000			01776nab a2200205 4500
005			20260520000228.0
008			260224s2008 xxu
245	0	0	_aMajor structural elements of the Miocene section, Burgos Basin, northeastern Mexico
260			_a _b _cnov. 2008
270			_a01/02/2011 ; 01/02/2011
300			_a11 p. ; 1479-1499
520			_aTranscripción del resumen del autor. Major Miocene structural elements of the Burgos Basin include a regionwide detachment system that connects extensional fault systems throughout the basin with an active diapir belt downdip, a regionwide pattern of downthrown extensional rollover folds, pervasive secondary faults, and salt and shale diapiric masses in the eastern part of the basin. An interpretation of two-dimensional seismic data suggests that the Burgos Basin Miocene section can be divided into four structural domains: expanded zone, Lamprea trend, Corsair-Wanda trend, and diapir belt. The westernmost unexpanded zone is the footwall of the expanded system part of the basin, which overlies a domain of Oligocene extension. Remaining trends represent an extensional accommodation related to the basinward migration of mobile salt and shale, which has produced a relatively uniform structural style in the Miocene section. The structural style observed in the Burgos Basin appears to define a transitional zone between gravitational collapse in the offshore Laguna Madre-Tuxpan shelf to the south and salt-related raft tectonics of the south Texas Gulf Coast.
581			_a11
773	0		_tAAPG Bulletin _g92
942			_cARTICULO
100	1		_aHernández-Mendoza, Javier J. _944405
100	1		_aDeAngelo, Michael V. _944406
100	1		_aWawrzyniec, Tim F. _936588
999			_c173107 _d173107