Recycling of ancient subduction-modified mantle domains in the Purang ophiolite (southwestern Tibet)
详细信息    查看全文
文摘

The Purang peridotites are not the complementary mantle residues of spatially associated oceanic crust.

The Purang peridotites may represent ancient subduction-modified SCLM domains.

The Purang peridotites have been rejuvenated by late-stage percolating N-MORB melts.

A deep mantle recycling model is preferred to reconcile the presence of SuR-UHP mineral assemblages.

© 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