太古宙—元古宙过渡分界及成矿动力体制转换

邓军; 孙忠实; 王建平; 王庆飞; 王喜臣; 燕长海

Volume 28 Issue 1

Jan. 2003

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Article Navigation > Earth Science > 2003 > 28(1): 87-96

DENG Jun, SUN Zhong-shi, WANG Jian-ping, WANG Qing-fei, WANG Xi-chen, YAN Zhang-hai, 2003. Demarcating Interval between Archean Group and Proterozoic Group and Ore-Forming Dynamical Transformation. Earth Science, 28(1): 87-96.

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Demarcating Interval between Archean Group and Proterozoic Group and Ore-Forming Dynamical Transformation

1.
Department ofEarth Science and Resource, China University of Geosciences, Beijing 100083, China
2.
The Key LaboratoryofLithosphere Tectonics and Exploration(KLLTE), MinistryofEducation, Beijing 100083, China
3.
Department ofEarth Science, Jilin University, Changchun 130026, China

Received Date: 2002-03-11
Publish Date: 2003-01-25

Abstract

Abstract

The narrowness and confusion of demarcating time between Archean and Proterozoic have kept deepening research on the early geology within great limits. Through determination demarcating and transiting criteria, the transformation of geo-dynamics system between Archean and Proterozoic can be divided into four types: transformation from compressional to extensional system, from vertical to horizontal, of principal stress, from mantle plume to plate tectonics. The relatively outcomes which formed within 0.3~0.5 billions year of transformations includes eucaryote, radioelements, magma and ores. The partition between Archean and Proterozoic should have a transiting line, that can be limited in 2.20~2.80 Ga. The partition has close relation with major geological events, and this work brings a new edification to ore-formation in depth.
- Archean-Proterozoic,
- transiting line,
- ore-forming dynamics,
- system transformation

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References(51)

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