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GEOCHEMICAL EFFECTS OF MAJOR ELEMENTS DURING FLUID ROCKS INTERAC TION IN MARINWOBO FAULT IN THE SOUTH MARGIN AREAS OF ALTAI MOUNTAINS
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作者 ZHAO Zhi zhong1, ZENG Qiao song2 and BI Hua1(1. Department of Resources, Environment and Tourism, Hainan Normal University, Haikou Hainan 571158, China 2. Changsha Institute of Geotectonics, Chinese Academy of Sciences, Changsha Hunan 410013, China) 《Geotectonica et Metallogenia》 2002年第1期68-75,共8页
There are four types of metamorphic rocks in the Marinwobo fault, i.e, cataclasite, mylonite, mictosite and migmatitic granite, and the formation of these rocks is due to the progressive metamorphism of the pyroclasti... There are four types of metamorphic rocks in the Marinwobo fault, i.e, cataclasite, mylonite, mictosite and migmatitic granite, and the formation of these rocks is due to the progressive metamorphism of the pyroclastics. The fluids play a very important role in the metamorphic process of these rocks in the Marinwobo fault, the most important feature is that the fluids not only result in the migration of the major elements of the deformation rocks, but also result in the volume loss of the deformation rocks in the deformation process. Thus the migration laws of the major elements in different stages of the progressive metamorphic process are discussed according to mass balance equations. Finally, the quantitative analysis of the mass loss and volume loss of the different rocks the in Marinwobo fault is discussed in this paper. 展开更多
关键词 GEOCHEMICAL effect fluids element migration marinwobo fault ALTAI Mts.
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