Deep-water depositional mechanisms and significance for unconventional hydrocarbon exploration (Record no. 189602)

MARC details
000 -LEADER
fixed length control field 02423nab a2200253 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2016 xxu ing
041 ## - IDIOMA
Idioma Inglés
245 00 - TITULO
Título Deep-water depositional mechanisms and significance for unconventional hydrocarbon exploration
Subtítulo A case study from the lower Silurian Longmaxi shale in the southeastern Sichuan Basin
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. mayo 2016
270 ## - FECHA DE CARGA
Fecha de carga 04/07/2016 ; 04/07/2016
300 ## - DESCRIPCION FISICA
Otra extensión 21 p. ; 773-794
520 ## - RESUMEN, ETC
Resumen Transcripción del resumen del autor: The purpose of this work was to study the depositional mechanisms and significance of the Longmaxi shale in the Sichuan Basin in southern China. Seven lithofacies were identified based on the detailed observation of outcrops and cores using petrographic and scanning electron microscope examination of thin sections and other data analyses: (1) laminated calcareous mudstone, (2) laminated carbonaceous mudstone, (3) laminated silty mudstone, (4) laminated claystone, (5) laminated siliceous shale, (6) siltstone, and (7) massive mudstone. The laminated mudstone and laminated claystone originated from suspension deposition, and siliceous shale is associated with ocean upwelling, whereas massive mudstone and siltstone were primarily deposited by turbidity currents. The depositional mechanisms have a great effect on the source rock and reservoir properties. Suspension deposition near oceanic upwelling zones can provide favorable conditions for the production and preservation of organic matter and are thus conducive to the formation of high-quality source rocks (total organic carbon content up to 5.4%). The reservoir storage spaces are primarily interlaminated fractures and organic pores with good physical reservoir properties (high porosity, permeability, and brittle mineral content). Turbidity currents may carry a large quantity of oxygen to the seafloor, resulting in the oxidation of organic matter, which is unfavorable for its preservation. The lithofacies formed by turbidity currents have relatively low total organic carbon contents (average:
581 ## - ESTADO DE COLECCIÓN
Estado de colección 5
773 0# - CORRECCIÓN
Título AAPG Bulletin
Partes relacionadas 100
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Liang, Chao
9 (RLIN) 55415
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Jiang, Zaixing
9 (RLIN) 55416
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Cao, Yingchang
9 (RLIN) 55417
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Wu, Minghao
9 (RLIN) 55418
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Guo, Ling
9 (RLIN) 55419
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Zhang, Chunming
9 (RLIN) 40807
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 200061842   200061842 06/03/2026 Artículo de Revista


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