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| 中扬子区海相地层油气成藏有利区层序样式分析 | |
| 引用本文： | 周雁,王成善,陈洪德,王正元,梁西文,文可东.中扬子区海相地层油气成藏有利区层序样式分析[J].沉积与特提斯地质,2002,22(1):22-29. |
| 作者姓名： | 周雁 王成善 陈洪德 王正元 梁西文 文可东 |
| 作者单位： | 1. 成都理工大学,油气地质及开发国家重点实验室,沉积地质研究所,四川,成都,610059;中国石化江汉油田分公司研究院,湖北,潜江,433124 2. 成都理工大学,油气地质及开发国家重点实验室,沉积地质研究所,四川,成都,610059 3. 中国石化江汉油田分公司研究院,湖北,潜江,433124 |
| 摘 要： | 通过中扬子区海相地层油气成藏背景的分析，成藏有用层序样式基本特征的研究和油成藏有利区的预测，笔者认为在具备盖层条件的前提下，有利区应该具备烃源条件和储集条件配置关系良好，一方面H型二级层序样式格架中海侵体系域烃源岩具备较多的T型三级层序或较少的H型三级层序；另一方面，H型二级层序样式格架中高位体系域储集岩具备较多的H型三级层序或较少的T型三级层序。中扬子区的古生界总体上保存条件优越，有利区主要位于湘鄂西、宜昌斜坡和江汉平原南部；上古生界总体上保存条件差异性明显，有利区主要位于渝东－鄂西区和江汉平原区。 |
| 关 键 词： | 层序地层 层序样式 海相沉积 油气勘探 扬子地块 海相地层 油气成藏 |
| 文章编号： | 1009-3850(2002)01-0022-08 |
| 收稿时间： | 2001/11/22 0:00:00 |
| 修稿时间： | 2001年11月22 |
Sequence patterns for the marine strata in potential oil and gas pools in the central Yangtze area |
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| ZHOU Yan,WANG Cheng-shan,CHEN Hong-de,WANG Zheng-yuan,LIANG Xi-wen,WEN Ke-dong.Sequence patterns for the marine strata in potential oil and gas pools in the central Yangtze area[J].Sedimentary Geology and Tethyan Geology,2002,22(1):22-29. | |
| Authors: | ZHOU Yan WANG Cheng-shan CHEN Hong-de WANG Zheng-yuan LIANG Xi-wen WEN Ke-dong |
| Institution: | 1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China;2. Research Institute of Oil Exploration and Development, Jianghan Oilfield Company, Qianjiang 433124, Hubei, China |
| Abstract: | The present paper discusses the sedimentary-tectonic settings of oil and gas accumulation in marine strata, sequence patterns for the marine strata and areas prospective for oil and gas pools in the central Yangtze area. Such an area should be well made up of source rocks, hydrocarbon reservoirs and seals. More precisely, the source rocks of the transgressive systems tract within the H-type second-order sequence framework consist of more T-type and/or less H-type third-order sequences, whereas the hydrocarbon reservoirs of the highstand systems tract within the H-type second-order sequence framework are composed of more H-type and/or less T-type third-order sequences. The potential areas in the Lower Palaeozoic strata include western Hunan and Hubei, Yichang slope, and southern Jianghan Plain, and those in the Upper Palaeozoic strata involve eastern Chongqing, western Hubei and Jianghan Plain. |
| Keywords: | sequence stratigraphy sequence patterns marine sediments oil and gas exploration Yangtze plate |
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