Abstract

The CAOB is a well-known Phanerozoic juvenile orogenic belt.

Keywords

Permian Nickel Sulfide Zircon Sandstone 

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Copyright information

© Springer-Verlag Berlin Heidelberg 2014

Authors and Affiliations

  1. 1.Institute of Geology and GeophysicsChinese Academy of SciencesBeijingPeople’s Republic of China

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