甘肃景泰红水堡晚石炭世沉积环境与沉积相分析

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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

文章导航 > 沉积学报 > 2003 > 21(3): 381-390

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.

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

1.
华东师范大学河口海岸国家重点实验室上海 200062;
2.
兰州大学地质系兰州 730000;
3.
曲阜师范大学地理系山东曲阜 273165

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

计量

文章访问数: 593
HTML全文浏览量: 21
PDF下载量: 508
被引次数: 0

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

1.
State Key Lab of Estuarine and Coastal Research, East China Normal Univers ity, Shanghai 200062;
2.
Geography Department of Qufu Normal University, Qufu Shandong 273165;
3.
Geology Department of Lanzhou University, Lanzhou 730000

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.
- 晚石炭世 /
- 沉积环境 /
- 沉积相 /
- 红水堡 /
- 甘肃景泰
Abstract: Hongshuibao is located in the northwest of Jingtai county, about 45km to the c ounty town, Gansu province. The area is in the east part of Caledonian folded belt of the North Qilian Mountain, stratigraphic units developed well. Fossils are abund ant, engage relationship is clear. The Upper Carboniferous Series is consists of Hongshuibao formation, Yanghugou formation and Taiyuan formation. Sedimentary e nvironment and facies changed from lagoon-tide flat, tributary river barrier t o the deltaic plain, clearly a regression sequence.
- Later Carboniferous epoch /
- sedimentary environment /
- sedimentary facies /
- Hongshuibao /
- Jingtai county

参考文献(19)

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计量

文章访问数: 593
HTML全文浏览量: 21
PDF下载量: 508
被引次数: 0

甘肃景泰红水堡晚石炭世沉积环境与沉积相分析

1. 华东师范大学河口海岸国家重点实验室上海 200062;

2. 兰州大学地质系兰州 730000;

3. 曲阜师范大学地理系山东曲阜 273165

作者简介:
谢小平,男,1966年出生,博士,讲师,沉积学

收稿日期: 2002-03-14
修回日期: 2002-05-17
刊出日期: 2003-09-10

中图分类号: P512.2;P534.45

关键词:

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.

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参考文献 (19)

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