The Cenozoic kinematics of Qatar: Evidence for high-angle faulting along the Dukhan ‘anticline’
作者： John M. Rivers , Kyle P. Larson
DOI: 10.1016/J.MARPETGEO.2018.03.034
关键词:
摘要: Abstract New geological mapping and observations made across Qatar favor a fault-controlled model for the Dukhan structure in western part of peninsula over previous fold-related regional erosion models. Regional stratigraphic relationships sedimentology record significant fault-localized accommodation development. This Miocene basin development may reflect far-field extension foreland coeval thrusting Oman. The subsequent change tectonics to convergence Zagros front is interpreted have led inversion present-day topography outcrop distribution.
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