Instituto Geológico y Minero de España

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Instituto Geológico y Minero de España
 Registros del al 7 de 7 encontrados

1.-  Cenozoic deformation front evolution, depocenter distribution and paleogeography of the Magdalena Valley, Eastern Cordillera and Llanos Basin of Colombia; implications for reservoir distribution
American Association of Petroleum Geologists and Society for Sedimentary Geology; Tulsa, OK; USA; Un, 2012
2012 AAPG annual convention & exhibition; abstracts volume
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2.-  Depositional and provenance record of the Paleogene transition from foreland to hinterland basin evolution during Andean orogenesis, northern middle Magdalena Valley basin, Colombia
Elsevier; Oxford; GBR; United Kingdom, 2011
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3.-  Factors controlling selective abandonment and reactivation in thick-skin orogens; a case study in the Magdalena Valley, Colombia
Geological Society of London; London; GBR; United Kingdom, 2013
Thick-skin-dominated orogens; from initial inversion to full accretion
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4.-  Integrated provenance analysis of a convergent retroarc foreland system; U/Pb ages, heavy minerals, Nd isotopes, and sandstone compositions of the middle Magdalena Valley basin, Northern Andes, Colombia
Elsevier; Amsterdam; NLD; Netherlands, 2012
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5.-  Inversion tectonics under increasing rates of shortening and sedimentation; Cenozoic example from the Eastern Cordillera of Colombia
Geological Society of London; London; GBR; United Kingdom, 2013
Thick-skin-dominated orogens; from initial inversion to full accretion
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6.-  Onset of fault reactivation in the Eastern Cordillera of Colombia and proximal Llanos Basin; response to Caribbean-South American convergence in early Palaeogene time
Geological Society of London; London; GBR; United Kingdom, 2013
Thick-skin-dominated orogens; from initial inversion to full accretion
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7.-  Tectonic controls on sedimentation in an intermontane hinterland basin adjacent to inversion structures; the Nuevo Mundo Syncline, middle Magdalena Valley, Colombia
Geological Society of London; London; GBR; United Kingdom, 2013
Thick-skin-dominated orogens; from initial inversion to full accretion
Ver registro


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