JURASSIC SED IMENTARY ENVIRONMENT IN THE QOMOLANGMA REGION

Liu Baojun; Yu guangmin; Wang Chenshan; Lan Bailong

ISSN 1000-0550 CN 62-1038/P

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Article Navigation > Acta Sedimentologica Sinica > 1983 > 1(2): 1-16

Liu Baojun, Yu guangmin, Wang Chenshan, Lan Bailong. JURASSIC SED IMENTARY ENVIRONMENT IN THE QOMOLANGMA REGION[J]. Acta Sedimentologica Sinica, 1983, 1(2): 1-16.

Citation:

Liu Baojun, Yu guangmin, Wang Chenshan, Lan Bailong. JURASSIC SED IMENTARY ENVIRONMENT IN THE QOMOLANGMA REGION[J]. Acta Sedimentologica Sinica, 1983, 1(2): 1-16.

JURASSIC SED IMENTARY ENVIRONMENT IN THE QOMOLANGMA REGION

1 Chengdu Institute of Geology and Mineral Resources;
2 Chengdu College of Geology

Received Date: 1982-04-26
Publish Date: 1983-06-10

Abstract

The Qomolangma region covers the area from Jirong to Gamba in the south of the Himalayan fauit. The welldeveloped Jurassic strata in this area are com-pietely exposed.and their total thickness is 4500m.This region belonged to a passive continental margin environment adjacent to Indian Plate during the Ju-rassic period, with active depositional setting,variedtypes,great thickness and rapid facies change.

References

[1]

(1) Wilson. J.L.,(1981)地质历史中的碳酸盐相(中译本)，地质出版社。

(2) Raup, D.M.and Stanley, S.M.,(1978)占生物学原理(中译本).地质出版社。

(3) Frey, R.W.et al..(1975) The Study of Trace Fossils, New York, Spri-nger-verlag。

(4) Hallam, A.，(1975)Jurassic Errvironrnerrts, London，New York,Melbaurne。

(5) Harms, et al.，(1975)SEPM Short Course X.2，Texas, Dallas。

(6) Reading, H.G.，(1978)Sedirttentary Enviroments and Facies,Oxford London。

(7) Stow，D.A.V.，(1979)Sedimemtology,V.26. X.3。

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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