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The Tian Shan Orogenic Belt,which is a subsidiary of the Central Asian Orogenic Belt,is the largest accretion area of continental crust on the Earth during the Phanerozoic.It has experienced several accretionary processes during the Palaeozoic period and has attracted much concern among geologists.An Early Palaeozoic intrusive rock belt extends
The Tian Shan Orogenic Belt, which is a subsidiary of the Central Asian Orogenic Belt, is the largest accretion area of continental crust on the Earth during the Phanerozoic. It has experienced several accretionary processes during the Palaeozoic period and has attracted much concerned among geologists. An Early Palaeozoic intrusive rock belt extends