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19:12 Jul 8, 2008 |
Spanish to English translations [PRO] Science - Geology / geological report | |||||||
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| Selected response from: liz askew United Kingdom Local time: 08:51 | ||||||
Grading comment
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Summary of answers provided | ||||
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4 +1 | overthrusts |
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4 +1 | thrust faults |
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Discussion entries: 1 | |
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overthrusts Explanation: Diccionario Politécnico de las Lenguas Española e Inglesa. |
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thrust faults Explanation: [PDF] ANNUAL INFORMATION FORM File Format: PDF/Adobe Acrobat - View as HTML its par, the Unidad Tectónica de Pliegues y Sobreescurrimientos (Tectonic Unit of Folds and Thrust Faults; Wilson. and Reyes, 1967) do not affect the ... www.infomine.com/index/pr/Pa068564.PDF - Similar pages -------------------------------------------------- Note added at 7 mins (2008-07-08 19:20:34 GMT) -------------------------------------------------- RESUMEN Sobre un basamento intrusivo metamórfico, afloran unidades sedimentarias de edades que van desde el Paleozoico hasta el Cenozoico, las rocas están afectadas por un estilo estructural dominante de pliegues anchos y largos de dirección andina, relacionados a fallas inversas de sobreescurrimientos regionales con vergencia hacia el Este. En su historia geológica, se han reconocido tectonismos expansivos y compresivos que han influenciado en la litología de los sedimentos, en la formación de altos y bajos estructurales, en la inversión tectónica y en la ausencia de algunas unidades estratigráficas; asimismo, se han determinado que algunas formaciones son potencialmente generadoras de hidrocarburos y otras con porosidad visual como buenas rocas reservorios. Además, existen algunas estructuras favorables para el entrampamiento de fluidos que deben ser confirmadas con sísmica. Palabras clave: Sobreescurrimiento, tectonismo, subducción. ABSTRACT Over a metamorphic intrusive basement, outcrop sedimentaries units that are from Paleozoic age until Cenozoic age; these rocks are deformed by a dominant structural style of wide and long fold of andean direction, related with thrust faults regionals with slope toward Est. In its geological history, it was recognized expansive and compresive tectonics, that have had some influency on lithologic sediments, in the upper and lower structural formations, in the inverted tectonic and in the absence of some stratigraphic units. Likewise it was determined that some stratigraphic units are potencialy hidrocarburiferous source rocks and others with good visual porosity are reservoir rocks. In addition there are some favorable structures to entrap fluids, which mst be confirmed with seismic reflextion. Keywords: Thrust fault, tectonic, subduction. -------------------------------------------------- Note added at 8 mins (2008-07-08 19:21:26 GMT) -------------------------------------------------- Thrust fault FAQ Thrust faults are formed by compressive stresses, and therefore often form where two tectonic plates collide, for example where an oceanic plate is ... www.talkorigins.org/faqs/lewis/ - 57k - Cached - Similar pages |
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