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陆架边缘三角洲研究进展及实例分析

朱筱敏 葛家旺 赵宏超 袁立忠 刘军

沉积学报2017,Vol.35Issue(5):945-957,13.
沉积学报2017,Vol.35Issue(5):945-957,13.DOI:10.14027/j.cnki.cjxb.2017.05.007

陆架边缘三角洲研究进展及实例分析

Development of Shelf-edge Delta Researches and Typical Case Analyses

朱筱敏 1葛家旺 1赵宏超 1袁立忠 2刘军2

作者信息

  • 1. 中国石油大学(北京)地球科学学院,北京 102249
  • 2. 中海石油(中国)深圳分公司研究院,广东深圳 518067
  • 折叠

摘要

Abstract

Since last century nineties,a special marine delta named shelf-edge delta widely developed at the margin of the shelf has been an international interest and new field for petroleum exploration, which is commonly character-ized by thick-bedded sand-rich deposits, large-scaled distribution, high porosity and perfect petroleum accumulation conditions associated with marine slope or deep-water fan deposits. The shelf-edge delta is usually developed during the falling stage or low-stand stage of sea-level,influenced by the slope tectonic structures.However,it can also occur during the high-stand stage,comprehensively controlled by sediment supply,accommodation space and climate condi-tions,and sometimes of wave or tide influence. Previous studies have extensively indicated that the deepwater sedi-mentation prediction based on shelf-slope clinoform growth model is similar to the shelf edge trajectory migration motif. Steeply rising shelf-edge trajectories and dominantly aggradational stacking patterns are fronted by large-scale mass-transport systems,while, flat to slightly falling shelf-edge trajectories and progradational and downstepping stacking patterns are empirically related to large-scale submarine fan systems associated sand-rich gravity flows. Slightly rising shelf-edge trajectories and progradational and aggradational stacking patterns are associated with mixed sand/mud gravity flows and moderate-scale slope-sand deposits. Abundant examples have been identified that the sand-rich de-posits of shelf-edge delta and deep-water fan systems serve a perfect source-reservoir-capping condition, prove to be good petroleum exploration targets. A large-scale and thick-bedded Oligocene shelf-edge delta deposits are observed in the Heshan Depression of Pearl River Mouth basin, northern slope of the South China Sea, in response to the suffi-cient sediment supply from the ancient Pearl River with a slow tectonic subsidence. Associated with the migration of shelf edge,the sigmoid seismic progradations of shelf-edge delta are significantly seaward prograded. The occurrence of incised valley and large scale submarine fan systems during the late Oligocene times,together with observed seismic reflection geometries suggest the development of flat to slightly falling shelf-edge trajectories and progradational and downstepping stacking patterns in the Heshan Depression. The related thick-bedded submarine fan systems associated sand-rich deposits are important and potential strategic oil and gas exploration targets in the future.

关键词

陆架边缘三角洲/深水扇/主控因素/预测模型/鹤山凹陷/南海北部

Key words

shelf-edge delta/deep-water fan/controlling factors/predication model/Heshan Depression/Northern South China Sea

分类

天文与地球科学

引用本文复制引用

朱筱敏,葛家旺,赵宏超,袁立忠,刘军..陆架边缘三角洲研究进展及实例分析[J].沉积学报,2017,35(5):945-957,13.

基金项目

国家科技重大专项子项目(2011ZX05025-005-02) (2011ZX05025-005-02)

国家自然科学基金项目(41272133) National Science and Technology Major Project, No. 2011ZX05025-005-02 (41272133)

National Natural Science Foundation of China,No. 41272133 ()

沉积学报

OA北大核心CSCDCSTPCD

1000-0550

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