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J4 ›› 2007, Vol. 15 ›› Issue (1): 1-9.

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THE PLATE TECTONICS ENVIRONMENT AND METALLOGENESIS WITHIN QINGHAI

 YI  Youchang1, MA  Cai2, LI  Yuelong1, PAN Tong1, LUO  Cairang3, WANG  Chunying1   

  1. 1.Qinghai Provincial Bureau of Nonferros Metal and Geological Mineral Exploration; Xining 810007; China; 2.Eighth Geological Party; Qinghai Provincial Bureau of Nonferros Metal and Geological Mineral Exploration; Xining 810012; 3.Westnorth Institute of Nonferrous Metals and Mineral Resources; Xian 710054; China.
  • Received:2006-12-24 Revised:2007-01-01 Online:2007-02-27 Published:2011-07-04

Abstract:

Within the plate tectonics system of Qinghai province,such The basement uplifted belt,the sedimentary belt of the oceanic crust,the island—arc uplifted belt,the magmatic islan d—arc belt,the rift belt and the active belt ofthe continental margin,the back(front)arc basin as the geoglogic environment of metallogenetic structure,there are clear diferences in their metallogenesis.During the diferent evolutionary phase of the plate tectonition ,there were diferent deposit associations.By experiencing the ovedape of repeated mountain—making activities,the depo sits have the feature of man y phases and many genesis of the metallogenesis.

Key words: Qinghai province, The plate tectonic units, Sedimenteril environment, Metallogenesi

CLC Number: 

  • P612

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