Article ID Journal Published Year Pages File Type
4682486 Journal of South American Earth Sciences 2012 7 Pages PDF
Abstract
► We investigated the deep structure of the Venezuelan Andes from a 3D geological model. ► The 3D model clearly displays the 3D shape and organisation of the main faults. ► The partitioning and the tectonic escape of the belt are explained by a single process of orogenic float. ► The upper crustal part of the Venezuelan Andes are decoupled from the underlying lithosphere above a horizontal décollement level.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth and Planetary Sciences (General)
Authors
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