Growth and evolution of Precambrian continental crust in the southwestern Tarim terrane: New evidence from the ca. 1.4 Ga A-type granites and Paleoproterozoic intrusive complex
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- 作者：Xian-Tao Yea ; b ; Chuan-Lin Zhangb ; zchuanlin1968@gmail.com" class="auth_mail" title="E-mail the corresponding author ; M. Santoshc ; d ; Jian Zhange ; Xian-Ke Fanb ; Ji-Jun Zhangf
- 关键词：Zircon geochronology ; Nd&ndash ; Hf&ndash ; O isotopes ; Geochemistry ; Crustal growth ; Tarim Craton
- 刊名：Precambrian Research
- 出版年：2016
- 出版时间：April 2016
- 年：2016
- 卷：275
- 期：Complete
- 页码：18-34
- 全文大小：7911 K
文摘
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The 1.4 Ga A-type granites were likely related to breakup of Columbia supercontinent.
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The crustal growth of southern Tarim terrane at 2.3–2.5 Ga, 3.3 Ga and 3.6–3.8 Ga.
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The early Precambrian basement of the Tarim Craton was composed of discrete terranes.