There are great bifurcations as yet on the structural environment and on the evolution of the Xingmeng Paleozoic orogenic belt in Southeast Inner Mongolia during the Carboniferous Period.

 
  • 內蒙古東南部古生代造山帶在石炭紀時(shí)期的構造環(huán)境和構造演化,至今在認識上存在較大的分歧。
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