南盘江盆地中北部三叠纪深水盆地古水流方向研究

彭成名; 王刚; 陈原林; 李正友; 薛灵文; 杨慧; 卢应辉; 侯芸

doi:10.14027/j.cnki.cjxb.2016.06.010

ISSN 1000-0550 CN 62-1038/P

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南盘江盆地中北部三叠纪深水盆地古水流方向研究

彭成名, 王刚, 陈原林, 李正友, 薛灵文, 杨慧, 卢应辉, 侯芸

文章导航 > 沉积学报 > 2016 > 34(6): 1120-1132

彭成名, 王刚, 陈原林, 李正友, 薛灵文, 杨慧, 卢应辉, 侯芸. 南盘江盆地中北部三叠纪深水盆地古水流方向研究[J]. 沉积学报, 2016, 34(6): 1120-1132. doi: 10.14027/j.cnki.cjxb.2016.06.010

引用本文:

PENG ChengMing, WANG Gang, CHEN YuanLin, LI ZhengYou, XUE LingWen, YANG Hui, LU YingHui, HOU Yun. Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin[J]. Acta Sedimentologica Sinica, 2016, 34(6): 1120-1132. doi: 10.14027/j.cnki.cjxb.2016.06.010

Citation:

PENG ChengMing, WANG Gang, CHEN YuanLin, LI ZhengYou, XUE LingWen, YANG Hui, LU YingHui, HOU Yun. Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin[J]. Acta Sedimentologica Sinica, 2016, 34(6): 1120-1132. doi: 10.14027/j.cnki.cjxb.2016.06.010

引用本文:

Citation:

PENG ChengMing, WANG Gang, CHEN YuanLin, LI ZhengYou, XUE LingWen, YANG Hui, LU YingHui, HOU Yun. Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin[J]. Acta Sedimentologica Sinica, 2016, 34(6): 1120-1132. doi: 10.14027/j.cnki.cjxb.2016.06.010

南盘江盆地中北部三叠纪深水盆地古水流方向研究

doi: 10.14027/j.cnki.cjxb.2016.06.010

彭成名^1,2,
王刚^1,2,3,
陈原林^4,,
李正友¹,
薛灵文¹,
杨慧^2,5,
卢应辉⁶,
侯芸¹

1.
成都理工大学地球科学学院成都 610059;
2.
油气藏地质及开发工程国家重点实验室(成都理工大学) 成都 610059;
3.
国土资源部构造成矿成藏重点实验室(成都理工大学) 成都 610059;
4.
贵州大学资源与环境工程学院贵阳 550025;
5.
成都理工大学能源学院成都 610059;
6.
江西省世纪矿业有限公司南昌 330002

基金项目: 中国地质调查局项目（1212011367500）

详细信息

作者简介:
彭成名,男,1989年出生,硕士,沉积盆地分析,E-mail:pcm_1214@126.com

通讯作者:
陈原林,男,硕士,E-mail:gs.ylchen14@mail.gzu.edu.cn

中图分类号: P534.51

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文章访问数: 654
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PDF下载量: 1251
被引次数: 0

Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin

1.
College of Earth Science, Chengdu University of Technology, Chengdu 610059, China;
2.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059, China;
3.
Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation of Ministry of Land and Resources(Chengdu University of Technology), Chengdu 610059, China;
4.
College of Resource and Environmental Engineering, Guizhou University, Guiyang 550025, China;
5.
College of Energy, Chengdu University of Technology, Chengdu 610059, China;
6.
Jiangxi Century Mining Co., LTD, Nanchang 330002, China

Funds: China Geological Survey Project,No.1212011367500

摘要

摘要: 南盘江盆地位于中国广西、贵州、云南三省毗邻地区，为晚二叠世-三叠纪期间演化的海相沉积盆地，建立在晚二叠世开始的裂谷系统基础之上，进入三叠纪中期，盆地范围进一步扩展、海水深度进一步加深，盆地内部主要沉积了一套深水复理石，晚三叠世沉积环境为前陆盆地，在盆地北部沉积有碎屑岩和碳酸盐岩建造。针对南盘江盆地中北部深水复理石沉积，测量了鲍马序列C段中的小型斜层理、爬升层理、包卷层理轴面倒向、槽模等反映古水流方向的沉积构造的产状，通过野外和室内复平面校正、古流向玫瑰花图的绘制，对研究区三叠纪古流向进行了系统研究，共获得49组古流向测量数据，通过古流向分析并结合沉积环境演化特征，对南盘江盆地物源区进行了讨论。研究结果认为中三叠世期间盆地南部广南、底圩、八达、富宁一线物源区来自南部的越北古陆；盆地东部的巴马、龙川、望谟一线物源区来自于东部及北东的江南古陆；盆地北部物源区位于盆地西北部和北部的扬子台地内部；盆地的沉积中心位于册亨以南、潞城以北地区；隆林县城和西林县城之间、阳圩和剥隘之间存在古隆起。晚三叠世期间盆地北部古流向发生明显变化，应与构造体制的变化密切相关。
- 南盘江盆地 /
- 三叠纪 /
- 复理石 /
- 鲍马序列 /
- 古水流
Abstract: The later Permian-Triassic Nanpanjiang deep marine basin is located in the adjacent areas among Guangxi, Guizhou, and Yunnan, which developed based on the rift system during the later Permian. The space and the depth of the basin increased during the middle-Triassic and a set of deepwater flysch sediment was preserved in the basin. The environment of the basin was identified as foreland basin where there was a set of clastic and carbonate sediment in the northern part of the basin. The main study areas lie in the northern and middle part of the Nanpanjiang Basin(NPJB). Some kinds of flysch sedimentary structures can be used in the field work to get paleocurrent such as small oblique bedding, small climbing ripple bedding, convolute bedding, flute cast and so on. Based on the field measurement, stratum attitude correction and the rose diagrams drawing of paleocurrent, this article discusses the paleocurrent of the sediment during the Triassic time. 49 sets of paleocurrent data were exhibited here by which sedimentary provenances of NPJB can be constrained. During the middle Triassic time the sedimentary provenance of the southern part of NPJB(for example near Guangnan, Dixu, Bada, Funing) would be the Vietnam Block to the south of NPJB, the sedimentary provenance of the eastern part of NPJB(for example near Bama, Longchuan, Wangmo) would be the Jiangnan Block to the east, and the sedimentary provenance of the northern part of NPJB would be the inner Yangtze Platform to the north. The centre of subsidence is located at the areas south to Ceheng and north to Lucheng. Two palaeohigh belts were indentified between Longlin city and Xilin city, between Yangxu town and Boai town. The paleocurrent changed significantly during the late Triassic time at the northern part of the NPJB which was considered as a consequence of the tectonic fragment change.
- Nanpanjiang Basin /
- Triassic /
- flysch /
- Bouma sequence /
- paleocurrent

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[1]	张新智, 吕沛宗, 方琳浩, 杨涵, 邓胜徽, 卢远征, 房亚男, 张小宇, 黄汝婷, 梁佳宝, 师生宝. 三叠纪—侏罗纪之交准噶尔盆地南缘野火记录及全球对比 . 沉积学报, 2022, 40(2): 473-483. doi: 10.14027/j.issn.1000-0550.2020.103
[2]	彭深远, 杨文涛, 张鸿禹, 方特. 华北盆地三叠纪物源特征及其沉积—构造演化 . 沉积学报, 2022, 40(5): 1228-1249. doi: 10.14027/j.issn.1000-0550.2021.021
[3]	龚大兴, 郭佳, 罗俊峰, 岳相元, 周雄, 周家云. 川西马尔康—金川地区晚三叠世松潘甘孜残留洋盆复理石建造沉积特征与沉积模式 . 沉积学报, 2019, 37(6): 1210-1223. doi: 10.14027/j.issn.1000-0550.2019.031
[4]	梁飞, 黄文辉, 牛君. 鄂尔多斯盆地西南缘二叠系山西组山1段-下石盒子组盒8段物源分析 . 沉积学报, 2018, 36(1): 142-153. doi: 10.3969/j.issn.1000-0550.2018.016
[5]	. 西藏山南地区上三叠统复理石郎杰学群岩性分布样式及其意义 . 沉积学报, 2014, 32(1): 36-43.
[6]	. 鸡西盆地早白垩世城子河组和穆棱组物源分析 . 沉积学报, 2012, 30(4): 661-671.
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[9]	刘志飞, LachlanK.Stewart. 图形显示和比较古水流数据的一种软件(PC99):以青藏高原北部可可西里盆地新生代古水流数据为例 . 沉积学报, 2002, 20(2): 354-358.
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南盘江盆地中北部三叠纪深水盆地古水流方向研究

doi: 10.14027/j.cnki.cjxb.2016.06.010

1. 成都理工大学地球科学学院成都 610059;

2. 油气藏地质及开发工程国家重点实验室(成都理工大学) 成都 610059;

3. 国土资源部构造成矿成藏重点实验室(成都理工大学) 成都 610059;

4. 贵州大学资源与环境工程学院贵阳 550025;

5. 成都理工大学能源学院成都 610059;

6. 江西省世纪矿业有限公司南昌 330002

基金项目: 中国地质调查局项目（1212011367500）

作者简介:
彭成名,男,1989年出生,硕士,沉积盆地分析,E-mail:pcm_1214@126.com

通讯作者: 陈原林,男,硕士,E-mail:gs.ylchen14@mail.gzu.edu.cn

收稿日期: 2015-12-11
修回日期: 2016-02-02
刊出日期: 2016-12-10

中图分类号: P534.51

关键词:

南盘江盆地 /

三叠纪 /

复理石 /

鲍马序列 /

古水流

摘要: 南盘江盆地位于中国广西、贵州、云南三省毗邻地区，为晚二叠世-三叠纪期间演化的海相沉积盆地，建立在晚二叠世开始的裂谷系统基础之上，进入三叠纪中期，盆地范围进一步扩展、海水深度进一步加深，盆地内部主要沉积了一套深水复理石，晚三叠世沉积环境为前陆盆地，在盆地北部沉积有碎屑岩和碳酸盐岩建造。针对南盘江盆地中北部深水复理石沉积，测量了鲍马序列C段中的小型斜层理、爬升层理、包卷层理轴面倒向、槽模等反映古水流方向的沉积构造的产状，通过野外和室内复平面校正、古流向玫瑰花图的绘制，对研究区三叠纪古流向进行了系统研究，共获得49组古流向测量数据，通过古流向分析并结合沉积环境演化特征，对南盘江盆地物源区进行了讨论。研究结果认为中三叠世期间盆地南部广南、底圩、八达、富宁一线物源区来自南部的越北古陆；盆地东部的巴马、龙川、望谟一线物源区来自于东部及北东的江南古陆；盆地北部物源区位于盆地西北部和北部的扬子台地内部；盆地的沉积中心位于册亨以南、潞城以北地区；隆林县城和西林县城之间、阳圩和剥隘之间存在古隆起。晚三叠世期间盆地北部古流向发生明显变化，应与构造体制的变化密切相关。

English Abstract

Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin

1. College of Earth Science, Chengdu University of Technology, Chengdu 610059, China;

2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059, China;

3. Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation of Ministry of Land and Resources(Chengdu University of Technology), Chengdu 610059, China;

4. College of Resource and Environmental Engineering, Guizhou University, Guiyang 550025, China;

5. College of Energy, Chengdu University of Technology, Chengdu 610059, China;

6. Jiangxi Century Mining Co., LTD, Nanchang 330002, China

Funds: China Geological Survey Project,No.1212011367500

Received Date: 2015-12-11
Rev Recd Date: 2016-02-02
Publish Date: 2016-12-10

Keywords:

Abstract: The later Permian-Triassic Nanpanjiang deep marine basin is located in the adjacent areas among Guangxi, Guizhou, and Yunnan, which developed based on the rift system during the later Permian. The space and the depth of the basin increased during the middle-Triassic and a set of deepwater flysch sediment was preserved in the basin. The environment of the basin was identified as foreland basin where there was a set of clastic and carbonate sediment in the northern part of the basin. The main study areas lie in the northern and middle part of the Nanpanjiang Basin(NPJB). Some kinds of flysch sedimentary structures can be used in the field work to get paleocurrent such as small oblique bedding, small climbing ripple bedding, convolute bedding, flute cast and so on. Based on the field measurement, stratum attitude correction and the rose diagrams drawing of paleocurrent, this article discusses the paleocurrent of the sediment during the Triassic time. 49 sets of paleocurrent data were exhibited here by which sedimentary provenances of NPJB can be constrained. During the middle Triassic time the sedimentary provenance of the southern part of NPJB(for example near Guangnan, Dixu, Bada, Funing) would be the Vietnam Block to the south of NPJB, the sedimentary provenance of the eastern part of NPJB(for example near Bama, Longchuan, Wangmo) would be the Jiangnan Block to the east, and the sedimentary provenance of the northern part of NPJB would be the inner Yangtze Platform to the north. The centre of subsidence is located at the areas south to Ceheng and north to Lucheng. Two palaeohigh belts were indentified between Longlin city and Xilin city, between Yangxu town and Boai town. The paleocurrent changed significantly during the late Triassic time at the northern part of the NPJB which was considered as a consequence of the tectonic fragment change.

引用本文:

Citation:

PENG ChengMing, WANG Gang, CHEN YuanLin, LI ZhengYou, XUE LingWen, YANG Hui, LU YingHui, HOU Yun. Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin[J]. Acta Sedimentologica Sinica, 2016, 34(6): 1120-1132. doi: 10.14027/j.cnki.cjxb.2016.06.010

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南盘江盆地中北部三叠纪深水盆地古水流方向研究

doi: 10.14027/j.cnki.cjxb.2016.06.010

作者简介:
彭成名,男,1989年出生,硕士,沉积盆地分析,E-mail:pcm_1214@126.com

通讯作者:
陈原林,男,硕士,E-mail:gs.ylchen14@mail.gzu.edu.cn

计量

Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin

计量

目录

南盘江盆地中北部三叠纪深水盆地古水流方向研究

doi: 10.14027/j.cnki.cjxb.2016.06.010

作者简介:
彭成名,男,1989年出生,硕士,沉积盆地分析,E-mail:pcm_1214@126.com

通讯作者: 陈原林,男,硕士,E-mail:gs.ylchen14@mail.gzu.edu.cn

English Abstract

Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin

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南盘江盆地中北部三叠纪深水盆地古水流方向研究

doi: 10.14027/j.cnki.cjxb.2016.06.010

作者简介: 彭成名,男,1989年出生,硕士,沉积盆地分析,E-mail:pcm_1214@126.com

通讯作者: 陈原林,男,硕士,E-mail:gs.ylchen14@mail.gzu.edu.cn

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出版历程

Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin

计量

出版历程

目录

南盘江盆地中北部三叠纪深水盆地古水流方向研究

doi: 10.14027/j.cnki.cjxb.2016.06.010

作者简介: 彭成名,男,1989年出生,硕士,沉积盆地分析,E-mail:pcm_1214@126.com

通讯作者: 陈原林,男,硕士,E-mail:gs.ylchen14@mail.gzu.edu.cn

English Abstract

Triassic Paleocurrent Study in the Middle-northern Part of the Nanpanjiang Deep Basin

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
彭成名,男,1989年出生,硕士,沉积盆地分析,E-mail:pcm_1214@126.com

通讯作者:
陈原林,男,硕士,E-mail:gs.ylchen14@mail.gzu.edu.cn

作者简介:
彭成名,男,1989年出生,硕士,沉积盆地分析,E-mail:pcm_1214@126.com