Registros del 1 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 Ver registro
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 Ver registro
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 Ver registro
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 Ver registro
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 Ver registro
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 Ver registro
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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