Origin of the Early Cretaceous Trachyte in Northern Guangdong Province Constraints of Sr-Nd-Pb Isotopes
详细信息   
摘要

The trachyte in the Dachangsha basin of the northern Guangdong province was formed in the Early Cretaceous (SHRIMP zircon U-Pb dating shows an age of tracphyte as 135.3±1.5 Ma) . The Sr-Nd-Pb isotopic composition characteristics of tracphyte are discussed. The Sr-Nd, Sr-Pb, Nd-Pb and Pb-Pb relationship of the tracphyte suggests that the trachyte should be originated from partial melting of the young lower crust, while the lower crust should be influenced by metasomatism of fluids from dehydration of subducted upper crust, and there was no upper crust contamination in the process of magma rising.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700