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Meng Qingre, Hu Jianmin. A Tide and Storm- Influenced Shoreline and Inner Shelf Sedimentary Sequence-Ruyang Group (Precambrian) of Western Henan[J]. Acta Sedimentologica Sinica, 1992, 10(1): 57-67.
Citation: Meng Qingre, Hu Jianmin. A Tide and Storm- Influenced Shoreline and Inner Shelf Sedimentary Sequence-Ruyang Group (Precambrian) of Western Henan[J]. Acta Sedimentologica Sinica, 1992, 10(1): 57-67.

A Tide and Storm- Influenced Shoreline and Inner Shelf Sedimentary Sequence-Ruyang Group (Precambrian) of Western Henan

  • Received Date: 1990-03-20
  • Publish Date: 1992-03-10
  • Ruyang Group, consisting of the Yunmengshan, Baicaoping, ;and Beidajian formations in an sacend-ing order. is the first sedimentary sequence overlying the Precambrian volcanic rocks in western Henan>which is geologically situated on the southern margin of North China Platform. Detailed facies and fades as-socia.tion analyses show that Ruyang Group was formed in tide- and storm-influenced coastal and innershelf environments. The group can be divided into nine main facies coarse-grained sandstone/conglomerate(F1),trough crossbedded sandstone(F2),compound crossbedded snadstone(F3),giant planarcross;bedded sandstone(F4),hummocky cross- stratified sandstone(F5),flat bedded sandstone(F6),low-angle crossbedded sandstone ( F7),interbedded sandstone/mudstone (F8) and channeldeposits facies (F9).
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    (3) 关保德等,1980,中国震旦亚界,天津科学技术出版社、288-313页.

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    (9) Ilamblin, A.P. and Walker, R.G., 1979, Can. J. Earth Sci., V.16, p.1673-1690.

    (10) Klein, G.de V., 1970, 1. Sediment. Petrol.,V.40, p.973-985.

    (11) Leckie, D. A. and Walker, R.G., 1982,Bull. Am. Assoc. Pet., V.66, p.138-157.

    (12) Levell, B. K., 1980. Sedimentology, V.27,p.539-557.

    (13) Mccrory,V.L.C. and Walker, R.G., 1986, Sedimentology, V.33, p.47-60.

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    (20) Walker, R.G., 1985, SEPM short course No.13, p.243-302.
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  • Received:  1990-03-20
  • Published:  1992-03-10

A Tide and Storm- Influenced Shoreline and Inner Shelf Sedimentary Sequence-Ruyang Group (Precambrian) of Western Henan

Abstract: Ruyang Group, consisting of the Yunmengshan, Baicaoping, ;and Beidajian formations in an sacend-ing order. is the first sedimentary sequence overlying the Precambrian volcanic rocks in western Henan>which is geologically situated on the southern margin of North China Platform. Detailed facies and fades as-socia.tion analyses show that Ruyang Group was formed in tide- and storm-influenced coastal and innershelf environments. The group can be divided into nine main facies coarse-grained sandstone/conglomerate(F1),trough crossbedded sandstone(F2),compound crossbedded snadstone(F3),giant planarcross;bedded sandstone(F4),hummocky cross- stratified sandstone(F5),flat bedded sandstone(F6),low-angle crossbedded sandstone ( F7),interbedded sandstone/mudstone (F8) and channeldeposits facies (F9).

Meng Qingre, Hu Jianmin. A Tide and Storm- Influenced Shoreline and Inner Shelf Sedimentary Sequence-Ruyang Group (Precambrian) of Western Henan[J]. Acta Sedimentologica Sinica, 1992, 10(1): 57-67.
Citation: Meng Qingre, Hu Jianmin. A Tide and Storm- Influenced Shoreline and Inner Shelf Sedimentary Sequence-Ruyang Group (Precambrian) of Western Henan[J]. Acta Sedimentologica Sinica, 1992, 10(1): 57-67.
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