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.

Electron petrography of fine-grained matrix in the Karoonda C4 carbonaceous chondrite

The study of matrices of rare Type 4 carbonaceous chondrites can reveal important information on parent body rnetamorp~ic processes and provide a comparison with processes on parent bodies of ordinary chc-idrites. Reflectance spectra (Tholen, 1984) from the two largest asteroids in the asteroid belt, Ceres and Pallas, suggest that they may be metamorphosed carbonaceous chondrites. These two asteroids constitute - onethird of the mass in the asteroid belt implying that type 4-6 carbonaceous chondrites are poorly represented in the meteorite collection and may be of considerable importance. The matrix of the C4 chondrite Karoonda has been investigated using a JEOL 2000FX analytical electron microscope (AEM) with an attached Tracor-Northem TN5500 energy dispersive spectrometer (EDS). In previous studies (Scott and Taylor, 1985; Fitzgerald, 1979; Van Schmus, 1969), the petrography of the Karoonda matrix has been described as consisting largely of coarse-grained (50-200 urn in size) olivine and plagioclase (20-100 um in size), associated with micrometer sized magnetite and rare sulphides. AEM observations on matrix show that in addition to these large grains, there is a significant fraction (10 vol%) of interstitial fine grained phases « 5 urn). The mineralogy of these fine-grained phases differs in some respects from that of the coarser-grained matrix identified by optical and SEM techniques (Scott and Taylor, 1985; Fitzgerald, 1979; Van Schmus, 1969). I~ particular crystals of two compositionally distinct pyroxenes « 2 urn in size) have been identified which have not been previously observed in Karoonda by other analytical techniques. Thin film microanalyses (Mackinnon et al., 1986) of these two pyroxenes indicate compositions consistent with augite and low-Ca pyroxene (- Fs27). Fine-grained anhedral olivine « 2 urn size) is the most abundant phase with composition -Fa29' This composition is essentially indistinguishable from that determined for coarser-grained matrix olivines using an electron microprobe (Scott and Taylor, 1985; Fitzgerald, 1979; Van Schmus, 1969). All olivines are associated with subhedral magnetites « 1 urn size) which contain significant Cr (- 2%) and Al (- 1%) as was also noted for larger sized Karoonda magnetites by Delaney et al. (1985). It has recently been suggested (Burgess et al., 1987) on the basis of sulphur release profiles for S-isotope analyses of Karoonda that CaS04 (anhydrite) may be present. However, no sulphate phase has, as yet, been identified in the matrix of Karoonda. Low magnification contrast images suggest that Karoonda may have a significant porosity within the fine-grained matrix fraction. Most crystals are anhedral and do not show evidence for significant compaction. Individual grains often show single point contact with other grains which result in abundant intergranular voids. These voids frequently contain epoxy which was used as part of the specimen preparation procedure due to the friable nature of the bulk sample.

Integrating petrography, mineralogy and hydrochemistry to constrain the influence and distribution of groundwater contributions to baseflow in poorly productive aquifers: Insights from Gortinlieve catchment, Co. Donegal, NW Ireland

Identifying groundwater contributions to baseflowforms an essential part of surfacewater body characterisation. The Gortinlieve catchment (5 km2) comprises a headwater stream network of the Carrigans River, itself a tributary of the River Foyle, NW Ireland. The bedrock comprises poorly productive metasediments that are characterised by fracture porosity. We present the findings of a multi-disciplinary study that integrates new hydrochemical and mineralogical investigations with existing hydraulic, geophysical and structural data to identify the scales of groundwater flow and the nature of groundwater/bedrock interaction (chemical denudation). At the catchment scale, the development of deep weathering profiles is controlled by NE-SW regional scale fracture zones associated with mountain building during the Grampian orogeny. In-situ chemical denudation of mineral phases is controlled by micro- to meso-scale fractures related to Alpine compression during Palaeocene to Oligocene times. The alteration of primary muscovite, chlorite (clinochlore) and albite along the surfaces of these small-scale fractures has resulted in the precipitation of illite, montmorillonite and illite/montmorillonite clay admixtures. The interconnected but discontinuous nature of these small-scale structures highlights the role of larger scale faults and fissures in the supply and transportation of weathering solutions to/from the sites of mineral weathering. The dissolution of primarily mineral phases releases the major ions Mg, Ca and HCO3 that are shown to subsequently formthe chemical makeup of groundwaters. Borehole groundwater and stream baseflow hydrochemical data are used to constrain the depths of groundwater flow pathways influencing the chemistry of surface waters throughout the stream profile. The results show that it is predominantly the lower part of the catchment, which receives inputs from catchment/regional scale groundwater flow, that is found to contribute to the maintenance of annual baseflow levels. This study identifies the importance
of deep groundwater in maintaining annual baseflow levels in poorly productive bedrock systems.

Petrography and geochemistry of the McArthur Township area, Ontario /

The McArthur Township area in the Archean Abitibi Belt of northeast Ontario contains northwesterly trending volcanic rocks which are located on a limb of a large syncline. The axial trace of the syncline passes through the adjacent Douglas Township. The Archean volcanic rocks and associated sedimentary rocks are intruded and deformed by two large plutons and a few smaller hypabyssal intrusions. A petrographic and geochemical study of the Precambrian rocks exposed 1n the study area was undertaken in order to investigate the metamorphic grade and geochemical characteristics of the rocks. All the samples were studied with the microscope and analysis of 20 major and trace elements were determined on a selection of the less altered specimens by x-ray fluorescence. Three different periods of igneous activity have occurred in the study area. The first two periods were dominated by volcanic extrusive rocks accompanied by gabbroic sills. The third cycle is the diapiric intrusion of the granitic plutons and subsequent metamorphism of the older rocks to the low to medium grade. Two periods of sedimentation are also recognized in the study area which occurred after the first and second cycle of volcanism. Chemically, the lavas are subdivided into three main associations: (1) The komatiitic association is characterized by high MgO, high Ni, low Ti02 and a low FeO*/(FeO* + MgO) ratio. They occupy the base of each volcanic cycle and some of the flows exhibit spinifex textures. (2) The tholeiitic association displays distinct iron and titanium enrichment trends in the intermediate membersor -i r (3) The calc-alkaline association contains low FeO* and TI02 and high Ni contents relative to modern calc-alkaline types. They are formed at the end of each cycle of volcanism and overlie the tholeiitic flows. All three associations of the first volcanic cycle are exposed in the study area, while the second cycle is represented by a komatiltic sequence. The volcanic rocks were possibly formed by multiple partial melting of the Archean mantle to produce parental magmas under various P - T conditions.

Petrography, geochemistry and structure of the Timmins area, Ontario

Regional structural analysis of the Timmins area indicates four major periods of tectonic deformation. The DI deformation is characterized by a series of isoclinal FI folds which are outlined in the study area by bedding, pillow tops and variolitic flows. The D2 deformation developed the Porcupine Syncline and refolded the Fl folds about a NE. axis. A pervasive S2 foliation developed during low grade (greenschist) regional metamorphism associated with the D2 deformation. The S2 foliation developed south of the Destor-Porcupine Break. The third phase of tectonic D3 deformation is recognized by the development of a S3 sub-horizontal crenulation cleavage which developed on the plane of the S2 foliation. No meso scopic folds are associated with this deformation. The 8 3 crenulation cleavage is observed south of the Destor-Porcupine Break. The D4 tectonic deformation is recorded as a subvertical S4 crenulation cleavage which developed on the plane of the S2 foliation and also offsets the S3 crenulation cleavage. Macroscopic F4 folds have refolded the F2 axial plane. No metamorphic recrystallization is associated with this deformation. The S4 crenulation cleavage is observed south of the Destor-Porcupine Break. Petrographic evidence indicates that the Timmins area has been subjected to pervasive regional low grade (greenschist) metamorphism which has recrystallized the original mineralogy. South of the study are~ the Donut Lake ultramafic lavas have been subjected to contact medium grade (amphibolite facies) metamorphism associated with the intrusion of the Peterlong Lake Complex. The Archean volcanic rocks of the Timmins area have been subdivided into komatiitic, tholeiitic and calcalkaline suites based on Zr, Ti0 2 and Ni. The three elements were used because of their r e lative immobility during subsequent metamorphic events. Geochemical observations in the Timmins area indicates that the composition of the Goose Lake and Donut Lake Formations are a series of peridotitic, pyroxenitic and basaltic komatiites. The Lower Schumacher Formation is a sequence of basaltic komatiites while the upper part of the Lower Schumacher Formation is an intercalated sequence of basaltic komatiites and low Ti0 2 tholeiites. The variolitic flows are felsic tholeiites in composition and geochemical evidenc e sugg ests that they developed as a n immiscible splitting of a tholeiitic magma. The Upper Schumacher Formation is a sequence of tholeiitic rocks dis p laying a mild iron enrichment. The Krist and Boomerang Formations are the felsic calc-alkaline rocks of the study area which are characteristically pyroclastic. The Redstone Fo rmation is dominantly a calc-alkali ne sequence of volcani c rocks whose minor mafic end me mbers exposed in 1t.he study hav e basaltic komatiitic compositions. Geochemical evidence sugges ts that the Keewatin-type se dimentary rocks have a composition similar to a quartz diorite or a granodiorite. Fi e l d obs ervations and petrographic evidence suggests that they were derived fr om a distal source and now repr esent i n part a turbidite sequence. The Timiskaming-type sedimentary rocks approach the c omp osi t ion of the felsic calc-alkaline rocks of the study area . The basal conglomerate in the study are a sugge s ts that th e uni t was derived fr om a proximal source. Petrographic and ge ochemical evidence suggests that the peridotitic and pyroxenitic komatiites originated as a 35-55% partial melt within the mantle, in excess of 100 Km. depth. The melt ros e as a diapir with the subsequent effusion of the ultramafic lavas, The basaltic komatiites and tholeiitic rocks originated in the mantle from lesser degrees of partial melting and fractionated in low pressure chambers. Geochemical evidence suggests a "genetic link" between the basaltic komatiites and tholeiites, The calc-alkaline rocks developed as a result of the increa.se In PO in the magma chamber. The felsic calcalkaline rocks are a late stage effusion possibly the last major volcanic eruptions in the area.

Petrography, Petrochemistry and petrogenesis of Huronian volcanic rocks of the Elliot Lake region, Ontario

In the Elliot lake region of northern Ontario, Yolcanlc lava piles represent the lowermost units of the Huronian SUpergroup. These rocks general1y trend east-west and belong to the Elliot lake Group. They are s1tuated on the north and south limbs or the QuIrke lake Syncline. The volcanIc rocks of this study contain a secondary minerai assemblage consisting of actinolite, biotite, chlorIte, eptdote/cllnozoislte tttanomagnettte and calcite characteristic of greenschist metamorphism. Compilation of data suggests that metamorphism of the volcanic rocks proceeded between 325- and 425-C and between 2.4 and 4.7 kb. Geochemtcally these lavas represent tholeiitic and calc-alkaline assemblages. The tholeiites are character1sttcally enriched tn Fe and Tt and consist mainly of basalts, basaltic andesites and andesites. These rocks are believed to have formed by the partIal melting of a peridottte source at low P-T. In contrast, the calc-alkaline rocks are depleted in Fe and TI, but show a signIficant enrichment In 51 and Zr; andesIte Is the major rock type for thIs assemblage. I·t Is postUlated that the calc-alkalIne sU1te of rocks was the result of eIther the partIal meltIng of abasaltic·magma at shallow depth, or the melttng of s1al1c crustal materIal due to the added we1ght of tholeiitIc material on an unstable crust and to downwarplng processes Inttlated by convection cells.

Geological collections : dynamical geology and petrography

UANL

México, su evolución social: síntesis de la historia política de la organización administrativa y militar y del estado económico de la Federación mexicana.. de sus conquistas en el campo industrial agrícola, minero, mercatil, etc. Inventario monumental que resume en trabajos magistrales..

UANL

Petrography, Geochemistry and Diagenesis of Coral Deposits of Kavaratti and Minicoy Islands, Lakshadweep, India

In the present thesis the petrographic, geochemical and digenetic variability of the sediments in the islands of Kavaratti and Minicoy has been investigated .The beach profile studies show that in the Kavaratti lagoon beach, the slope is steeper in the southern and south central part than in the northern end’s marginal deposition is taking place in the northern end of the Kavaratti island, whereas a marginal erosion is observed at the southern end. In Minicoy the slope of the lagoon beach is gentle in the south and is slightly steeper at the northern part of the beach. The southern and northern beach sections show a marginal deposition. Based on the mineralogical and geochemical studies it is concluded that the main digenetic changes observed is the transformation of aragonite to LMC.The transformation takes place mainly in the vadose zone and is caused by the abundance of fresh water infiltration.

Guía didáctica minero-ambiental del litoral de la Región de Murcia.

Investigación realizada bajo la modalidad de Proyectos de Investigación Educativa, en la licencia por estudios concedida a su autora durante el curso 2005-2006 por la Dirección General de Personal de la Consejería de Educación y Cultura de la Región de Murcia.

Realizaciones educativas promovidas por el empresario minero asturiano

Concretar y caracterizar la pol??tica educativa puesta en pr??ctica por el sector m??s representativo de la burgues??a industrial, abordando su actuaci??n concreta en el ??mbito escolar, desde la d??cada de los 80 del siglo XIX hasta el t??rmino de la Segunda Rep??blica. Cuantificar, periodizar la configuraci??n de la red escolar que desarrollan los patronos de las grandes empresas hulleras, documentarla, tipificarla en sus rasgos m??s determinantes, y las distintas fases y rasgos diferenciales. El primer cap??tulo ofrece una s??ntesis apretada que presenta a los protagonistas, el empresario minero, en relaci??n con el fen??meno de la industrializaci??n y el posterior desarrollo. El segundo cap??tulo atiende las condiciones que explican la adopci??n, por parte de los patronos de la miner??a asturiana, del programa paternalista destinado a configurar el inexistente trabajador industrial, dando cuenta de los sistemas ideados y experimentados por la patronal para el logro de objetivos productivos. En el tercer cap??tulo se analizan las diferentes instituciones patronales que sirven de veh??culo de gesti??n e intervenci??n educativa en la poblaci??n obrera. En el cuarto se analiza la intervenci??n patronal en el tiempo escolar y no escolar de los hijos de sus obreros, los objetivos y medios de consecuci??n, as?? como los elementos de la filantrop??a y el higienismo presentes en la educaci??n de la infancia y juventud de ambos sexos, as?? como en la educaci??n de adultos. Y por ??ltimo el quinto cap??tulo se centra en la creaci??n y desarrollo del mapa escolar patronal, cuya periodizaci??n responde a las adaptaciones provocadas por la convivencia con una realidad social, laboral, econ??mica, pol??tica e ideol??gica cambiante. Fuentes documentales bibliogr??ficas y archiv??sticas. La instauraci??n en Asturias en la segunda mitad del siglo XIX de la industria a gran escala oblig?? a los patrones a crear poblaci??n obrera y transformar los modos y h??bitos de vida y trabajo preindustriales, y a formar y disciplinar a los obreros que, en aquellas actividades industriales como la miner??a subterr??nea y la metal??rgia, depend??an del trabajador de oficio. Para ello se crearon un conjunto de instituciones patronales como la vivienda obrera, las cajas de ahorros y retiros, las cajas y asociaciones de socorros, economatos o cooperativas y las escuelas, que fueron inversiones productivas, pues a largo plazo podr??an disponer de obreros productivos y disciplinados.

Gestión inmobiliaria en los proyectos de infraestructura : enfoque al sector minero y petrolero

Con la realización y publicación de este libro se busca, principalmente, hacer una presentación y exposición del panorama legal relacionado con la negociación, adquisición, acceso y utilización de predios o terrenos –bien sean propiedad privada, como del Estado—requeridos para el desarrollo y ejecución de las actividades de los sectores minero y petrolero. Asimismo, se hace un breve repaso de algunos conceptos jurídicos generales relacionados con el tema de bienes inmuebles y servidumbres, contemplados en el Código Civil Colombiano, como antesala para el mejor entendimiento de su parte especial. Comprende esta última un estudio profundo y detallado en lo relacionado con la teoría y práctica utilizada y ejercida actualmente en las actividades de exploración y explotación de minas e hidrocarburos. Se trata también todo lo referente al tema procesal para lo concerniente a negociaciones, servidumbres y expropiaciones, así como la claridad en cuanto a la vigencia y correcta interpretación de sus normas. De igual modo, se aplica la misma metodología para el estudio dedicado al sector energético en los temas de servidumbre y expropiación. Este libro se ha enfocado a servir de guía legal y conceptual para quienes ejercen las prácticas minera, petrolera y energética, y para todos los interesados en los temas históricos relacionados con éstas y que son de suma importancia para su ejercicio.

Afrolatinidad y globalización : perspectiva étnica de la globalización. Estudio de caso : Proyecto Minero Mande Norte entre los municipios colombianos del Carmen del Darien y Murindó

El fenómeno de la globalización es una realidad que caracteriza la política internacional mundial que hace referencia principalmente a los procesos económicos, y a las innovaciones tecnológicas, sociales y culturales que están transformando nuestra manera de percibir e interpretar el mundo. En Colombia se han dado cambios muy importantes para el reconocimiento de los derechos de los grupos afrocolombianos. Uno de los cambios importantes, es el derecho de las comunidades afrocolombianas en cuanto a su desarrollo social, cultural y económico. Dentro del contexto nacional, el Pacifico colombiano es un territorio caracterizado por ser un polo de desarrollo, una región reconocida por su riqueza biológica y cultural, donde se realizan grandes proyectos de desarrollo y de extracción de recursos naturales. Pero estos proyectos tiene una alta incidencia en la pérdida de control de las comunidades sobre su territorio e incluso sobre su propio destino. La Muriel Minning Company es una multinacional de los Estados Unidos que actualmente desarrolla el Mega proyecto minero "Mandé Norte"; el gobierno colombiano le otorgó nueve títulos mineros para explotar y comercializar las reservas de cobre y los subproductos de oro y molibdeno. Colombia, como muchos otros países del sur, esta siendo fuertemente afectada en términos de diversidad cultural, construcción de sociedades sustentables y preservación del medio ambiente, por la intervención que en nuestros territorios hacen las multinacionales a través de megaproyectos, que sólo están generando pobreza, perdida de la diversidad cultural y biológica, deterioro de las condiciones ambientales sustentables, desplazamiento forzado.

Thanatos Empresarial : muerte empresarial en el sector minero causas y consecuencias

Este trabajo hace parte del proyecto de investigación de Thanatos Empresarial, el propósito del tema fue seleccionado con el fin de encontrar un factor o patrón común existente entre las empresas del sector minero colombiano, teniendo en cuenta aquellas que hayan sido liquidadas, estén cursando un proceso de liquidación obligatoria o aun estén desarrollando actividades. El trabajo fue dividido en tres partes principales. En la primera expresamos la problemática que cursa el país por la mortalidad prematura de empresas en el país, problemática que en lugar de disminuir sigue aumentando, pese a que desde hace más de cuatro décadas se han venido creando y modernizando leyes que buscan fomentar la creación de empresas sostenibles y de la misma manera ayudar a aquellas que se vean en la necesidad de entrar en un proceso de liquidación. La segunda parte de la investigación esta nutrida de datos recogidos por entidades, principalmente del estado, durante los últimos 15 años, por medio de los cuales se puede ver detalladamente las cifras de empresas que han venido entrando a procesos de liquidación, concordato, reorganización etc. y como pese a las leyes, muy pocas son las que logran sobrevivir a este proceso. Los resultados obtenidos mediante el análisis de estos datos corroboran de manera precisa esta premisa, las leyes existentes no están siendo suficientes para frenar la mortalidad de empresas en lo que respecta al sector minero nacional. Las empresas no toman decisiones por si solas, al mando de ellas están diferentes personas que como capitanes de un barco dirigen el rumbo de la misma, dependiendo de qué decisiones se tomen desde la dirección y la gerencia la empresa lograra recorrer el camino del éxito o del fracaso. Lamentablemente muchos de los emprendedores colombianos deciden dirigir su compañía sin buscar ayuda de algunos estamentos que fueron creados para ayudarlos y evitar la crisis de las empresas, tales como las cámaras de comercio, y por lo mismo debido a su inexperiencia o al abuso de toma de decisiones arriesgadas terminan por echar por la borda la empresa y poniendo en dificultades a todos los que de una u otra forma interactuaban con esta. Esta investigación cobra importancia cuando aquellas personas que desean crear empresa, buscan informarse con anterioridad sobre los problemas pueden cursar cuando entren en el mercado, encontrando en este trabajo una herramienta valiosísima en la gestión de la crisis la cual hace las veces de guía para evitar repetir el patrón que causa la muerte prematura de muchas empresas en el sector minero y en general en la economía Colombiana.