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Coesite from quartz-jadeitite in the Dabie Mountains, Eastern China

Published online by Cambridge University Press:  05 July 2018

Wen Su ,
Shutong Xu ,
Laili Jiang  and
Yican Liu
Wen Su
Affiliation:
Anhui Institute of Geology Hefei, 230001, P. R. China
Shutong Xu
Affiliation:
Anhui Institute of Geology Hefei, 230001, P. R. China
Laili Jiang
Affiliation:
Anhui Institute of Geology Hefei, 230001, P. R. China
Yican Liu
Affiliation:
Anhui Institute of Geology Hefei, 230001, P. R. China
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Extract

The Dabie Mountains is a collisional orogen between the North China and Yantze Continental plates. It is composed, from south to north, of the foreland fold and thrust belt alternated with molasse basin, the subducted cover and basement of the Yangtze continental plate, the meta-ophiolitic melange belt, the forearc meta-flysch nappe (bounded by southward and northward thrust belts) in which there may be a buried volcanic arc and a relict back-arc basin (Fig. 1A) (Xu et al., 1992a, 1994).

Keywords

coesitejadeitequartz-jadeititeEastern China
Type
Short Communications
Information
Mineralogical Magazine , Volume 60 , Issue 401 , August 1996 , pp. 659 - 662
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1996

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References

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