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《Geological Review》 1990-03
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BLUESCHISTS IN THREE TECTONIC ENVIRONMENTS IN NORTHERN CHINA

Gao Changlin, Ji Rangshou, Qin Deyu and Yin Yong(Central Laboratory of Petroleum Geology, Ministry of Geology and Mineral Resources, Wuxi)  
This paper deals with the characteristics of A-, B-and C-type blueschists in three tectonic environments. 1. The origin of bluesehist in Ondor Sum, Nei Mongol, is related to the subduction of the Mongolian paleo-oceanic plate. It is classified as B-type blueschist and its main characteristics are as follows: a) The blueschist belt is wide and there are a great variety of high-pressure minerals in this type of blueschist. b) The blueschist is associated with ophiolite. The ophiolite exhibits a strata sequence and the geological and geochemical characteristics of oceanic crust. c) The blueschist belt is a part of the paired metamorphic belts. 2. The origin of blueschist in Songshugou(Shangnan, Shaanxi)is related to the obduction of the plate. It is classified as C-type blueschist and the main characteristics are: a) The blueschist is associated with ophiolite which has either the geological and geochemical characteristics of oceanic crust or oceanic-continental transitional crust. b) The blueschist belt is narrow and there are no paired metamorphic belts. 3. The blueschist in Zhaochuan, Shangnan, Shaanxi, is classified as A-type blueschist and the main characteristics are: a) The blueschist is obviously controlled by fault zones and may occur in various types of ortho-and para-metamorphic rocks. b) The blueschist is not associated with ophiolite. c) The blueschist belt is narrow and there are no paired metamorphic belts
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