Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia

XIEXiao ping; WANGYong dong; SHENHuan ting

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Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(1): 19-28

XIEXiao ping, WANGYong dong, SHENHuan ting. Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia[J]. Acta Sedimentologica Sinica, 2004, 22(1): 19-28.

Citation:

XIEXiao ping, WANGYong dong, SHENHuan ting. Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia[J]. Acta Sedimentologica Sinica, 2004, 22(1): 19-28.

Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia

1.
State Key Laboratory of Estuarine and Coastal Science Research, Eastern China Normal University, Shanghai 200062;
2.
Department of Geography, Qufu Normal University, QufuShandong 273165;
3.
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008

Received Date: 2002-09-24
Rev Recd Date: 2002-12-17
Publish Date: 2004-03-10

Abstract

The Late Carboniferous marine and non marine alternating deposits are well developed and outcropped in Xiaheyan of Zhongwei County, Ningxia Hui Autonomous Regionnorthwest China, including the Hongtuwa, Yanghugou and Taiyuan Formations. The facies analysis and sedimentary environment evolution are investigated in this study based on evidences of lithology, color, granularity analysis, facies indicator, geochemical data as well as fossil fauna and flora and Spore Pollen assemblages. Five facies are recognized including lagoon, tide flat, distributary bay estuarine sandbar, seashore and lowland marsh and tidal plainas well. In addition, the palaeogeographical background and sedimentary environmental evolution in Zhongwei of Ningxia are revealed and reconstructed based upon comparisons of the sedimentary characteristics with adjacent regions, including Eastern Sector of North Qilian, Ordos Basin and Taiyuan area of Northern China.
- Late Carboniferous,
- facies analysis,
- sedimentary environment,
- Zhongwe,
- Ningxia

References

[1]	刘志才,郑昭昌,杨逢清,等.宁夏中卫校育川的纳缪尔期地层剖面. 地层学杂志,1983,7(2):130～134[Liu Zhicai, Zheng Zhaochang, Yang Fengqing, et al. A Namurian stratigraphical section of Jiaoyuchuan, Zhongwei,Ningxia. Journal of Stratigraphy,1983,7 (2): 130～134]
[2]	刘志才,郑昭昌. 宁夏中卫、中宁地区纳缪尔期地层. 见: 地层古生物论文集.1988,19(1):219～230[Liu Zhicai, Zheng Zhaochang. Namurian stratigraphy of Zhongwei and Zhongning, Ningxia. In: Thesises collections of stratigraphy and paleotologica.1988,19: 219～230]
[3]	杨逢清.宁夏中卫、中宁地区纳缪尔期贫氧生物相特征.地球科学-中国地质大学学报,1992, 17(3):271～279[Yang Fengqing. Characteristics of the Namurian dysaerobic biofacies from Zhongwei and Zhongning regions, Ningxia, China.Earth Science, 1992,17(3):271～279]
[4]	杨式溥,田树刚,郑昭昌.宁夏中卫校育川纳缪尔期牙形石.见:地层古生物论文集,1988.22,23～30[Yang Shipu, Tian Shugang, Zheng Zhaochang. Namurian Conodonts from Xiaoyuchuan, Ningxia. In: Theses collections of stratigraphy and paleotologica,1988.22,23～30]
[5]	霍福臣,潘行适,尤国林,等. 宁夏地质概论.北京:科学出版社,1989. 18～149[Huo Fuchen,Pan Xingshi, You Guolin,et al. Introduction to geology of Ningxia.Beijing: Science Press,1989. 118～149 ]
[6]	Li Xingxue, Shen Guanglong, Wu Xiuyuan, et al.Successional changes of Late Carboniferous autochthonous clastic swamp taphonomic phytocommunities from Xiaheyan, Zhongwei, Ningxia. In: Jin Yugan, Wang Jungeng and Xu Shanhong, eds.Palaeoecology of China. Nanjing: Nanjing University Press,1991.151～167
[7]	沈光隆,吴秀元,李克定. 北祁连地区石炭-二叠系界线问题. 甘肃地质学报,1993,2(2):1～14[Shen Guanglong, Wu Xiuyuan, Li Keding.Carboniferous-Permian boundary of North Qilian District.Acta Geologica Gansu,1993,2(2): 1～14]
[8]	王永栋. 宁夏中卫晚石炭世维斯发期孢粉组合.植物学报,1995,37(12):978～985[Wang Yongdong. Westphalian Sporo-Pollen assemblages from the Upper Carboniferous in Zhongwei, Ningxia. Acta Botanica Sinica, 1995,37(12): 978～985]
[9]	王永栋,沈光隆. 宁夏中卫上石炭统羊虎沟组的一个孢粉学事件.微体古生物学报,1995,12(2):199～205[Wang Yongdong, Shen Guanglong.An upper Carboniferous palynological event from the Northwest China Yanghugou Formation in Zhongwei of Ningxia.Acta Micropalaeotologica Sinica,1995,12 (2): 199～205]
[10]	王永栋,沈光隆,吴秀元. 宁夏中卫县下河沿太原组生物地层-兼论石炭-二叠系分界. 中国区域地质,1995,(2):164～172[Wang Yongdong, Shen Guanglong, Wu Xiuyuan. Biostratigraphy of the Taiyuan Formation at Xiaheyan, Zhongwei county, Ningxia-with a discussion of the Carboniferous-Permian boundary.Regional Geology of China,1995,(2): 164～172]
[11]	Wang Yongdong.Palynological zonations and paleoecology of Carboniferous sequence from Zhongwei of Ningxia, China.Paleobotanist, 1995, 44: 48～61
[12]	Wang Yongdong. Carboniferous palynostratigraphy and strato-boundaries in Zhongwei of Ningxia, China. Journal of Northwest University(English Edit.), 1996,26: 43～48
[13]	Wang Yongdong, Shen Guanlong, Wu Xiuyuan.Micro-and Megafloral remains of Namurian H-G1 Zones from Zhongwei, Ningxia, China. Paleobotanist, 1996,45: 224～232
[14]	高联达.宁夏石炭纪、早二叠世孢子带和石炭-二叠系界线. 甘肃地质学报,1994,3(1):1～26[Gao Lianda.Carboniferous and early Permian Spore zonations and the boundary of the Carboniferous-Permian in Ningxia.Acta Geologica Gansu,1994, 3(1): 11～26]
[15]	吴秀元,李星学,沈光隆,等. 甘肃靖远石炭系研究新进展[J]. 地层学杂志,1987,11(3):163～176[Wu Xiuyuan, Li Xingxue, Shen Guanglong, et al.New advances in the study of Carboniferous rocks of Jingyuan, eastern Gansu.Journal of Stratigraphy,1987, 11(3): 163～179]
[16]	西安地质学院等. 甘肃河西走廊东部地区石炭纪和二叠纪地层以及沉积相和生储条件的研究.西安:西北大学出版社,1989.1～136[Xi'an Geology College,et al. The study of the Carboniferous and Permian stratigraphy and facies and resource reservoir condition of the east part of Hexi Corridor, Gansu.Xi'an: Northwest University Press,1989.1～136]
[17]	刘宝珺主编. 沉积岩石学.北京:地质出版社,1980.295～297[Liu Baojun edited. Sedimentary lithology. Beijing: Geological Publishing House,1980.295～297]
[18]	佟再三,李汉业. 靖远磁窑晚石炭世沉积环境基本特征. 甘肃地质学报,1995,4(1):21～29[Tong Zaisan, Li Hanye.Basic features of late Carboniferous sedimentary ebvironment at Ciyao in Jingyuan county, Gansu. Acta Geologica Gansu,1995,4 (1): 21～29]
[19]	佟再三. 北祈连东段石炭纪古地理与构造关系初探. 甘肃地质学报,1993,2(2):61～66[Tong Zaisan. On the relationship between Carboniferous paleogeography and tectonics in the East part of the North Qilian mountains.Acta Geologica Gansu,1993,2(2): 61～66]
[20]	佟再三,李汉业. 北祈连东段石炭纪岩相古地理基本特征.沉积学报,1994,12(1):89～97[Tong Zaisan, Li Hanye.Characteristics of Carboniferous lithofacies and paleogeography in Eastern part of North Qilian.Acta Sedimentologica Sinica,1994, 20 (1): 89～97]
[21]	何宝珍,晁吉祥.西北地区石炭纪古地理轮廓及沉积特征.煤田地质与勘探,1982,(2):14～20[He Baozhen,Chao Jixiang. The characteristics of the Carboniferous paleogeography and sedimentary significance in northwest China. Coal Geology and Prospecting,1982,(2): 14～20]
[22]	吴汉宁,周立发,赵重远. 阿拉善及邻区石炭二叠系古地磁学研究及意义. 中国科学(B辑),1993,23:527～536[Wu Hanning, Zhou Lifa, Zhao Zhongyuan.The paleomagnetic study and significance of Carboniferous-Permian in Alashan and adjacent area.Science in China (Series B), 1993,.23: 527～536]
[23]	Huang Baochun, Yo-ichiro Otofuji, Zhu Rixiang,et al. Paleomagnetism of Carboniferous sediments in the Hexi Corridor: its origin and tectonic implications.Earth and Planetary Science Letters,2001,194:135～149

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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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Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia

1. State Key Laboratory of Estuarine and Coastal Science Research, Eastern China Normal University, Shanghai 200062;

2. Department of Geography, Qufu Normal University, QufuShandong 273165;

3. Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008

Received Date: 2002-09-24

Rev Recd Date: 2002-12-17

Publish Date: 2004-03-10

Key words:

Abstract: The Late Carboniferous marine and non marine alternating deposits are well developed and outcropped in Xiaheyan of Zhongwei County, Ningxia Hui Autonomous Regionnorthwest China, including the Hongtuwa, Yanghugou and Taiyuan Formations. The facies analysis and sedimentary environment evolution are investigated in this study based on evidences of lithology, color, granularity analysis, facies indicator, geochemical data as well as fossil fauna and flora and Spore Pollen assemblages. Five facies are recognized including lagoon, tide flat, distributary bay estuarine sandbar, seashore and lowland marsh and tidal plainas well. In addition, the palaeogeographical background and sedimentary environmental evolution in Zhongwei of Ningxia are revealed and reconstructed based upon comparisons of the sedimentary characteristics with adjacent regions, including Eastern Sector of North Qilian, Ordos Basin and Taiyuan area of Northern China.

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Reference (23)

[1]	刘志才,郑昭昌,杨逢清,等.宁夏中卫校育川的纳缪尔期地层剖面. 地层学杂志,1983,7(2):130～134[Liu Zhicai, Zheng Zhaochang, Yang Fengqing, et al. A Namurian stratigraphical section of Jiaoyuchuan, Zhongwei,Ningxia. Journal of Stratigraphy,1983,7 (2): 130～134]
[2]	刘志才,郑昭昌. 宁夏中卫、中宁地区纳缪尔期地层. 见: 地层古生物论文集.1988,19(1):219～230[Liu Zhicai, Zheng Zhaochang. Namurian stratigraphy of Zhongwei and Zhongning, Ningxia. In: Thesises collections of stratigraphy and paleotologica.1988,19: 219～230]
[3]	杨逢清.宁夏中卫、中宁地区纳缪尔期贫氧生物相特征.地球科学-中国地质大学学报,1992, 17(3):271～279[Yang Fengqing. Characteristics of the Namurian dysaerobic biofacies from Zhongwei and Zhongning regions, Ningxia, China.Earth Science, 1992,17(3):271～279]
[4]	杨式溥,田树刚,郑昭昌.宁夏中卫校育川纳缪尔期牙形石.见:地层古生物论文集,1988.22,23～30[Yang Shipu, Tian Shugang, Zheng Zhaochang. Namurian Conodonts from Xiaoyuchuan, Ningxia. In: Theses collections of stratigraphy and paleotologica,1988.22,23～30]
[5]	霍福臣,潘行适,尤国林,等. 宁夏地质概论.北京:科学出版社,1989. 18～149[Huo Fuchen,Pan Xingshi, You Guolin,et al. Introduction to geology of Ningxia.Beijing: Science Press,1989. 118～149 ]
[6]	Li Xingxue, Shen Guanglong, Wu Xiuyuan, et al.Successional changes of Late Carboniferous autochthonous clastic swamp taphonomic phytocommunities from Xiaheyan, Zhongwei, Ningxia. In: Jin Yugan, Wang Jungeng and Xu Shanhong, eds.Palaeoecology of China. Nanjing: Nanjing University Press,1991.151～167
[7]	沈光隆,吴秀元,李克定. 北祁连地区石炭-二叠系界线问题. 甘肃地质学报,1993,2(2):1～14[Shen Guanglong, Wu Xiuyuan, Li Keding.Carboniferous-Permian boundary of North Qilian District.Acta Geologica Gansu,1993,2(2): 1～14]
[8]	王永栋. 宁夏中卫晚石炭世维斯发期孢粉组合.植物学报,1995,37(12):978～985[Wang Yongdong. Westphalian Sporo-Pollen assemblages from the Upper Carboniferous in Zhongwei, Ningxia. Acta Botanica Sinica, 1995,37(12): 978～985]
[9]	王永栋,沈光隆. 宁夏中卫上石炭统羊虎沟组的一个孢粉学事件.微体古生物学报,1995,12(2):199～205[Wang Yongdong, Shen Guanglong.An upper Carboniferous palynological event from the Northwest China Yanghugou Formation in Zhongwei of Ningxia.Acta Micropalaeotologica Sinica,1995,12 (2): 199～205]
[10]	王永栋,沈光隆,吴秀元. 宁夏中卫县下河沿太原组生物地层-兼论石炭-二叠系分界. 中国区域地质,1995,(2):164～172[Wang Yongdong, Shen Guanglong, Wu Xiuyuan. Biostratigraphy of the Taiyuan Formation at Xiaheyan, Zhongwei county, Ningxia-with a discussion of the Carboniferous-Permian boundary.Regional Geology of China,1995,(2): 164～172]
[11]	Wang Yongdong.Palynological zonations and paleoecology of Carboniferous sequence from Zhongwei of Ningxia, China.Paleobotanist, 1995, 44: 48～61
[12]	Wang Yongdong. Carboniferous palynostratigraphy and strato-boundaries in Zhongwei of Ningxia, China. Journal of Northwest University(English Edit.), 1996,26: 43～48
[13]	Wang Yongdong, Shen Guanlong, Wu Xiuyuan.Micro-and Megafloral remains of Namurian H-G1 Zones from Zhongwei, Ningxia, China. Paleobotanist, 1996,45: 224～232
[14]	高联达.宁夏石炭纪、早二叠世孢子带和石炭-二叠系界线. 甘肃地质学报,1994,3(1):1～26[Gao Lianda.Carboniferous and early Permian Spore zonations and the boundary of the Carboniferous-Permian in Ningxia.Acta Geologica Gansu,1994, 3(1): 11～26]
[15]	吴秀元,李星学,沈光隆,等. 甘肃靖远石炭系研究新进展[J]. 地层学杂志,1987,11(3):163～176[Wu Xiuyuan, Li Xingxue, Shen Guanglong, et al.New advances in the study of Carboniferous rocks of Jingyuan, eastern Gansu.Journal of Stratigraphy,1987, 11(3): 163～179]
[16]	西安地质学院等. 甘肃河西走廊东部地区石炭纪和二叠纪地层以及沉积相和生储条件的研究.西安:西北大学出版社,1989.1～136[Xi'an Geology College,et al. The study of the Carboniferous and Permian stratigraphy and facies and resource reservoir condition of the east part of Hexi Corridor, Gansu.Xi'an: Northwest University Press,1989.1～136]
[17]	刘宝珺主编. 沉积岩石学.北京:地质出版社,1980.295～297[Liu Baojun edited. Sedimentary lithology. Beijing: Geological Publishing House,1980.295～297]
[18]	佟再三,李汉业. 靖远磁窑晚石炭世沉积环境基本特征. 甘肃地质学报,1995,4(1):21～29[Tong Zaisan, Li Hanye.Basic features of late Carboniferous sedimentary ebvironment at Ciyao in Jingyuan county, Gansu. Acta Geologica Gansu,1995,4 (1): 21～29]
[19]	佟再三. 北祈连东段石炭纪古地理与构造关系初探. 甘肃地质学报,1993,2(2):61～66[Tong Zaisan. On the relationship between Carboniferous paleogeography and tectonics in the East part of the North Qilian mountains.Acta Geologica Gansu,1993,2(2): 61～66]
[20]	佟再三,李汉业. 北祈连东段石炭纪岩相古地理基本特征.沉积学报,1994,12(1):89～97[Tong Zaisan, Li Hanye.Characteristics of Carboniferous lithofacies and paleogeography in Eastern part of North Qilian.Acta Sedimentologica Sinica,1994, 20 (1): 89～97]
[21]	何宝珍,晁吉祥.西北地区石炭纪古地理轮廓及沉积特征.煤田地质与勘探,1982,(2):14～20[He Baozhen,Chao Jixiang. The characteristics of the Carboniferous paleogeography and sedimentary significance in northwest China. Coal Geology and Prospecting,1982,(2): 14～20]
[22]	吴汉宁,周立发,赵重远. 阿拉善及邻区石炭二叠系古地磁学研究及意义. 中国科学(B辑),1993,23:527～536[Wu Hanning, Zhou Lifa, Zhao Zhongyuan.The paleomagnetic study and significance of Carboniferous-Permian in Alashan and adjacent area.Science in China (Series B), 1993,.23: 527～536]
[23]	Huang Baochun, Yo-ichiro Otofuji, Zhu Rixiang,et al. Paleomagnetism of Carboniferous sediments in the Hexi Corridor: its origin and tectonic implications.Earth and Planetary Science Letters,2001,194:135～149

Facies Analysis and Sedimentary Environment Reconstruction of the Late Carboniferous in Zhongwei,Ningxia

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