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《EARTH SCIENCE FRONTIERS》 1998-01
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STUDY ON CHEMICAL HETEROGENEITIES OF MANTLE CRUSTAL SYSTEMS AND GEOCHEMICAL BOUNDARIES OF BLOCKS

Zhu Bingquan(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640)  
The studies on multi isotopic systematics of rocks derived from mantle and crust show that there exist chemical heterogeneties of blocks in the golbe, in which geochemical provinces of four types with geochemical steep zones as boundaries can be distinguished. They are the East Gondwana(such as Cathaysia and Tibet Indochina in Continental China), the West Gondwana, the Pacific(such as Jiamusi, Central Mongolia, Liaojiaobo, North Xinjiang, South Gobia) and the Laurasia(such as North China, China Korea, Xing'an and Tarim). There exists a tight relationship between the geochemical and geophysical steep zones. Geochemical steep zones in tectonics can be classified as two kinds; i.e.the tectonic dominance and the recessiveness, which can be well explained in the light of a tectonic flyover model between surface and buried structures as well as their transition from each other. The distribution of super large deposits and mineralization intensive domains are tightly controlled by the geochemical steep zones, especially at their turning points; in which reconstruction mineralization associated with dynamic metamorphism and magmatism occurs mainly on the dominant steep zones, whereas volcanism and MVT deposits are related to the recessive geochemical boundaries. The most of oil fields with industrial index are also located at the cross districts between basin and tectonic recessive geochemical boundaries.
【Fund】: 国家科委攀登计划A和B项 国家自然科学基金会重大项目
【CateGory Index】: P591
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