MESOZOIC GRANITIC MAGMATISM AND METALLOGENY IN THE KHENTEY RANGE,MONGOLIA |
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| Authors: | Ochir Gerel |
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| Abstract: | 1 Introduction Petrogenesis of Mesozoic granitoids in Mongolia that comprise the Mongol-Okhotsk foldbelt was studied during more than 40 years.This belt is well known province of the Mesozoic magmatism and mineralization including gold,copper and molybdenum,tin and tungsten,lead and zinc,and fluorite.In the middle of the 1950's Chen Guoda proposed the diwa theory to explain tectonic activity in Chinese platform.In Russian Far East for similar processes the activization (revivation) theory was proposed which explained intracontinental events in the Mongol-okhotsk foldbwlt. |
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