(Table 1) K-Ar age determinations on biotite from coarse sand within DSDP Sample 72-516F-76-4,107-115

Qualitative petrographic study of selected clastic horizons within the Eocene section of Hole 516F has revealed the presence of abundant fine-grained lithic fragments, probably volcanic, along with coarser fragments of quartz and feldspar apparently derived from a nearby plutonic terrain. In detail, poor sorting, presence of graded bedding, and an abundance of clay suggest these are turbidite horizons locally derived from a mixed volcanic/plutonic terrain, possibly with some direct contribution from contemporary volcanic ash falls. A progressive increase in plutonic versus volcanic components with time is, however, more consistent with an erosional origin for most of this material. Unusual euhedral dark biotite is abundant in several of the lower clastic horizons; it is most easily interpreted as microphenocrysts weathered in situ out of alkalic volcanic ash. Biotite separated from Sample 516F-76-4,107-115 cm, has been dated by the K-Ar method at about 46 Ma. Alkaline volcanoes active on the Rio Grande Rise in the middle Eocene would be the most probable source of this ash and would be consistent with other evidence for potassic, alkaline volcanism along the Rio Grande Rise and at the Tristan da Cunha hot spot.

Estudio de los materiales que componen el sistema constructivo de las viviendas del casco histórico de Maracaibo (Venezuela)

En este trabajo de investigación que se presenta para optar al grado de Doctor, se analizan y estudian los materiales que conforman las viviendas de mampostería de arenisca “Piedra de Ojo” del casco histórico de Maracaibo, Venezuela, construidas en el siglo XIX. No existe una bibliografía descriptiva técnico-constructiva del sistema constructivo, por lo que esta tesis complementa la escasa descripción estilística existente donde apenas se mencionan algunos materiales de construcción. Definido el marco histórico y las manzanas del área en donde se encontraban las viviendas preseleccionadas a estudiar, en la visita de campo se seleccionaron 12 que se encontraban en estado de deterioro, y que permitieron recolectar las muestras más fácilmente. Para realizar la caracterización y comportamientos de los diferentes materiales utilizados: piedra y morteros en los cerramientos, maderas en armaduras de tejados, techos y carpintería de puertas y ventanas, cerámicos en muros y acabados, etc. Para complementar lo antes dicho se ha dividido esta tesis en seis capítulos: En el capítulo I se desarrolla el estado del arte a nivel nacional e internacional de trabajos de investigación, similares. Se aborda la memoria histórica, que es una reseña de la evolución de la vivienda en la ciudad de Maracaibo. En el capítulo II se describe la metodología empleada en la tesis, de acuerdo a los objetivos, tanto generales como específicos de la investigación. Que ha cubierto diferentes frentes: consulta bibliográfica, levantamiento planimétrico, toma de muestras, análisis de visu, caracterización físico-química y correlación de resultados. Se ha desarrollado el trabajo tanto in situ como en laboratorio y despacho. El capítulo III presenta la caracterización de la arenisca “Piedra de Ojo”, se desarrolla: la descripción geológica y caracterización petrológica. Se reseñan los ensayos realizados en laboratorio como: caracterización de visu, caracterización petrográfica, estudio petrográfico por microcopia óptica de trasmisión, estudio petrográfico por microcopia electrónica de barrido, microscopia electrónica de barrido en modo electrones secundarios (SSE) y microscopia electrónica de barrido en modo electrones retrodispersados. También las propiedades escalares de los mampuestos y los siguientes valores: densidades, porosidades y resistencia mecánicas, entre otros. En el capítulo IV se analizan las características de los morteros aplicados en las viviendas, y la patología o lesiones que presentan. Se clasifican en tres tipos: mortero de junta o asiento, de enfoscado y revoco. Se documenta la realización de los ensayos físicos y químicos, resistencia mecánica y de granulometría; se explican sus componentes principales: conglomerante de cal, áridos y aditivos y la tecnología de fabricación, así como las características físicas, hídricas, químicas y granulométricas. El capítulo V, contiene las aplicaciones constructivas de los materiales de albañilería, Se describen otros elementos de la vivienda como; cimentaciones, muros mixtos, molduras, apliques y pinturas y finalmente pavimentos. Y en el capítulo VI se analizan las especies de madera más representativas usadas en las armaduras de las cubiertas, así como los elementos de cubrición. De igual forma se describe la carpintería de puertas y ventanas, así como sus dinteles o cargaderos de madera y se realiza la identificación anatómica, las propiedades físicas y mecánicas de las utilizadas. Entre los resultados y conclusiones se determinó que el 90% de los materiales utilizados en su construcción proceden de zonas cercanas a la construcción de la vivienda, como la formación El Milagro convertida en cantera de piedra y que el resto de los materiales provenían de la Isla de Toas y de la exportación de las islas del Caribe y de Europa como el cemento. El principal aporte de esta investigación es el análisis técnico constructivo y la caracterización física, mecánica y química de los materiales de la vivienda, con el fin de que dicha información sea usada para definir los materiales nuevos a utilizar en las restauraciones de las viviendas y en futuras líneas de investigación. ABSTRACT In this research paper submitted to opt to the degree of Doctor, the materials that make the “Piedra de Ojo” sandstone masonry houses of the historical center of Maracaibo, Venezuela, built in the XIX century, are analyzed and studied. There exists no technical-constructive descriptive literature of the constructive system, so this thesis complements the very limited existing stylistic description, where barely some construction materials are mentioned. With the historical context and the blocks of the area where the preselected houses to be studied being defined, 12 of these houses that were in a state of decay (deterioration) were selected and this condition allowed to collect samples more easily, in order to carry out the characterization and behavior of the different materials used: stone and mortars in the walls, wood trusses in roofs, ceilings and woodwork of doors and windows, walls and ceramic finishes, etc. To complement the foregoing, this thesis has been divided in six chapters: In Chapter I, the state of art at national and international levels of similar research is developed, which is a review of the evolution of housing in the city of Maracaibo. In Chapter II, the methodology used in the thesis is described, according to the research’s objectives, general and specific ones, which have covered several fronts: literature survey, planimetric survey, sampling, visu analysis, physical-chemical characterization and correlation of results. Chapter III presents the characterization of the “Piedra de Ojo” sandstone; geological description and petrologic characterization are developed. Essays performed in the laboratory are reviewed, such as: visu characterization, petrographic characaterization, petrographic study by optical microscopy of transmission, petrographic study by electronic scanning microscopy in secondary electron mode (SSE) and electron microscopy scaning by backscattered electron mode. Also scalar properties of the masonry and the following: density, porosity and mechanical resistance, among others. In Chapter IV, characteristics of the mortars used in the houses are analyzed and pathology or damages are presented. They are classified into three types: grout, cement render and plaster. Physical and chemical testing, mechanical strength and grain size (granulometric) is documented; its main components are explained: lime binder, aggregates and additives and manufacturing technology as well as the physical, water, chemical and granulometric characteristics. Chapter V contains the constructive applications of masonry materials. Other housing elements are described, such as; foundations, mixed walls, moldings, wall paintings and finally floorings (pavements). And in chapter VI the most representative species of wood used in the overhead fixtures and cover elements are analyzed. Likewise, woodwork of doors and windows and their wooden lintels or landings are described; anatomical identification and physical and mechanical properties of the ones used is made. The results and conclusions determined that 90% of the materials used in its construction came from areas near the construction of housing, such as El Milagro formation, converted into stone quarry and other materials came from the Toas Island and from the export of the Caribbean islands and Europe, such as cement. The main contribution of this research is the constructive technical analysis and physical, mechanical and chemical characterization of the materials of the houses, in order that such information is used to define the new materials to be used in the housing restoration and future research lines.

Estudio de propiedades físicas de las rocas

El objetivo de este taller es mostrar a los alumnos mediante experiencias de laboratorio sencillas y de bajo coste algunas metodologías de estudio de las propiedades físicas de las rocas como material de construcción. Las propiedades físicas de las rocas determinan su uso y comportamiento tanto como materiales de construcción como soportes de obra civil. La determinación de las propiedades físicas complementan el estudio mineralógico y textural (petrográfico) de los materiales pétreos y naturales. Las propiedades petrofísicas más importantes que se abordan en este taller son el sistema poroso (porosidad); transporte de fluidos (permeabilidad, capilaridad); propiedades mecánicas (estáticas y dinámicas); la durabilidad de las rocas frente a las sales, hielo, ataque ácido, etc.

Evolução diagenética e caracterização dos reservatórios da seção devoniana na Bacia do Rio do Peixe-Nordeste do Brasil

The Rio do Peixe Basin represents a main basin of northeastern Brazil and pioneering work positioned the rocks of this basin in the Early Cretaceous. However, a recent study, based on integrated pollen analysis from three wells, found an unprecedented siliciclastic sedimentary section, in the region, of early Devonian age. Therefore, the present study aims a detailed petrographic and petrological analysis of this devonian section, in the Rio do Peixe Basin and proposes a diagenetic evolution, to understand the characteristics of the porous system, identify the main reservoir petrofacies with the main factors impacting on the quality of these rocks as reservoirs and a quick study on the provenance of this section. The petrographic study was based on samples obtained from subsurface and surface. The diagenetic evolution of petrofacies and its identification were based only on subsurface samples and the study of provenance was based on surface samples. The thin sections were prepared from sandstones, pelites and sandstones intercalated with pelites. The original detrital composition for this section is arcosean and the main diagenetic processes that affected these rocks occur in various depths and different conditions, which resulted in extensive diagenetic variety. The following processes were identified: early fracture and healing of grains; albitization of K-feldspar and plagioclase; siderite; precipitation of silica and feldspar; mechanical infiltration of clay and its transformation to illite/esmectite and illite; autigenesis of analcime; dissolution; autigenesis of chlorite; dolomite/ferrous dolomite/anquerite; apatite; calcite; pyrite; titanium minerals and iron oxide-hidroxide. The occurrence of a recently discovered volcanism, in the Rio do Peixe Basin, may have influenced the diagenetic evolution of this section. Three diagenetic stages affected the Devonian section: eo, meso and telodiagenesis. This section is compositionally quite feldspathic, indicating provenance from continental blocks, between transitional continental and uplift of the basement. From this study, we observed a wide heterogeneity in the role of the studied sandstones as reservoirs. Seven petrofacies were identified, taking into account the main diagenetic constituent responsible for the reduction of porosity. It is possible that the loss of original porosity was influenced by intense diagenesis in these rocks, where the main constituent for the loss of porosity are clays minerals, oxides and carbonate cement (calcite and dolomite)

Marbles and carbonate rocks from central Morocco: a petrographic, mineralogical and geochemical study

Petrographic, mineralogical, and stable isotopes (delta C-13, delta O-18 values) compositions were used to characterise marbles and sedimentary carbonate rocks from central Morocco, which are considered to be a likely source of ornamental and building material from Roman time to the present day. This new data set was used in the frame of an archaeometric provenance study on Roman artefacts from the town of Thamusida (Kenitra, north Morocco), to assess the potential employment of these rocks for the manufacture of the archaeological materials. A representative set of samples from marbles and other carbonate rocks (limestone, dolostone) were collected in several quarries and outcrops in the Moroccan Meseta, in a region extending from the Meknes-Khenifra alignment to the Atlantic Ocean. All the samples were studied using a petrographic, mineralogical and geochemical methods. The petrographic and minerological investigations (optical microscopy, electron microscopy, X-ray diffraction) allowed to group the carbonate rocks in limestones, foliated limestone, diagenetic breccias and dolostone. The limestones could be further grouped as mudstones, wackestones-packstones, crinoid grainstones, oolitic grainstone and floatstones. Textural differences allowed to define marbles varieties. The stable carbon and oxygen isotope composition proved to be quite useful in the discrimination of marble sources, with apparently less discriminatory potential for carbonate rocks.