000			01898nmc a2200205 4500
005			20260520010443.0
008			260224s xxu
040			_aBAAB
082			_a068.82 553.28 C62 15730
100	1		_aDoiny Cabré, Juan Pedro
100	1		_aFumarola, Lara Azul
111	2		_aCongreso de Exploración y Desarrollo de Hidrocarburos (11er : 2022 nov. 8 - 11 : Mendoza)
245	0	0	_aCARACTERIZACIÓN Y MODELADO ESTRUCTURAL DE LOS ANTICLINALES CASHIRIARI Y SAN MARTÍN EN LA FAJA PLEGADA Y CORRIDA DE CAMISEA, ANDES CENTRALES, PERÚ
270			_a15/08/2023 ; 15/08/2023
300			_a16 p. ; 317-331
520			_aThe Camisea fold and thrust belt, located in the southern Ucayali Basin, has been extensively studied due to its important hydrocarbon accumulations. High-quality 3D depth-migrated seismic data allows the identifica-tion of five structural trends in a thin-skinned fold and thrust belt. The main structures are north-verging thrusts with a basal detachment that deepens southward. The San Martin and Cashiriari anticlines, which are the focus of this work, are interpreted as fault-bend folds. In order to analyze along-strike variations of these structures, four cross-sections were made. Besides the north-verging thrusts, high angle reverse faults with opposite vergence can be identified. The analysis of the crosscutting relationships between the different structures allows us to define a sequence of deformation in which the high angle reverse faults precede and are cut by the main north-verging thrusts. A kinematic evolution of the structure is presented in order to verify the correct restoration and validate the structural cross-section interpretation.
856			_uhttps://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2022/GeologíaEstructural/geologia-estructural-y-tectonica15.PDF
942			_cCONGTP
945			_aDominguez, Silvia
999			_c195973 _d195973