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甘肃景泰红水堡晚石炭世沉积环境与沉积相分析

谢小平 佟再三 沈焕庭

谢小平, 佟再三, 沈焕庭. 甘肃景泰红水堡晚石炭世沉积环境与沉积相分析[J]. 沉积学报, 2003, 21(3): 381-390.
引用本文: 谢小平, 佟再三, 沈焕庭. 甘肃景泰红水堡晚石炭世沉积环境与沉积相分析[J]. 沉积学报, 2003, 21(3): 381-390.
XIE Xiao-ping, TONG Zai-san, SHEN Huan-ting. Analysis on Sedimentary Environment and Facies in Later Carboniferous Epoch of Hongshuibao, Jingtai County,Gansu Province[J]. Acta Sedimentologica Sinica, 2003, 21(3): 381-390.
Citation: XIE Xiao-ping, TONG Zai-san, SHEN Huan-ting. Analysis on Sedimentary Environment and Facies in Later Carboniferous Epoch of Hongshuibao, Jingtai County,Gansu Province[J]. Acta Sedimentologica Sinica, 2003, 21(3): 381-390.

甘肃景泰红水堡晚石炭世沉积环境与沉积相分析

详细信息
    作者简介:

    谢小平,男,1966年出生,博士,讲师,沉积学

  • 中图分类号: P512.2;P534.45

Analysis on Sedimentary Environment and Facies in Later Carboniferous Epoch of Hongshuibao, Jingtai County,Gansu Province

  • 摘要: 甘肃省景泰县红水堡地处北祁连加里东褶皱带东段。晚石炭世地层包括红土洼组、羊虎沟组及太原组。根据岩性、颜色、粒度分析、沉积相标志及古生物组合并结合古生态、以及地球化学特征,将景泰红水堡晚石炭世沉积环境与沉积相划分为泻湖、潮坪、支间湾河口坝和三角洲平原。一个明显的陆源沉积物向海推进的海退序列.
  • [1] 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): 163~179 [Wu Xiuyuan, Li Xingxue, Shen Guanglong, et al. New advance in the study of Carboniferous rocks of Jingyuan, eastern Gansu[J]. Journal of Stratigraphy, 1987, 11(3):163~179 ]
    [2] 甘肃省地质矿产局区调队.甘肃的石炭系[M]. 兰州:甘肃科学技术出版社, 1987[Area Geological Survey Team of Geological and Mineral Bureau of Gansu Province.Carboniferous System in Gansu Province [M]. Lanzhou: Gansu Science & Technology Press, 1987 ]
    [3] 甘肃省地质矿产局.甘肃省区域地质志,第19号[M].1989.171~202[Geological and Mineral Bureau of Gansu Province. Area Geological Records of Gansu Province, No.19 [M]. 1989. 171~202]
    [4] 王增吉等著.中国地层 8, 中国的石炭系[M].北京:地质出版社, 1990.67~92,377~388[Wang Zengji, et al. eds. Chinese Stratum 8, Chinese Carboniferous System [M].Beijing: Geological Publishing House, 1990. 67~92,377~388 ]
    [5] 霍福臣等.宁夏地质概论[M]. 北京:科学出版社,1989.118~149[Huo Fuchen,Pan Xingshi, You Guolin, et al. Introduction to geology of Ningxia[M].Beijing: Science Press, 1989. 118~149 ]
    [6] 吴秀元, 赵修衤右. 中国石炭纪陆相地层的划分和对比-中国各纪地层对比表及说明书[M].北京:科学出版社, 1982[Wu Xiuyuan, Zhao Xiuhu. Division and comparison of Chinese Carboniferous Terrestrial facies stratum-The table and explanation book of Chinese different Periods Strarum [M]. Beijing: Science Press, 1982]
    [7] 刘宝王君主编.沉积岩石学[M].北京:地质出版社,1980.99~136[Liu Baojun. edited.Sedimentary lithology[M].Beijing: Geology Press, 1980. 295~297 (in Chinese)]
    [8] Jason Hilton, Shi-Jun Wang, Jean Galtier, et al. An Early Permian plant assemblage from the Taiyuan Formation of North China with compression/impression and permineralized preservation[J]. Review of Palaeobotany & Palynology, 2001,114: 175~189
    [9] 余素玉, 何镜宇.沉积岩石学[M].北京:中国地质大学出版社, 1989[Yu Suyu, He Jingyu. Sedimentary lithology [M].Beijing: China Geology University Press, 1989]
    [10] Li X X, Shen G L, Tian B L,et al.Some notes of the Carboniferous and Permian floras in China[A]. In: Li X X,ed. Fossil floras of China through the geological ages(English Edition)[C]. Guangzhou: Guangdong Science and Technology Press, 1995. 244~304
    [11] Wu X Y. Carboniferous floras[A]. In: Li X X, ed.Fossil floras of China through the geological ages(English Edition)[C]. Guangzhou: Guangdong Science and Technology Press, 1995.78~118
    [12] Baochun Huang,Yo-ichiro Otofuji,Rixiang Zhu,et al. Paleomagnetism of Carboniferous Sediments in the Hexi Corridor:its origin andtectonic im plications [J].Earth and Planetary Science Letters,2001,194:135~149
    [13] 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[M].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[M]. Xi'an: Northwest University Press, 1989.1~136 ]
    [14] Richard C.Selley. Applied sedimentology, Second Edition[M]. London:United Kingdom, Academic Press, 2000.130~506
    [15] Gerhard Einsele. Sedimentary basins evolution,facies,and sediment budget[M]. Tubingen:Germany. 1992.29~53,94~176
    [16] 佟再三,李汉业. 北祁连东段石炭纪岩相古地理基本特征[J]. 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[J].Acta Sedimentologica Sinica, 1994, 20 (1): 89~97]
    [17] 佟再三,李汉业. 靖远磁窑晚石炭世沉积环境基本特征[J]. 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]
    [18] 煤炭科学研究院地质勘探分院等. 太原西山含煤地层沉积环境[M]. 北京: 煤炭工业出版社, 1987.485~533[Geological Prospect Branch of Coal Science Institute, et al. The sedimentary environment of coal-bearing strarum of Xishan,Taiyuan[M]. Beijing: Coal Industry Press, 1987.485~533]
    [19] 何宝珍,晁吉祥. 西北地区石炭纪古地理轮廓及沉积特征[J]. 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[J]. Coal Geology and Prospecting, 1982, (2): 14~20]
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  • 收稿日期:  2002-03-14
  • 修回日期:  2002-05-17
  • 刊出日期:  2003-09-10

目录

    甘肃景泰红水堡晚石炭世沉积环境与沉积相分析

      作者简介:

      谢小平,男,1966年出生,博士,讲师,沉积学

    • 中图分类号: P512.2;P534.45

    摘要: 甘肃省景泰县红水堡地处北祁连加里东褶皱带东段。晚石炭世地层包括红土洼组、羊虎沟组及太原组。根据岩性、颜色、粒度分析、沉积相标志及古生物组合并结合古生态、以及地球化学特征,将景泰红水堡晚石炭世沉积环境与沉积相划分为泻湖、潮坪、支间湾河口坝和三角洲平原。一个明显的陆源沉积物向海推进的海退序列.

    English Abstract

    谢小平, 佟再三, 沈焕庭. 甘肃景泰红水堡晚石炭世沉积环境与沉积相分析[J]. 沉积学报, 2003, 21(3): 381-390.
    引用本文: 谢小平, 佟再三, 沈焕庭. 甘肃景泰红水堡晚石炭世沉积环境与沉积相分析[J]. 沉积学报, 2003, 21(3): 381-390.
    XIE Xiao-ping, TONG Zai-san, SHEN Huan-ting. Analysis on Sedimentary Environment and Facies in Later Carboniferous Epoch of Hongshuibao, Jingtai County,Gansu Province[J]. Acta Sedimentologica Sinica, 2003, 21(3): 381-390.
    Citation: XIE Xiao-ping, TONG Zai-san, SHEN Huan-ting. Analysis on Sedimentary Environment and Facies in Later Carboniferous Epoch of Hongshuibao, Jingtai County,Gansu Province[J]. Acta Sedimentologica Sinica, 2003, 21(3): 381-390.
    参考文献 (19)

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