Detrital Zircon Provenance of Pliocene Yinggehai Formation in the Ledong Gas Field of the Yinggehai-Song Hong Basin  

作　　者：WANG Ce LIANG Xinquan FU Jiangang ZHOU Yun JIANG Ying DONG Chaoge 

机构地区：[1]State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences,Guangzhou 510640, China [2]University of Chinese Academy of Sciences, Beijing 100049, China [3]School of Earth Science, Guilin University of Technology, Guilin 541004, China

出　　处：《Acta Geologica Sinica(English Edition)》2015年第A01期279-280,共2页地质学报（英文版）

基　　金：financially supported by the National Science and Technology Major Project of China(No.2011ZX05023-004-11);the Nation Natural Science Foundation of China(Nos.40872080 and 41072081)

摘　　要：1 Introduction Over the past decades, a number of hydrocarbon reservoirs have been discovered in the deepwater area of the Yinggehai-Song Hong Basin, South China Sea. The NW-oriented Yinggehai-Song Hong Basin, located on the continental shelf at water depths of 50-200 m in the northwestern South China Sea, is one of the largest Cenozoic pull-part basins in the world.1 Introduction Over the past decades, a number of hydrocarbon reservoirs have been discovered in the deepwater area of the Yinggehai-Song Hong Basin, South China Sea. The NW-oriented Yinggehai-Song Hong Basin, located on the continental shelf at water depths of 50-200 m in the northwestern South China Sea, is one of the largest Cenozoic pull-part basins in the world.

分 类 号：P618.13[天文地球—矿床学]