Neoproterozoic subduction-related basaltic magmatism in the northern margin of the Tarim Craton: Implications for Rodinia reconstruction
详细信息 查看全文
- 作者：Qingyan Tanga ; Zhaowei Zhangb ; Chusi Lic ; cli@indiana.edu" class="auth_mail" title="E-mail the corresponding author ; Yalei Wangb ; Edward M. Ripleyc
- 关键词：Mafic-ultramafic rocks ; Mantle plume ; Subduction ; Tarim Craton ; Rodinia
- 刊名：Precambrian Research
- 出版年：2016
- 出版时间：November 2016
- 年：2016
- 卷：286
- 期：Complete
- 页码：370-378
- 全文大小：1976 K
文摘
- •
Neoproterozoic mafic-ultramafic rocks in N. Tarim were not produced by mantle plume.
- •
The temporal-spatial distribution of these rocks does not show a hotspot track.
- •
Whole rock chemical and isotopic compositions indicate that they are arc cumulates.
- •
Northern Tarim was part of the Neoproterozoic Circum-Rodinia Subduction System.