento del territorio, desde las extensiones de bosques mediterráneos al norte y al oeste continuación del Monte del Pardo, a los distintos tipos de cultivo que se adaptaban al sustrato geológico y la forma del terreno (de las suaves ondulaciones de sedimentos arcósicos al norte a las extensas plataformas arenosas y yesíferas del sur), además de las zonas de huertos aprovechando las depresiones y los cursos de agua (arroyo del Monte Carmelo, arroyo de Valdebebas, arroyo del Quinto, arroyo del Santo, arroyo Butarque, arroyo Meaques y arroyo Pozuelo). Una vez reconocida la realidad física, el capítulo 5, avanza en la descripción de los distintos modelos de ciudad propuestos desde el planeamiento urbanístico, en sus distintas escalas, la regional y la municipal, como respuesta a la coyuntura social, económica y política que ha caracterizado el proceso de ocupación del Anillo Verde al compás de la construcción del AMM. Se han reunido las propuestas de planeamiento municipal de los distintos municipios que disponían de terreno calificado como Anillo Verde: Madrid, Coslada, Getafe, Leganés, Alcorcón, Boadilla del Monte y Pozuelo de Alarcón. Además se han incorporado las distintas propuestas de ordenación territorial que han servido de referencia al planeamiento municipal, en todas sus versiones, desde las sectoriales, de mayor éxito y apoyo institucional, a los distintos intentos de ordenación integral, de mayor complejidad pero de menor calado, precisamente por la dificultad de consenso entre la ordenación física y el desarrollo económico, entre los intereses privados y el beneficio público. El primer horizonte, comienza con la formulación del Plan General de Ordenación Urbana del Área Metropolitana de Madrid de 1963, su desarrollo y la puesta en marcha de los primeros planes municipales en la década de los años setenta, donde se comprueba la necesidad de un marco regional que “ordene” el territorio de forma integral y sirva de referencia a las actuaciones sectoriales que habían marcado el primer desarrollo metropolitano. El segundo, se sitúa dos décadas más tarde con la aprobación del Plan General de Ordenación Urbana de Madrid de 1985 y el conjunto de planes municipales de los términos limítrofes, que siguen su filosofía de austeridad en cuanto a crecimiento territorial. El tercero se inicia en 1997 con la siguiente generación de planes de corte neoliberal que imponen un modelo territorial basado en las grandes operaciones metropolitanas de centralidad, infraestructuras y equipamiento, que consumen de forma indiscriminada la totalidad del territorio madrileño. Será en el último capítulo del segundo bloque (capítulo 6) donde se represente gráficamente a escala metropolitana y se analicen las 229 piezas que han ido colmatando el espacio destinado a Anillo Verde, según los parámetros de estudio, en base a las cuales se plantean las primeras conclusiones generales de la tesis, poniendo de manifiesto que las alianzas entre los agentes soberanos en la construcción de la ciudad y su entorno han trasgredido sucesivamente las determinaciones del Planeamiento en su definición de modelo de ciudad y territorio, acusando la carencia de recursos instrumentales y jurídicos que alentaron el proceso de su desmantelamiento, y revelando la influencia de los condicionantes geográficos y naturales en la especialización funcional y segregación social en el conjunto del Área Metropolitana de Madrid. Se remata el discurso metropolitano con una batería de conclusiones que interpretan el fenómeno de ocupación del anillo de verdor metropolitano confirmando las hipótesis iniciales, reconociendo los valores medioambientales y culturales trasgredidos, sus diversos actores, las numerosas operaciones urbanísticas desarrolladas con distintos usos y envergadura, así como los instrumentos de planeamiento utilizados, en base a las cuales se materializa la construcción del AMM según un modelo extendido (spread), dibujando una mancha de aceite (o grase-spots según Geddes) que precisamente había querido evitarse desde el planeamiento urbanístico con la definición de un Anillo Verde, espacio inmune a la edificación, que se aleja de su papel estructurante (equilibrador entre la ciudad y sus habitantes) para convertirse en armadura de la estructura comunicativa, que una vez consolidada se convierte en la mejor aliada de la máquina inmobiliaria. El último paso, se desarrolla en el bloque III que se divide en los capítulo 7,8 y 9 y supone la comprobación de lo descrito en el conjunto de escala metropolitana, en dos aspectos fundamentales, la falta de consideración por los valores culturales y medioambientales que han modelado el territorio, imprimiéndole un carácter singular y específico y, la estructura del dominio del suelo, donde se reconoce de forma precisa el grupo social y los agentes encargados en cada momento de comercializar los suelos del anillo, que bajo el paraguas de la urgencia social y el engañoso beneficio popular, obtienen importantes beneficios económicos. Con esa intención, se da un salto hacia la escala municipal y urbana, seleccionando dos escenarios de estudio, el municipio de Pozuelo de Alarcón, que representa la materialización del crecimiento suburbano de la élite madrileña ocupando las zonas de mayor valor ecológico del anillo, y el distrito de Hortaleza-Barajas que ofrece su territorio a las grandes operaciones metropolitanas, apoyándose en el eje de actividad marcado por la conexión Madrid-Barcelona y el sistema aeroportuario de escala global, ambos situados al norte de la línea de borde entre la Sierra y la Mancha, ocupando por tanto los lugares más valiosos de la geografía madrileña (estructura funcional anticipada por Bidagor en 1946 en su modelo de ciudad adaptada al territorio madrileño) Una vez descrito este proceso trasgresor de límites, de normas, de conductas, y desde una perspectiva del fenómeno suficientemente documentada, en el capítulo 10, se realiza una reflexión sobre la incidencia real de la propuesta urbanística del Anillo Verde en la construcción del AMM, de la misma forma que se sugieren nuevos roles al planeamiento en un formato intencionado de largo recorrido en oposición a lo inmediato y circunstancial, que permita hacer una nueva lectura de los presupuestos teóricos que conformaban la idea del Anillo Verde, espacio articulador (medioambiental, social y cultural) del territorio madrileño. ABSTRACT The Metropolitan Greenbelt was defined by the 1963 Master Plan for the Madrid Metropolitan Area (MMA), following established international models of urban development, as the structural framework of the MMA, the principal open space within its network of open spaces and a public area of recreation and contact with nature for the residents of Madrid. In reality, however, it ha become a reserve of land in which various alliances between the institutional authorities and the dominant social class have been operating on the margin of the original plan, exposing a scarcity of legal and cultural resources for the safeguarding of common interests, and in which the geographical and natural characteristics of the territory itself have come to play an influential role in the functional specialization and spatial segregation of the MMA. With that idea as its HYPOTHESIS, the aim of this THESIS is to demonstrate its reality. The first step in this is to delineate, temporally and spatially, the object of study; i.e. the Metropolitan Greenbelt2. The second is to contextualize historically and disciplinarily those theoretical ideas which conform to the greenbelt concept. The third is to acknowledge, locate and document the elements which have characterized the urban occupation of the Greenbelt and classify these according to the parameters of time, function, urban development and form, which in turn would enable the geography, use, instrumentation and form of its transformation to be analysed on a general metropolitan scale. The fourth step, as a method of verification, is an in-depth analysis of two representative settings within the metropolitan network: the municipality of Pozuelo de Alarcón and the Hortaleza-Barajas district. The content of the document is divided into three parts. Part I focuses on the study’s theoretical foundations, Part II establishes a line of argument at the metropolitan level and Part III examines the phenomenon from a municipal and urban perspective. The thesis, then, begins with a study of the greenbelt concept itself and its meaning, which is far more complex than the accepted instrumental dimension of limiting and containing urbanization in response to the growth of the industrial city of the early 20th century, and which is based on a decentralization of the traditional city. This wider purpose is the setting aside of a large reserved space to safeguard the natural and cultural values of the region and thereby achieve a balance between the city and its residents; that is to say, between man and the space he inhabits. The principal currents of thought in urban planning will then be examined. These have drawn upon a variety of disciplines (economics, sociology, geography, biology, ecology) to develop theories for establishing a new urban order according to the principles of social, economic and environmental equity, and have involved a constant interchange between Europe and the United States. Thus, the City Garden and Regionalist movements would clear the way for proposals such as Greater London and Great Berlin, Chicago and Washington, in which the greenbelt would play a fundamental role. The participation of our own country and the city of Madrid is also discussed, through regional models such as the Besteiro Plan and urban ones like the Bidagor Plan, direct forerunners of 1963’s General Organizational Plan for the Madrid Metropolitan Area, which would set into motion the organization of Madrid’s metropolitan growth. The line of argument followed in this thesis is two-fold: first, an examination of metropolitan development in keeping with the city model as defined in the various General Plans for the development of both the municipality of Madrid and the seven surrounding municipalities which have land designated for its Greenbelt; and second, an examination of this growth in relation to Regional Planning measures, is detailed on a smaller scale (municipal and district), where the conditioning factors affecting the land property structure and the network of biophysical units may be analysed in depth. The first of these is dealt with in Part II and organized into three chapters (4, 5 and 6). Chapter 4 is dedicated to the obligatory starting point of the geographical setting itself. The biophysical characteristics of the territories set aside for the Greenbelt, and which historically have played a role in the area’s exploitation, are described here. These range from expanses of Mediterranean woodland to the north and west of Monte del Pardo to the various types of farmland that have been adapted to the geological substratum and the contours of the terrain (gentle undulations of arkosic sediment in the north, and wide sandy and gypsiferous tableland in the south), as well as orchards planted in low valleys and along watercourses (the creeks of Monte Carmelo, Valdebebas, Quinto, Santo, Butarque, Meaques and Pozuelo). Once this physical reality ha been detailed, in Chapter 5 will examine the various city models proposed by urban planners, both regionally and municipally, in response to the confluence of social, economic and political interests that have characterized the process of occupation in the Greenbelt area during the construction of the MMA. Municipal planning proposals will be collected and examined for the various municipalities which have land designated for the Greenbelt: Madrid, Coslada, Getafe, Leganés, Alcorcón, Boadilla del Monte and Pozuelo de Alarcón. Furthermore, the various territorial organization proposals which have served as references for municipal planning will also be addressed here, in all of their versions –from the sectorial, which have met with more success and institutional approval, to the many attempts at integration, which have been more complex but less influential, precisely for the difficulty of reconciling physical organization with economic development, and private interest with public benefit. The first period in this process was the development of the General Plan of 1963, followed by the first municipal development plans of the 1970s, in which the need for a regional framework that “organized” the territory in an integral fashion was defined. This would serve as a reference for the sectorial actions that marked the metropolitan area’s initial development. The second came two decades later with the approval of the General Plan of 1985, and the network of municipal plans for the surrounding communities, which followed the same philosophy of austerity with regard to territorial growth. The third would begin to take form in 1997, as a new generation of neo-liberal development plans imposed a territorial model based on centralized large-scale metropolitan operations of infrastructure and equipment, which would indiscriminately consume the totality of Madrid’s land. At the end of the Part II, in Chapter 6, the metropolitan area will be represented graphically and the 229 pieces that have been gradually encroaching upon land designated for the Greenbelt will be analysed. This analysis will be carried out according to the parameters defined for the study, and the first general conclusions of the thesis will be based on its findings. It will show how alliances between the various governing authorities in the construction of the city and its environment have successively violated established plans with regard to the definitions of city and territory, how shortages of instrumental and judicial resources have accentuated the dismantling process, and how natural and geographical factors have influenced functional specialization and social segregation in the Madrid Metropolitan Area. The final step, detailed in Part III, will address two fundamental aspects of what has just been described: the lack of consideration for the cultural and environmental values which have shaped this territory and imprinted upon it a specific and unique character; and the structure of land domination, with a precise identification of the social group and agents responsible at each stage of the Greenbelt’s commercialization, who, under an umbrella of social urgency and deceptive public benefit, have used it to obtain substantial financial rewards. For this purpose, a closer look is taken at two specific areas: the municipality of Pozuelo de Alarcón, representative of the suburban growth of an elite population which has occupied the Greenbelt areas of the greatest ecological value; and the Hortaleza-Barajas district, which has offered its territory to large metropolitan business interests, based on activities centred on the connection between Madrid and Barcelona and the system of international air travel. Both of these settings are located to the north of the line which divides the Sierra from La Mancha, and thus occupy the most valuable land in the Madrid region (a functional structure anticipated by Bidagor in 1946, with his city model adapted to the territory of Madrid). Finally, an attempt will be made to interpret the phenomenon of metropolitan Greenbelt occupation, confirming initial hypotheses, specifying the environmental and cultural values that have been violated, and identifying the various players involved, as well as numerous urbanization operations of varying sizes and interests, and the instruments of planning they have used. It will be seen from this that the construction of the MMA has in fact followed a “spread” model, a “grease spot” (as Geddes calls it) which, from the outset of the planning process and according to the definition of a greenbelt as a construction-free zone, was precisely to be avoided. This structural role (to provide a balance between a city and its residents) has thus been abandoned and the Greenbelt converted instead into a communicative framework which, once consolidated, has become the greatest ally of the real estate machine. After this process of violating limits, norms and established behaviour has been described and solidly documented, a reflection will be made on the real influence of the Greenbelt proposal in the construction of the MMA. At the same time, new roles will be suggested for future planning, roles which are deliberate and long term, in opposition to the immediate and circumstantial. This will enable a new interpretation of the theoretical principles behind the greenbelt concept, a space designed to connect the territory of Madrid environmentally, socially and culturally.

The structure of the two amino-terminal domains of human ICAM-1 suggests how it functions as a rhinovirus receptor and as an LFA-1 integrin ligand

The normal function of human intercellular adhesion molecule-1 (ICAM-1) is to provide adhesion between endothelial cells and leukocytes after injury or stress. ICAM-1 binds to leukocyte function-associated antigen (LFA-1) or macrophage-1 antigen (Mac-1). However, ICAM-1 is also used as a receptor by the major group of human rhinoviruses and is a catalyst for the subsequent viral uncoating during cell entry. The three-dimensional atomic structure of the two amino-terminal domains (D1 and D2) of ICAM-1 has been determined to 2.2-Å resolution and fitted into a cryoelectron microscopy reconstruction of a rhinovirus–ICAM-1 complex. Rhinovirus attachment is confined to the BC, CD, DE, and FG loops of the amino-terminal Ig-like domain (D1) at the end distal to the cellular membrane. The loops are considerably different in structure to those of human ICAM-2 or murine ICAM-1, which do not bind rhinoviruses. There are extensive charge interactions between ICAM-1 and human rhinoviruses, which are mostly conserved in both major and minor receptor groups of rhinoviruses. The interaction of ICAMs with LFA-1 is known to be mediated by a divalent cation bound to the insertion (I)-domain on the α chain of LFA-1 and the carboxyl group of a conserved glutamic acid residue on ICAMs. Domain D1 has been docked with the known structure of the I-domain. The resultant model is consistent with mutational data and provides a structural framework for the adhesion between these molecules.