The Middle-shallow Water Sedimentary Environment of the Late Sinian of South Anhui&mdash;&mdash;Based on the olistotrome and the siliceous storm sediments

YU Xin-qi; SHU Liang-shu; DENG Ping; WANG De-en; ZHI Li-geng

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2003 > 21(3): 398-403

YU Xin-qi, SHU Liang-shu, DENG Ping, WANG De-en, ZHI Li-geng. The Middle-shallow Water Sedimentary Environment of the Late Sinian of South Anhui——Based on the olistotrome and the siliceous storm sediments[J]. Acta Sedimentologica Sinica, 2003, 21(3): 398-403.

Citation:

The Middle-shallow Water Sedimentary Environment of the Late Sinian of South Anhui——Based on the olistotrome and the siliceous storm sediments

1.
Department of Earth Sciences of Nanjing University, Nanjing 210093;
2.
Research Institute No.290,CNNC,Shaoguan Guangdong 512026;
3.
332Team of Anhui Bureau of Geology and Mineral Resourc es, Huangshan Anhui 245000

Received Date: 2002-04-15
Rev Recd Date: 2002-06-12
Publish Date: 2003-09-10

Abstract

We have found in Shexian and Xiuning Counties of South Anhui that ther e are some turbidite interlayers and a debris flow caused olistostrome near the to p of the Lantian Formation of the lower member of the Upper Sinian, and t here are some siliceous storm sediments in the Piyuangcun Formation of the top m ember of the Upper Sinian.These discoveries indicate that the area of South Anh u i belongs to a hemipelagic or shallow environment when sedimentation occurs duri ng the late Sinian,not a pelagic environment as being usually believed,at lea st the sedimentary surface was not lower than the wave base of the storm.
- olistostrome,
- storm sediments,
- Piyuancun and Lantian Formations,
- Late Sinian,
- South Anhui,

References

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The Middle-shallow Water Sedimentary Environment of the Late Sinian of South Anhui——Based on the olistotrome and the siliceous storm sediments

1. Department of Earth Sciences of Nanjing University, Nanjing 210093;

2. Research Institute No.290,CNNC,Shaoguan Guangdong 512026;

3. 332Team of Anhui Bureau of Geology and Mineral Resourc es, Huangshan Anhui 245000

Received Date: 2002-04-15

Rev Recd Date: 2002-06-12

Publish Date: 2003-09-10

Key words:

Abstract: We have found in Shexian and Xiuning Counties of South Anhui that ther e are some turbidite interlayers and a debris flow caused olistostrome near the to p of the Lantian Formation of the lower member of the Upper Sinian, and t here are some siliceous storm sediments in the Piyuangcun Formation of the top m ember of the Upper Sinian.These discoveries indicate that the area of South Anh u i belongs to a hemipelagic or shallow environment when sedimentation occurs duri ng the late Sinian,not a pelagic environment as being usually believed,at lea st the sedimentary surface was not lower than the wave base of the storm.

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Reference (42)

[1]	周永章,涂光枳,Edward H Chown 等. 粤西古水剖面震旦系顶部层状硅质岩的热水成因属性:岩石学和地球化学证据[J]. 沉积学报,1994,12(3):1～11[Zhou Yongzhang, Tu Guangzhi, Edward H. Choen, et al. Hydrothermal origin of Top Sinian chert formation at Gushui, Western Guangdong, China: Petrologic and Geochemical Evidence[J]. Acta Sedimentologica Sinica, 1994, 12(3): 1～11]
[2]	冯彩霞,刘家军.硅质岩的研究现状及其成矿意义[J].世界地质,2001,20(2):119～123[ Feng Caixia,Liu Jiajun. Current research situation of siliceous rocks and its mineralization significance [J]. World Geology, 2001, 20(2): 119～123]
[3]	王东安. 扬子地台晚元古代以来硅质岩地球化学特征及其成因[J]. 地质科学,1994,29(1):41～54 [ Wang Dong'an. The geochemical feature of siliceous rocks since late Proterozoic in the Yangtze platform and their genesis[J]. Scientia Geologica Sinica, 1994, 29(1): 41～54]
[4]	刘学义.石门雄黄矿区角砾岩硅质岩成因新探[J]. 湖南地质,1992,11(1):11～15[ Liu Xueyi. New undersdanding about the origin of the breccia and siliceous rocks in Shimen Realgar Ore region[J]. Hunan Geology, 1992, 11(2): 11～15]
[5]	刘家军,郑明华,刘建明等.西秦岭寒武系硅质岩建造喷流沉积作用与矿质聚集[J]. 高校地质学报,1998, 4(1):20～33[ Liu Jiajun, Zheng Minghua, Liu Jianming, et al. Submarine exhalative sedimentation and mineralization of the silicalite Formation in Western Qinling, China[J]. Geological Journal of China Universities, 1998, 4(1):20～33]
[6]	朱洪发,秦德余,刘翠章.论华南孤峰组和大隆组硅质岩成因、分布规律及其构造机制[J]. 石油实验地质,1989, 11(4):341～348[ Zhu Hongfa, Qin Deyu,Liu Cuizhang. On the origin, distributive pattern and tectonic control of siliceous rocks in Gufeng and Dalong Formations, South China[J]. Experimental Petroleum Geology, 1989, 11(4): 341～348]
[7]	李胜荣,高振敏.华南下寒武统黑色岩系中的热水成因硅质岩[J]. 矿物学报,1996, 16(4):416～422[ Li Shengrong, Gao Zhangmin. Silicalites of hydrothermal origin in the Lower Cambrian black rock series of South China[J]. Acta Mineralogica Sinica, 1996, 16(4): 416～422]
[8]	杨健民,王登红,毛景文等.硅质岩岩石化学研究方法及其在"镜铁山式"铁矿床中的应用[J].岩石矿物学杂志,1999,18(2):108～120[ Yang Jianmin, Wang Denghong, Mao Jingwen, et al. The petrochemica1 research method for silicalite and its application to the"Jingtieshan type" iron deposits[J]. Acta Petrologica et Mineralogica, 1999, 18(2): 108～120]
[9]	沈上越,魏启荣,程惠兰等. "三江"地区哀牢山带两类硅质岩特征及大地构造意义[J].岩石矿物学杂志,2001,20(1):42～46[ Shen Shangyue, Wei Qirong, Cheng Huilan, et al. Characteristics and Geotectonic Implications of Sorts of Silicalites in Ailao Mountain Belt,"Three-River" Area[J]. Acta Petrologica et Mineralogica, 2001, 20(1): 42～46]
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The Middle-shallow Water Sedimentary Environment of the Late Sinian of South Anhui——Based on the olistotrome and the siliceous storm sediments

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The Middle-shallow Water Sedimentary Environment of the Late Sinian of South Anhui——Based on the olistotrome and the siliceous storm sediments

1. Department of Earth Sciences of Nanjing University, Nanjing 210093;

2. Research Institute No.290,CNNC,Shaoguan Guangdong 512026;

3. 332Team of Anhui Bureau of Geology and Mineral Resourc es, Huangshan Anhui 245000

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The Middle-shallow Water Sedimentary Environment of the Late Sinian of South Anhui——Based on the olistotrome and the siliceous storm sediments

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The Middle-shallow Water Sedimentary Environment of the Late Sinian of South Anhui——Based on the olistotrome and the siliceous storm sediments

1. Department of Earth Sciences of Nanjing University, Nanjing 210093; 2. Research Institute No.290,CNNC,Shaoguan Guangdong 512026; 3. 332Team of Anhui Bureau of Geology and Mineral Resourc es, Huangshan Anhui 245000

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1. Department of Earth Sciences of Nanjing University, Nanjing 210093;

2. Research Institute No.290,CNNC,Shaoguan Guangdong 512026;

3. 332Team of Anhui Bureau of Geology and Mineral Resourc es, Huangshan Anhui 245000