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深水沉积的动力学机制和响应

Process of Dynamics and Its Response of Deep-Water Sedimentation

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【作者】 王英民王海荣邱燕彭学超张文明李文成

【Author】 WANG Ying-min1 WANG Hai-rong1,2 QIU Yan3 PENG Xue-chao3 ZHANG Wen-ming1 LI Wen-cheng3(1.Key Laboratory of Education Ministry for Hydrocarbon Accumulation Mechanism,University of Petroleum,Beijing 102249;2.Basin and Reservoir Research Center,University of Petroleum,Beijing 102249;3.Institute of Guangzhou Marine Geological Survey,Guangzhou 510760)

【机构】 中国石油大学石油天然气成藏机理教育部重点实验室广州海洋地质调查局区域地质调查所广州海洋地质调查局区域地质调查所 北京102249北京102249中国石油大学盆地与油藏研究中心北京102249广州510760北京102249

【摘要】 深水环境动力机制极为复杂,重力(流)机制类型多样且可能呈有序演化。底流包括温盐循环驱动的底流、风驱底流,以及顺峡谷上下运动的潮汐底流等;而内波可能也为重要的地质营力。在这些机制或孤立、或互动作用下,深水环境发育的沉积物类型、成因也极为复杂,它们具有重要的古气候、油气意义。

【Abstract】 Various processes operate deep-water environment and interplay in very complex way.Gravity(or gravity current)process may act in a variety of ways and systematic evolution may happen between them.Bottom currents(commonly refer as contour current)include those driven by thermocline circulation,those driven by wind,and tidal bottom current running up and down in canyons.Internal wave may be one important geological forces.In all such processes acting either isolate or jointly the type and genesis of sediment of deep-water environment is very complex,and own potential palaeo-climate information and hydrocarbon perspective.

【基金】 国家自然科学基金(批准号:40572067)资助
  • 【文献出处】 沉积学报 ,Acta Sedimentologica Sinica , 编辑部邮箱 ,2007年04期
  • 【分类号】P512.22
  • 【被引频次】60
  • 【下载频次】1691
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