The location and evolution of the tectonic boundary between the Paleoproterozoic Jiao-Liao-Ji Belt and the Longgang Block, northeast China
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- 作者：Chong Penga ; pengchong13@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Lin-Fu Xuea ; pc512516@163.com" class="auth_mail" title="E-mail the corresponding author ; Ming Zhua ; zhuming13@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Yuan Chaia ; chaiyuan13@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Wen-Yu Liub ; 605027525@qq.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：North China Craton ; Jiao-Liao-Ji Belt ; Longgang Block ; Fault ; Non-seismic geophysical ; Tectonic boundary
- 刊名：Precambrian Research
- 出版年：2016
- 出版时间：January 2016
- 年：2016
- 卷：272
- 期：Complete
- 页码：18-38
- 全文大小：9703 K
文摘
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Tectonic boundary between the Jiao-Liao-Ji Belt and the Longgang Block is identified.
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The basin-controlling boundary fault indicates a continental rift or rift-and-collision belt.
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The Lianshanguan rock mass contains Archean TTG gneiss and Paleoproterozoic granite.
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The Eastern Block can be regarded as a micro-block.