1887

Abstract

Compressive structures have been identified , along the Serranía del Interior Oriental Range foothills, using 2D<br>seismic reflexion profiles, recorded by PDVSA. Major tectonic elements, shown are: Urica fault, Tala - Pirital<br>thrusts and the Mud-diapir trend. Thrusts and associated ramps occurred during the Late Miocene - Pliocene.<br>Extensional features to the east, might have been triggered during the last 5 Ma. by remobilisation of lower<br>Miocene shale.

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/content/papers/10.3997/2214-4609-pdb.215.sbgf428
1999-08-15
2020-04-04
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.215.sbgf428
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