The Junggar orogen, Xinjiang, China, is an important part of the Ural-Mongolian orogen as well as one of the typical collisional orgenic areas. The collisional orogenesis in the area occurred in the Carboniferous and Permian, and shows the character of th
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陈衍景.1996.准噶尔造山带碰撞体制的成矿作用及金等矿床分布规律[J].地质学报,70(3). Chen Yanjing.1996. MINERALIZATION DURING COLLISIONAL OROGENESIS AND ITS CONTROL OF THE DISTRIBUTION OF GOLD DEPOSITS IN JUNGGAR MOUNTAINS, XINJIANG, CHINA[J]. Acta Geologica Sinica,70(3).
