THE LOWER SILURIAN CONTOURITE AND ITS GEOLOGICAL IMPLICATION IN CENTRAL ANHUI PROVINCE  

作　　者：姜在兴 赵澂林 熊继辉 

机构地区：[1]University of Petroleum, Dongying 257062, PRC

出　　处：《Chinese Science Bulletin》1990年第13期1101-1104,共4页

摘　　要：Ⅰ. INTRODUCTIONThe study area is located at the northern mountains of Chaohu City in central Anhui Province. The Silurian system, consisting of the lower series Gaojiabian and the middle series Fentou formation with total thickness over 570 m, is parallelly unconformably overlain and underlain by Ordovician Maoshan formation and Silurian Wutong formation, respectively. The contourite or contour current deposit occurs at the lower Craojiabian formation.

关 键 词：CONTOURITE CHARACTERS significance. 

分 类 号：N[自然科学总论]