中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Sublacustrine gravity-induced deposits: The diversity of external geometries and origins

文献类型:期刊论文

作者Pan, Shuxin1; Liu, Huaqing1; Xu, Duonian1; Wei, Pingsheng1; Qu, Yongqiang1; Guan, Xin1; Liu, Caiyan1; Zhang, Shuncun2
刊名SEDIMENTARY GEOLOGY
出版日期2020-09-01
卷号407页码:17
关键词Gravity-induced deposits External geometry MTDs Hyperpycnal flows Lake-floor topography The Songliao Basin
ISSN号0037-0738
DOI10.1016/j.sedgeo.2020.105738
英文摘要Our current knowledge of deep-water depositional systems is mainly built of extensive achievements obtained from marine basins. Although lacustrine basins are important oil & gas productive areas of the world, gravity-induced deposits in these basins are poorly understood in the literature when compared with those documented in marine basins. Based on new insights from 3D seismic data, this paper attempts to investigate the effect of the interaction between gravity-induced flows and lake-floor topography on the resulting external geometry of gravity-induced deposits in the Cretaceous Qingshankou and Nenjiang formations of the Songliao Basin (SLB). Eight different shapes of gravity-induced deposits were identified in the SLB, and which were in turn grouped into four distinct categories according to external shape, internal architecture and spatial assembly: (1) Channel-fan complexes; (2) Fan-form complexes; (3) Strip-form complexes; and (4) Pond-form complexes. Furthermore, fan-form complexes can be subdivided into four subcategories (isolated fan with compressional ridges, isolated fan without compressional ridges, mother-son fans and stacked fans). Strip-form complexes can be subdivided into two subcategories, including strip-form controlled by gully system and strip-form controlled by growth faults. Sediment transport mechanism (density flows or mass transport flows) and lake-floor topography together influence the pathways, runout distances, discharge places and internal characteristics of gravity induced deposits, which could ultimately influence external geometries of gravity-induced deposits in the SLB. Consequently, sublacustrine gravity-induced deposits does not exhibit classic fan-like geometry. Frequent and powerful hyperpycnal flows associated with flood events are fairly common, and develop channel-distal fan complexes. MTDs exhibit various external geometries, which are significantly affected by growth faults, slope gullies, gradient, and basin-floor irregularities. The new depositional model built from the SLB is vital to understanding the distribution of gravity-flow deposits in a sublacustrine slope. (C) 2020 Elsevier B.V. All rights reserved.
WOS关键词MASS-TRANSPORT COMPLEXES ; SEISMIC GEOMORPHOLOGY ; SONGLIAO BASIN ; SUBMARINE FANS ; TURBIDITE SYSTEMS ; HYPERPYCNAL FLOWS ; TECTONIC CONTROLS ; DEBRIS-FLOWS ; UPPER-SLOPE ; SEA-FLOOR
资助项目National Natural Science Foundation of China[41872116] ; National Natural Science Foundation of China[41772099] ; National Science and Technology Major Project[2017ZX05001-003]
WOS研究方向Geology
语种英语
WOS记录号WOS:000568166300005
出版者ELSEVIER
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project
源URL[http://ir.iggcas.ac.cn/handle/132A11/98224]  
专题地质与地球物理研究所_兰州油气中心
通讯作者Pan, Shuxin
作者单位1.PetroChina, Northwest Branch, Res Inst Petr Explorat & Dev, Lanzhou 730020, Peoples R China
2.Chinese Acad Sci, Key Lab Petr Resources Res, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714
Pan, Shuxin,Liu, Huaqing,Xu, Duonian,et al. Sublacustrine gravity-induced deposits: The diversity of external geometries and origins[J]. SEDIMENTARY GEOLOGY,2020,407:17.
APA Pan, Shuxin.,Liu, Huaqing.,Xu, Duonian.,Wei, Pingsheng.,Qu, Yongqiang.,...&Zhang, Shuncun.(2020).Sublacustrine gravity-induced deposits: The diversity of external geometries and origins.SEDIMENTARY GEOLOGY,407,17.
MLA Pan, Shuxin,et al."Sublacustrine gravity-induced deposits: The diversity of external geometries and origins".SEDIMENTARY GEOLOGY 407(2020):17.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。