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二连盆地重磁异常地质意义及上古生界结构认识

Geological implications of gravity and magnetic anomalies in Erlian Basin and understanding of Upper Paleozoic structures

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【作者】 宋景明金凤鸣王玉青孙朝辉高林姚欢赵荔刘喜恒时聪

【Author】 Song Jingming1,Jin Fengming2,Wang Yuqing1,Sun Zhaohui2,Gao Lin1,Yao Huan2,Zhao Li1,Liu Xiheng2 and Shi Cong2.1.BGP Inc.,CNPC,Zhuozhou,Hebei 072750,China2.Huabei Oilfield Ltd.,PetroChina,Renqiu,Hebei 062552,China

【机构】 中国石油集团东方地球物理公司中国石油华北油田公司

【摘要】 二连盆地为我国一个中型油气区。本文在对研究区重磁资料统一拼接、处理基础上,通过分析重磁资料反映的地质结构信息,结合区域地震资料,推断了该区上古生界地质结构。综合研究认为,二连盆地上古生界受深大断裂控制,在西拉木伦河断裂以北上古生界残余厚度较大,并形成两个厚度中心,即二连—苏尼特右旗厚度中心和西乌珠穆沁旗—东乌珠穆沁旗厚度中心。前者厚度为3000m,后者上古生界厚度大、分布广,最厚可达6300m,是后续研究的重要目标区。

【Abstract】 Erlian Basin is a middle-scale oilfiled of China.Our work in the basin is as follows:merging and process gravity and magnetic data acquired in the basin,analyzing the geological implications of the data,and finally predicting Upper Paleozoic structures together with available seismic data.The comprehensive study concludes that Upper Paleozoic formations are dominantly controlled by big deep faults in the basin.In the north of the Xilamulun-River fault,the residual Upper Paleozoic formations have the big thickness.There are two thickness centers,i.e.Erlian-Suyouqi Zone and Xiwuqi-Dongwuqi Zone.The maximum thickness of the former is about 3000 m,and the maximum thickness of the later is about 6300 m.Both of them have not only big thickness but also a wide coverage,and are considered as future potential targets.

【基金】 国土资源部油气专项(第二批)“二连盆地上古生界石油地质特征及战略选区”(2009GYXQ12-03)资助
  • 【文献出处】 石油地球物理勘探 ,Oil Geophysical Prospecting , 编辑部邮箱 ,2012年S1期
  • 【分类号】P618.13
  • 【被引频次】4
  • 【下载频次】197
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