The Late Paleozoic Radiolarian Cherts in Southern Guangxi and Preliminary Exploration on Paleo-Tethys in Guangxi  

作　　者：吴浩若 邝国敦 咸向阳 李日俊 王忠诚 

机构地区：[1]Institute of Geology, Academia Sinica, Beijing 100029, PRC [2]Institute of Geology, Academia Sinica, Beijing 100029, PRC Guangxi Institute of Geology,Nanning 530023,PRC

出　　处：《Chinese Science Bulletin》1994年第12期1025-1029,共5页

基　　金：Project supported by the National Natural Science Foundation of China ;the Laboratory of Lithosphere Tectonic Evolution, Institute of Geology, Academia Sinica.

摘　　要：The existence of the Paleo-Tethys in western Yunnan has generally beenrecognized as the progress in geological studies there during the last decade.Recently, Japanese geologists proposed that the Carboniferous-Permian volcanic arcand seamount rock associations in Japan originated from the low-latitudeProto-Pacific realm, and their northward migration seems to have started in or afterthe Triassic times. Then the very interesting problems are facing us: how does

关 键 词：chert radiolana GUANGXI PALEO-TETHYS Proto-Pacific. 

分 类 号：Q915[天文地球—古生物学与地层学]