Paleoenvironmental Record from Wuqi Paleolake in Northern Chinese Loess Plateau  

作　　者：GUO Jiao WANG Wei WU Lijie CHEN Hongyun DONG Qiuyao 

机构地区：[1]Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2014年第S1期8-9,共2页地质学报（英文版）

基　　金：Project supported by the Geological Survey Project of China Geological Survey(Grant No.1212011120047)

摘　　要：Jinding core(ZK04,36°47′35.36″N,108°19′05.24″E)is located in the northern area of Luohe river basin,northern Chinese loess plateau,lying to the southeast of Wuqi County about 20 km.The total depth of Core ZK04 is 92.20Jinding core(ZK04,36°47′35.36″N,108°19′05.24″E)is located in the northern area of Luohe river basin,northern Chinese loess plateau,lying to the southeast of Wuqi County about 20 km.The total depth of Core ZK04 is 92.20

关 键 词：Wuqi paleolake magnetic susceptibility grain size paleomagnetic chronology PALEOENVIRONMENT Chinese Loess Plateau 

分 类 号：P532[天文地球—古生物学与地层学]