Petroleum accumulations and inversion structures in the Xihu Depression, East China Sea Basin (Record no. 186153)

MARC details
000 -LEADER
fixed length control field 02903nab a2200217 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2011 xxu ing
041 ## - IDIOMA
Idioma Inglés
245 00 - TITULO
Título Petroleum accumulations and inversion structures in the Xihu Depression, East China Sea Basin
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. oct. 2011
270 ## - FECHA DE CARGA
Fecha de carga 13/10/2011 ; 13/10/2011
300 ## - DESCRIPCION FISICA
Otra extensión 12 p. ; 429-440
520 ## - RESUMEN, ETC
Resumen Transcripción del resumend el autor. The central inversion zone in the Xihu Depression, East China Sea, was formed during the Late Miocene and inversion here involves the entire Tertiary succession, nearly 10,000 m thick. Lithologically, the succession is composed mainly of sandstones and mudstones with minor coals and limestones. Hydrocarbons are present in a series of structural traps which formed as a result of the inversion process. Oil and gas exploration in the Xihu Depression has demonstrated that at least 90% of the commercial reserves so far found occur in inversion-related structural traps in the Eocene Pinghu Formation and Oligocene Huagang Formation (with minor reserves in Miocene strata) in the central inversion zone. The main reservoir lithology is sandstone. Studies have also confirmed that effective structural traps are controlled by the strength and style of inversion tectonics. However, the relationship between the geometry, kinematics and magnitude of the inversion structures and the oil and gas accumulations is not well understood. Based on 2D reflection seismic results and data from several wells, factors influencing the accumulation of hydrocarbons in the study area are considered, and include inversion fault activity rate, inversion ratio and the thickness of sediments eroded. The results show that the best exploration targets are located in the southern part of the central inversion zone. This area has a relatively low inversion fault activity rate (average 3.0 m/Ma), a low inversion ratio (average 0.4), and a relatively small thickness of sediments were eroded from the Miocene Longjing and Liulang Formation (=400 m) and Eocene Pinghu Formation. By contrast, the northern part of the inversion zone has a relatively high inversion fault activity rate (average 6.8 m/Ma), a high inversion ratio (0.8), and greater thicknesses were eroded (400 m to 1200 m). This may have resulted in the less favourable preservation conditions and the large-scale leakage of oil and gas. An analysis of the relationship between the inversion-related structural traps and hydrocarbon accumulations shows that most oil and gas accumulations occur in the southern part of the central inversion zone, especially in the Longjing, Liulang and Pinghu Formations.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 4
773 0# - CORRECCIÓN
Título Journal of Petroleum Geology
Partes relacionadas 34
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Yang, F.-L.
9 (RLIN) 51945
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Xu, X.
9 (RLIN) 51946
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Zhao, W.-F.
9 (RLIN) 51947
Holdings
Biblioteca propietaria Biblioteca actual Fecha de adquisición Inventario Total de préstamos Inventario Fecha de carga Tipo de item KOHA
Biblioteca Alejandro Angel Bulgheroni Biblioteca Alejandro Angel Bulgheroni 06/03/2026 200058246   200058246 06/03/2026 Artículo de Revista


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