孙吴—嘉荫盆地淘淇河组湖底扇沉积特征

2009年 31卷 第3期
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SEDIMENTARY CHARACTERISTICS OF SUBLACUSTRINE FAN OF TAOQIHE FORMATION OF LOW CRETACEOUS IN SUNWU-JIAYIN BASIN
张雷1,2 刘招君2 杨婷1 杜江峰2 侯伟3
ZHANG Lei1,2 LIU Zhao-jun2 YANG Ting1 DU Jiang-feng2 HOU Wei3
1.中国石油大学资源与信息学院,北京 昌平 102249; 2.吉林大学地球科学学院,吉林 长春 130061
1.College of Resources and Information,China University of Petroleum,Changping Beijing 102249,China;2.College of Earth Sciences,Jilin University,Changchun Jilin 130061,China
孙吴—嘉荫盆地; 沾河断陷; 淘淇河组; 湖底扇; 沉积特征; 石油地质意义;
Sunwu-Jiayin Basin; Zhanhe Rift; Taoqihe Formation; Sublacutrine fan; sedimentary characteristic; significance of petroleum geological;
10.3863/j.issn.1674-5086.2009.03.013