陆相断陷湖盆层序构型与砂体发育分布特征

doi:10.11743/ogg20220402

Abstract

Abstract:

Efficient oil and gas exploration and development in petroliferous continental rift basins relies heavily on a profound understanding of sequence stratigraphic architectures and sandbody distribution characteristics in different tectonic evolution stages. Based on a review of the development status of sequence stratigraphy and geological characteristics of continental rift basins， this study characterizes the sequence stratigraphic architectures and sandbody distribution according to a four-stage tectonic evolution of the basins： ① During the early syn-rift stage， faulting at basin boundaries starts with parasequences being vertically aggraded and superposed， and with near-source coarse-grained depositional systems including alluvial fan， distributary channel， and fan delta being developed. ② During the main syn-rift stage， faulting intensifies with parasequences showing a variety of overlapping styles in different structural belts and systems tracts， and basins fill mainly with fluvial， delta and gravity flow. ③ During the transition stage from rifting to depression， faulting starts to wean with parasequences being overlapped and dominated by progradation and aggradation， and depositional systems dominated by axial fluvial and deltaic depositional systems being developed. ④ During the post-rift depression and subsidence stage， faulting nearly ends with basins in an overcompens and with the fluvial-shallow-water deltas being developed. Current hot topics and future development of sequence stratigraphy in continental rift basins are also discussed based on the above analyses.

Key words: sequence architecture, sandbody distribution, tectonic evolution stage, depositional system, sequence stratigraphy, continental rift basin

CLC Number:

TE121.3

Xiaomin Zhu, Hehe Chen, Jiawang Ge, Mingxuan Tan, Qianghu Liu, Zili Zhang, Yaxiong Zhang. Characterization of sequence architectures and sandbody distribution in continental rift basins[J]. Oil & Gas Geology, 2022, 43(4): 746-762.

Figures/Tables 2

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Characterization of sequence architectures and sandbody distribution in continental rift basins

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