造山带岩相古地理研究与实践&mdash;&mdash;以甘肃省奥陶纪为例

牟传龙; 王启宇; 王秀平; 陈小炜; 周恳恳; 葛祥英

doi:10.14027/j.cnki.cjxb.2016.01.001

ISSN 1000-0550 CN 62-1038/P

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造山带岩相古地理研究与实践——以甘肃省奥陶纪为例

牟传龙, 王启宇, 王秀平, 陈小炜, 周恳恳, 葛祥英

文章导航 > 沉积学报 > 2016 > 34(1): 1-14

牟传龙, 王启宇, 王秀平, 陈小炜, 周恳恳, 葛祥英. 造山带岩相古地理研究与实践——以甘肃省奥陶纪为例[J]. 沉积学报, 2016, 34(1): 1-14. doi: 10.14027/j.cnki.cjxb.2016.01.001

引用本文:

MOU ChuanLong, WANG QiYu, WANG XiuPing, CHEN XiaoWei, ZHOU KenKen, GE XiangYing. The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province[J]. Acta Sedimentologica Sinica, 2016, 34(1): 1-14. doi: 10.14027/j.cnki.cjxb.2016.01.001

Citation:

MOU ChuanLong, WANG QiYu, WANG XiuPing, CHEN XiaoWei, ZHOU KenKen, GE XiangYing. The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province[J]. Acta Sedimentologica Sinica, 2016, 34(1): 1-14. doi: 10.14027/j.cnki.cjxb.2016.01.001

引用本文:

Citation:

MOU ChuanLong, WANG QiYu, WANG XiuPing, CHEN XiaoWei, ZHOU KenKen, GE XiangYing. The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province[J]. Acta Sedimentologica Sinica, 2016, 34(1): 1-14. doi: 10.14027/j.cnki.cjxb.2016.01.001

造山带岩相古地理研究与实践——以甘肃省奥陶纪为例

doi: 10.14027/j.cnki.cjxb.2016.01.001

牟传龙^1,2,
王启宇^1,2,3,
王秀平^1,2,
陈小炜^1,2,
周恳恳^1,2,
葛祥英^1,2

1.
成都地质调查中心成都 610082;
2.
国土资源部沉积盆地与油气资源重点实验室成都 610082;
3.
山东科技大学山东青岛 266590

基金项目: 国家科技重大专项(2008ZX05043-005);中国地质调查局项目(1212010916060)

详细信息

作者简介:
牟传龙男 1965年出生研究员沉积地质与油气地质 E-mail: cdmchuanlong@163.com

中图分类号: P586;P531

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文章访问数: 415
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The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province

1.
Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China;
2.
Key Laboratory for Sedimentary Basin and Oil and Gas Resources, MLR, Chengdu 610082, China;
3.
Shangdong University of Science and Technology, Qingdao, Shandong 266590, China

Funds: Major National Science and Technology Project, NO.2008ZX05043-005; China Geological Survey Project, NO.1212010916060

摘要

摘要: 造山带古地理的恢复与重建难度较大且尚无研究方法体系可循。选择地处复杂中央造山带的甘肃省奥陶纪为例,结合前人研究资料首次编制了早、中晚奥陶世的沉积构造格架及沉积盆地类型图,分析了它们之间的空间配置关系。在“构造控盆、盆控相”的思路控制下,以沉积岩性、结构—构造、古生物组合等为基础,以优势相原则,共划分出滨浅海相、浅海陆棚相、开阔台地相、台地边缘浅滩相、潮坪相以及半深海(含斜坡相)—深海相等7类沉积相类型,采用“在同一板块、构造背景下形成的沉积盆地内及空间连续配置的沉积盆地之间采用瓦尔特相律对古地理进行合理的恢复;对不同的板块及构造背景下形成的沉积盆地或者是空间不连续配置的沉积盆地之间,古地理单元的恢复则按现今出露地层所反应出的沉积环境忠实地表现,古地理单元之间可以不遵循瓦尔特相律”的方法恢复与重建了研究区的古地理面貌,编制了相应的古地理图。为造山带岩相古地理的研究提供了一种编图思路,具理论和实践意义。
- 造山带 /
- 甘肃省 /
- 奥陶纪 /
- 构造 /
- 瓦尔特相律 /
- 沉积相 /
- 岩相古地理
Abstract: It's difficult to restore and reconstruct the palaeogeographic of the orogenic belt, and there was no research method system to follow. Ordovician in Gansu province was the study target. Combined with the existing study, compiled the sedimentary tectonic map and the sedimentary basin type map of the Lower-Middle-Late Ordovician, the relationship of spatial disposition between them was analyzed. Under the "basin-controlling tectonic, facies-controlling basin" thought, on the basis of the sedimentary lithology, texture-structure and the paleontological, and using the dominant facies principle, littoral-neritic facies, shelf facies, open sea platform facies, platform margin shoals facies, tidal flat facies, bathyal facies (including slope facies) and abyssal facies were figured outin study area. "In the same plate and the same tectonic settings, or in the sedimentary basin which have the space connection configuration, the Walther facies law was used to restore the paleogeographic of the basin. However, restoring paleogeographic of the basin by the real sedimentary environment of the emergence stratums, Palaeogeographic units can't follow the Walther facies law." Under the guidance of the principle, Paleogeography of the study area was restored and rebuilt, also, the corresponding paleogeographic map was established. It provides a mapping train of restoring lithofacies-paleogeographic for orogenic belt, which has the theoretical and practical significance.
- orogenic belt /
- Gansu province /
- Ordovician structure /
- Walther facies /
- sedimentary facies /
- lithofacies-palaeogeography /

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[1]	闫伟, 刘洋, 郭玮, 周黎霞, 蔡郑红, 黄正良. 鄂尔多斯盆地西部奥陶纪乌拉力克期岩相古地理特征【鄂尔多斯盆地乌拉力克组海相页岩气勘探专辑】 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.096
[2]	杨帅, 陈安清, 张玺华, 李乾, 徐胜林, 陈聪, 孙诗, 李富祥, 罗倩, 文龙, 陈洪德. 四川盆地二叠纪栖霞—茅口期古地理格局转换及勘探启示 . 沉积学报, 2021, 39(6): 1466-1477. doi: 10.14027/j.issn.1000-0550.2021.072
[3]	王秀平, 牟传龙, 王启宇, 周恳恳, 梁薇, 葛祥英, 陈小炜. 再论岩相古地理可作为页岩气地质调查之指南 . 沉积学报, 2018, 36(2): 215-231. doi: 10.14027/j.issn.1000-0550.2018.001
[4]	胡光明, 李国栋, 魏新善, 李雁冰. 靖边潜台西侧奥陶系马五₄亚段岩相古地理特征 . 沉积学报, 2017, 35(3): 527-539. doi: 10.14027/j.cnki.cjxb.2017.03.011
[5]	杨华, 傅强, 齐亚林, 周新平, 龚宁, 黄少雄. 鄂尔多斯盆地晚三叠世延长期古湖盆生物相带划分及地质意义 . 沉积学报, 2016, 34(4): 688-693. doi: 10.14027/j.cnki.cjxb.2016.04.009
[6]	. 湖南晚奥陶世凯迪晚期—赫南特期沉积相及岩相古地理 . 沉积学报, 2014, 32(1): 8-18.
[7]	. 新疆北部石炭纪岩相古地理 . 沉积学报, 2013, 31(04): 571-579.
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造山带岩相古地理研究与实践——以甘肃省奥陶纪为例

doi: 10.14027/j.cnki.cjxb.2016.01.001

1. 成都地质调查中心成都 610082;

2. 国土资源部沉积盆地与油气资源重点实验室成都 610082;

3. 山东科技大学山东青岛 266590

基金项目: 国家科技重大专项(2008ZX05043-005);中国地质调查局项目(1212010916060)

作者简介:
牟传龙男 1965年出生研究员沉积地质与油气地质 E-mail: cdmchuanlong@163.com

收稿日期: 2014-09-02
修回日期: 2014-11-06
刊出日期: 2016-02-10

中图分类号: P586;P531

关键词:

造山带 /

甘肃省 /

奥陶纪 /

构造 /

瓦尔特相律 /

沉积相 /

岩相古地理

摘要: 造山带古地理的恢复与重建难度较大且尚无研究方法体系可循。选择地处复杂中央造山带的甘肃省奥陶纪为例,结合前人研究资料首次编制了早、中晚奥陶世的沉积构造格架及沉积盆地类型图,分析了它们之间的空间配置关系。在“构造控盆、盆控相”的思路控制下,以沉积岩性、结构—构造、古生物组合等为基础,以优势相原则,共划分出滨浅海相、浅海陆棚相、开阔台地相、台地边缘浅滩相、潮坪相以及半深海(含斜坡相)—深海相等7类沉积相类型,采用“在同一板块、构造背景下形成的沉积盆地内及空间连续配置的沉积盆地之间采用瓦尔特相律对古地理进行合理的恢复;对不同的板块及构造背景下形成的沉积盆地或者是空间不连续配置的沉积盆地之间,古地理单元的恢复则按现今出露地层所反应出的沉积环境忠实地表现,古地理单元之间可以不遵循瓦尔特相律”的方法恢复与重建了研究区的古地理面貌,编制了相应的古地理图。为造山带岩相古地理的研究提供了一种编图思路,具理论和实践意义。

English Abstract

The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province

1. Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China;

2. Key Laboratory for Sedimentary Basin and Oil and Gas Resources, MLR, Chengdu 610082, China;

3. Shangdong University of Science and Technology, Qingdao, Shandong 266590, China

Funds: Major National Science and Technology Project, NO.2008ZX05043-005; China Geological Survey Project, NO.1212010916060

Received Date: 2014-09-02
Rev Recd Date: 2014-11-06
Publish Date: 2016-02-10

Keywords:

Abstract: It's difficult to restore and reconstruct the palaeogeographic of the orogenic belt, and there was no research method system to follow. Ordovician in Gansu province was the study target. Combined with the existing study, compiled the sedimentary tectonic map and the sedimentary basin type map of the Lower-Middle-Late Ordovician, the relationship of spatial disposition between them was analyzed. Under the "basin-controlling tectonic, facies-controlling basin" thought, on the basis of the sedimentary lithology, texture-structure and the paleontological, and using the dominant facies principle, littoral-neritic facies, shelf facies, open sea platform facies, platform margin shoals facies, tidal flat facies, bathyal facies (including slope facies) and abyssal facies were figured outin study area. "In the same plate and the same tectonic settings, or in the sedimentary basin which have the space connection configuration, the Walther facies law was used to restore the paleogeographic of the basin. However, restoring paleogeographic of the basin by the real sedimentary environment of the emergence stratums, Palaeogeographic units can't follow the Walther facies law." Under the guidance of the principle, Paleogeography of the study area was restored and rebuilt, also, the corresponding paleogeographic map was established. It provides a mapping train of restoring lithofacies-paleogeographic for orogenic belt, which has the theoretical and practical significance.

引用本文:

Citation:

MOU ChuanLong, WANG QiYu, WANG XiuPing, CHEN XiaoWei, ZHOU KenKen, GE XiangYing. The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province[J]. Acta Sedimentologica Sinica, 2016, 34(1): 1-14. doi: 10.14027/j.cnki.cjxb.2016.01.001

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造山带岩相古地理研究与实践——以甘肃省奥陶纪为例

doi: 10.14027/j.cnki.cjxb.2016.01.001

作者简介:
牟传龙男 1965年出生研究员沉积地质与油气地质 E-mail: cdmchuanlong@163.com

计量

The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province

计量

目录

造山带岩相古地理研究与实践——以甘肃省奥陶纪为例

doi: 10.14027/j.cnki.cjxb.2016.01.001

1. 成都地质调查中心成都 610082;

2. 国土资源部沉积盆地与油气资源重点实验室成都 610082;

3. 山东科技大学山东青岛 266590

作者简介:
牟传龙男 1965年出生研究员沉积地质与油气地质 E-mail: cdmchuanlong@163.com

English Abstract

The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province

1. Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China;

2. Key Laboratory for Sedimentary Basin and Oil and Gas Resources, MLR, Chengdu 610082, China;

3. Shangdong University of Science and Technology, Qingdao, Shandong 266590, China

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造山带岩相古地理研究与实践——以甘肃省奥陶纪为例

doi: 10.14027/j.cnki.cjxb.2016.01.001

作者简介: 牟传龙 男 1965年出生 研究员 沉积地质与油气地质 E-mail: cdmchuanlong@163.com

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The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province

计量

出版历程

目录

造山带岩相古地理研究与实践——以甘肃省奥陶纪为例

doi: 10.14027/j.cnki.cjxb.2016.01.001

1. 成都地质调查中心 成都 610082; 2. 国土资源部沉积盆地与油气资源重点实验室 成都 610082; 3. 山东科技大学 山东青岛 266590

作者简介: 牟传龙 男 1965年出生 研究员 沉积地质与油气地质 E-mail: cdmchuanlong@163.com

English Abstract

The Lithofacies-palaeogeographic Research and Practice of Orogenic Belt: An example of Ordovician in Gansu province

1. Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China; 2. Key Laboratory for Sedimentary Basin and Oil and Gas Resources, MLR, Chengdu 610082, China; 3. Shangdong University of Science and Technology, Qingdao, Shandong 266590, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
牟传龙男 1965年出生研究员沉积地质与油气地质 E-mail: cdmchuanlong@163.com

1. 成都地质调查中心成都 610082;

2. 国土资源部沉积盆地与油气资源重点实验室成都 610082;

3. 山东科技大学山东青岛 266590

作者简介:
牟传龙男 1965年出生研究员沉积地质与油气地质 E-mail: cdmchuanlong@163.com

1. Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China;

2. Key Laboratory for Sedimentary Basin and Oil and Gas Resources, MLR, Chengdu 610082, China;

3. Shangdong University of Science and Technology, Qingdao, Shandong 266590, China