作者: ShiFeng Wang , WeiLin Zhang , XiaoMin Fang , Shuang Dai , Oliver Kempf
DOI: 10.1007/S11434-008-0132-9
关键词:
摘要: The Zanda basin is one of the very important basins at the north slope of the Himalaya Range. Thus the study of the basin strata will provide critical information about the tectonic evolution of the Himalayan Orogenic Belt. 268 oriented block samples were collected in the 750-m-thick sections of the Zanda basin. The characteristic remanent magnetization (ChRM) was isolated that decays linearly to the origin between 500° C and 690° C for most studied samples. An age range of 9.5–2.6 Ma was estimated from the correlation between our …