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| 楚雄盆地构造演化及其对油气聚集的控制 | |
| 引用本文： | 杨庆道,王伟锋,吴思卫,李继白,刘传山,潘博.楚雄盆地构造演化及其对油气聚集的控制[J].中国石油勘探,2011,16(4):29-36. |
| 作者姓名： | 杨庆道 王伟锋 吴思卫 李继白 刘传山 潘博 |
| 作者单位： | 1. 中国石油大学(华东)地球资源与信息学院,山东省青岛市266555;中国石化西南石油局云南物探公司,云南省昆明市650233 2. 中国石油大学(华东)地球资源与信息学院,山东省青岛市,266555 3. 中国石化油田企业经营管理部,北京,100728 4. 中国石化西南石油局云南物探公司,云南省昆明市,650233 |
| 摘 要： | 楚雄盆地位于扬子板块的西南缘.红河断裂控制盆地的西南边界,断裂走向在该区域发生大角度转折,由华南地区的北西西向变为研究区的北西向,再到青藏高原变为北西西向.中生代以来,除了受到来自西南部的印度板块北移过程中北北东向持续挤压应力外,由于金沙江-红河断裂的存在,并从燕山期以来多次转换、传递来自中国东部滨太平洋构造域的板块向... |
| 关 键 词： | 楚雄盆地 构造 构造特征 构造演化 油气聚集 控制 |
Tectonic Evolution of Chuxiong Basin and Its Control on Hydrocarbon Accumulation |
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| Yang Qingdao,Wang Weifeng,Wu Siwei,Li Jibai,Liu Chuanshan,Pan Bo .College of Geo-Resources , Information of China University of Petroleum,Qingdao City,Sh,ong Province ,.Yunna Geophysical Company of Southeast Petroleum Bureau,SINOPEC,Kunming City,Yunnan Province ,.Oilfield Management.Tectonic Evolution of Chuxiong Basin and Its Control on Hydrocarbon Accumulation[J].China Petroleum Exploration,2011,16(4):29-36. | |
| Authors: | Yang Qingdao Wang Weifeng Wu Siwei Li Jibai Liu Chuanshan Pan Bo College of Geo-Resources Information of China University of Petroleum Qingdao City Sh ong Province Yunna Geophysical Company of Southeast Petroleum Bureau SINOPEC Kunming City Yunnan Province Oilfield Management |
| Affiliation: | Yang Qingdao1,2,Wang Weifeng1,Wu Siwei3,Li Jibai2,Liu Chuanshan2,Pan Bo2 1.College of Geo-Resources and Information of China University of Petroleum,Qingdao City,Shandong Province 266555,2.Yunna Geophysical Company of Southeast Petroleum Bureau,SINOPEC,Kunming City,Yunnan Province 650023,3.Oilfield Management Department of SINOPEC,Beijing 100728 |
| Abstract: | Chuxiong Basin is located at the southwest margin of Yangtze tectonic plate.The Red River fracture controls the southwest boundary of the Basin with a high angle transition from NWW in the southeast to NW of study area,then NWW again in the Qinghai-Tibet Plateau.Maximum principal stress orientation in the Basin has changed several times since Mesozoic from nearly SN to EW,the Red River fault has undergone left-lateral or right-lateral strike-slip movement,accompanied by internal block rotating,due to the co... |
| Keywords: | Chuxiong Basin tectonic tectonic characteristics tectonic evolution hydrocarbon accumulation control |
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