The discovery of early Permian reef belt in east Kunlun and its significance

The early permian reef belt is distributed in the southern side of eastern Kunlun, north area of Qinghai-Tibet Plateau. The core-reef facies of thc reel extends from Tuosuo Lake to Huashixia. Lots of reef breccia was found at the southern slope of the mre-reef belt, and to the north of the reef belt...

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Bibliographic Details
Published in:Chinese science bulletin 1998-06, Vol.43 (11), p.947-950
Main Authors: Yongbiao, Wang, Kexing, Zhang, Yiming, Gong, Zhi, Zhang, Mansheng, Luo
Format: Article
Language:English
Subjects:
Algae
Aquatic plants
Belts
Breccia
corals
early
east
Echinodermata
Hydrozoa
Kunlun
lakes
Limestone
Permian
reef
Rhodophyta
topographic slope
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Summary:The early permian reef belt is distributed in the southern side of eastern Kunlun, north area of Qinghai-Tibet Plateau. The core-reef facies of thc reel extends from Tuosuo Lake to Huashixia. Lots of reef breccia was found at the southern slope of the mre-reef belt, and to the north of the reef belt there is back-reef limestone. Cacisponges, hydrozoa, bryozoa,Tabulozoa, Tubiphytes and red algae are the main frame-building organisms.Archaeolithoporella, laminated blue-green algaes,Tabulozoa andTubiphytes played a role of binding or encrustating. There are many kinds of epibiont in the mf, including brachiopod, gasterid, foraminifera, echinoderm and simple coral. The type and the characteristics of the reef-building organisms in eastern Kunlun and Animaqing are basically thr same as those in the south of Chi.
ISSN:1001-6538
2095-9273
1861-9541
2095-9281
DOI:10.1007/bf02884620