汉南&mdash;川东北灯影组古地理演化：晚震旦世扬子西北缘拉张背景的沉积学证据

杨瑞青; 杨风丽; 周晓峰; 周志

doi:10.14027/j.issn.1000-0550.2018.146

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

汉南—川东北灯影组古地理演化：晚震旦世扬子西北缘拉张背景的沉积学证据

杨瑞青, 杨风丽, 周晓峰, 周志

文章导航 > 沉积学报 > 2019 > 37(1): 189-199

杨瑞青, 杨风丽, 周晓峰, 周志. 汉南—川东北灯影组古地理演化：晚震旦世扬子西北缘拉张背景的沉积学证据[J]. 沉积学报, 2019, 37(1): 189-199. doi: 10.14027/j.issn.1000-0550.2018.146

引用本文:

YANG RuiQing, YANG FengLi, ZHOU XiaoFeng, ZHOU Zhi. Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian[J]. Acta Sedimentologica Sinica, 2019, 37(1): 189-199. doi: 10.14027/j.issn.1000-0550.2018.146

Citation:

YANG RuiQing, YANG FengLi, ZHOU XiaoFeng, ZHOU Zhi. Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian[J]. Acta Sedimentologica Sinica, 2019, 37(1): 189-199. doi: 10.14027/j.issn.1000-0550.2018.146

引用本文:

Citation:

YANG RuiQing, YANG FengLi, ZHOU XiaoFeng, ZHOU Zhi. Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian[J]. Acta Sedimentologica Sinica, 2019, 37(1): 189-199. doi: 10.14027/j.issn.1000-0550.2018.146

汉南—川东北灯影组古地理演化：晚震旦世扬子西北缘拉张背景的沉积学证据

doi: 10.14027/j.issn.1000-0550.2018.146

杨瑞青^1,2,
杨风丽^1,2,,
周晓峰²,
周志³

1.
同济大学海洋地质国家重点实验室, 上海 200092;
2.
同济大学海洋与地球科学学院, 上海 200092;
3.
中国地质调查局油气资源调查中心, 北京 100083

基金项目: 国家重点研发计划项目（2016YFC0601005）；国家科技重大专项（2016ZX05034）；中央高校基本科研业务费专项资金（22120180128）

详细信息

作者简介:
杨瑞青,女,1993年出生,硕士,沉积古环境,E-mail:rqyang@tongji.edu.cn

通讯作者:
杨风丽,女,教授,E-mail:yangfl@tongji.edu.cn

中图分类号: P618.13;P534.31

计量

文章访问数: 493
HTML全文浏览量: 16
PDF下载量: 252
被引次数: 0

Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian

1.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;
2.
School of Ocean and Earth Science, Tongji University, Shanghai 200092, China;
3.
Oil & Gas Survey, China Geology Survey, Beijing 100083, China

Funds: the National Key Research and Development Program of China, No. 2016YFC0601005; National Science and Technology Major Project,No. 2016ZX05034; the Fundamental Research Funds for the Central Universities, No. 22120180128

摘要

摘要: 古地理面貌的呈现往往是构造演化与沉积充填共同作用的结果。通过对野外露头系统的观察与分析，在汉南—川东北地区进行了晚震旦世灯影期沉积相分析，识别出古隆起、局限台地、开阔台地和台缘斜坡4种类型的古地理单元；确定了汉南—川东北地区地势南高北低、各沉积单元呈南北向和北东向展布，且在平面上呈现“一隆两凹”的古地理面貌特征。在露头及盆地内钻井岩芯识别出的同沉积断层等特征，反映了沉积区处于拉张构造背景；且古地理研究中所确定的沉积坳陷区与隆起区的位置与重磁震等地球物理资料中识别出的裂陷/坳陷和古隆起位置相吻合，证实了四川盆地内绵竹—乐至—隆昌—长宁拉张槽/裂陷槽和万源—达州裂陷槽的存在，表明灯影期汉南—川东北地区处于拉张的构造背景，反映古地理背景发生了由稳定沉积到活动拉张的变化，并且经历了稳定沉积、拉张前奏和主体拉张三个阶段，进一步印证了沉积演化与构造背景之间的耦合关系。
- 灯影组 /
- 古地理演化 /
- 拉张背景 /
- 汉南&mdash /
- 川东北
Abstract: The appearance of paleogeography is the result of the joint action of tectonic evolution and sedimentary filling. In this study, which was based on previous research and exploration results, systematic observations and analyses of the field outcrops in Hannan-Northeastern Sichuan Basin were conducted. The results reveal that there are four types of paleogeographic units in Dengying Formation in the Late Sinian: ancient Hannan paleo-uplift， restricted platforms open platforms and slopes. The terrain in the northeastern part of the Hannan-Northeastern Sichuan Basin is lowest in the south and highest in the north; the depositional elements are distributed in the north-south and northeasterly directions. The paleogeographic appearance in the study area was of “one uplift, two depressions”. It is suggested that the study area was in an extensional setting, which is reflected by the characteristics of co-sedimentary faults identified from outcrops and drillings. In addition, the location of the rift/depression identified in the geophysical data is consistent with the location of the ancient land on the paleogeographic map. This confirms the existence of the Mianzhu-Lezhi-Longchang-Changning pull/rift and Wanyuan-Dazhou rift in Sichuan Basin, and also indicates an extensional setting in the study area during the Dengying period. The paleogeographic background was transformed from one of stable deposition to active extension, and experienced stable deposition, prelude and main extension. Thus, this study further indicates the coupling relationship between sedimentary evolution and tectonic setting.
- Dengying Formation /
- paleogeographic evolution /
- extensional tectonic setting /
- Hannan-northeastern Sichuan /

HTML全文

参考文献(0)

[1]	姚鑫阳, 胡忠贵, 武赛军, 谢武仁, 杨帅奇, 姚敏, 毕宇航. 川东北地区开江-梁平海槽东侧长兴组沉积特征及有利区预测【华南古大陆演化及其资源效应专辑】 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.043
[2]	张敬轩, 罗翠, 王夏, 张磊, 刘倩, 李星霖, 张木辉, 潘松圻. 川东北灯影组克劳德管富集层及其储集特征分析 . 沉积学报, 2024, 42(4): 1185-1199. doi: 10.14027/j.issn.1000-0550.2024.049
[3]	谷一凡. 川中震旦系灯影组古岩溶储层成岩序列及其成储-成藏效应【“华南古大陆演化及其资源环境效应”专辑】 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.098
[4]	丁一, 刘树根, 文龙, 文华国, 陈代钊, 宋金民, 王瀚, 王林康, 陈明思, 陈荣庆, 李智武. 中上扬子地区震旦纪灯影组沉积期碳酸盐岩台地古地理格局及有利储集相带分布规律 . 沉积学报, 2024, 42(3): 928-943. doi: 10.14027/j.issn.1000-0550.2023.135
[5]	李安鹏, 高达, 胡明毅, 赵玉茹, 朱传勇, 戴逸晨. 川中地区灯影组四段微生物岩沉积模式及主控因素 . 沉积学报, 2023, 41(4): 1080-1096. doi: 10.14027/j.issn.1000-0550.2021.156
[6]	王仲学, 丁仲昭, 樊鑫, 戴霜, 马欢欢. 甘肃陇东新庄井田延安组沉积环境分析 . 沉积学报, 2023, 41(2): 545-558. doi: 10.14027/j.issn.1000-0550.2022.077
[7]	赵坤, 满玲, 贺然, 李松倬, 祝圣贤, 郎咸国. 川东北地区晚埃迪卡拉纪灯影期海水氧化还原环境重建 . 沉积学报, 2023, 41(1): 183-195. doi: 10.14027/j.issn.1000-0550.2021.083
[8]	张云峰, 唐雨, 唐洪明, 孙尧斌, 屈海洲, 王振宇, 刘冬玺. 川西北杨坝剖面埃迪卡拉系灯影组核形石组构特征 . 沉积学报, 2022, 40(5): 1302-1312. doi: 10.14027/j.issn.1000-0550.2021.046
[9]	宋泽章, 柳广弟, 罗冰, 曾庆才, 田兴旺, 戴鑫, 姜仁, 王云龙, 李强, 赵珺仪, 阿比德·阿不拉null, 臧建鹏. 深层、超深层致密碳酸盐岩储层固态沥青测井评价 . 沉积学报, 2021, 39(1): 197-211. doi: 10.14027/j.issn.1000-0550.2020.127
[10]	余晶洁, 宋金民, 刘树根, 杨迪, 王瀚, 赵聪, 邓双林, 何宇, 李立基. 川东北地区下寒武统龙王庙组白云岩成因分析 . 沉积学报, 2020, 38(6): 1284-1295. doi: 10.14027/j.issn.1000-0550.2019.108
[11]	金民东, 谭秀成, 李毕松, 朱祥, 曾伟, 连承波. 四川盆地震旦系灯影组白云岩成因 . 沉积学报, 2019, 37(3): 443-454. doi: 10.14027/j.issn.1000-0550.2018.148
[12]	林孝先, 彭军, 侯中健, 韩浩东, 李旭杰, 马春疆. 四川汉源-峨边地区上震旦统灯影组藻白云岩特征及成因研究 . 沉积学报, 2018, 36(1): 57-71. doi: 10.3969/j.issn.1000-0550.2018.008
[13]	蒋裕强, 谷一凡, 刘均, 邓吉刚, 张洁伟, 张航, 徐艳霞. 川东北龙岗东地区二叠系-三叠系热液活动证据及意义 . 沉积学报, 2018, 36(1): 1-11. doi: 10.3969/j.issn.1000-0550.2018.002
[14]	牟传龙, 王秀平, 梁薇, 王远翀, 门欣. 上扬子区灯影组白云岩葡萄体特征及成因初探——以南江杨坝地区灯影组一段为例 . 沉积学报, 2015, 33(6): 1097-1110. doi: 10.14027/j.cnki.cjxb.2015.06.004
[15]	陈梅. C、O同位素在川东北碳酸盐岩储层研究中的应用 . 沉积学报, 2011, 29(2): 217-225.
[16]	乔占峰. 川东北地区飞仙关组层序地层特征及演化模式 . 沉积学报, 2010, 28(3): 462-470.
[17]	郑荣才. 川东北地区飞仙关组层序—岩相古地理特征和鲕滩预测 . 沉积学报, 2009, 27(1): 1-8.
[18]	方少仙, 侯方浩, 董兆雄. 上震旦统灯影组中非叠层石生态系兰细菌白云岩 . 沉积学报, 2003, 21(1): 96-105.
[19]	向芳, 陈洪德, 张锦泉. 资阳地区震旦系古岩溶作用及其特征讨论 . 沉积学报, 2001, 19(3): 421-424.
[20]	王兴志, 穆曙光, 方少仙, 侯方浩, 黄继祥. 四川资阳地区灯影组滩相沉积及储集性研究 . 沉积学报, 1999, 17(4): 578-583.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 493
HTML全文浏览量: 16
PDF下载量: 252
被引次数: 0

汉南—川东北灯影组古地理演化：晚震旦世扬子西北缘拉张背景的沉积学证据

doi: 10.14027/j.issn.1000-0550.2018.146

1. 同济大学海洋地质国家重点实验室, 上海 200092;

2. 同济大学海洋与地球科学学院, 上海 200092;

3. 中国地质调查局油气资源调查中心, 北京 100083

基金项目: 国家重点研发计划项目（2016YFC0601005）；国家科技重大专项（2016ZX05034）；中央高校基本科研业务费专项资金（22120180128）

作者简介:
杨瑞青,女,1993年出生,硕士,沉积古环境,E-mail:rqyang@tongji.edu.cn

通讯作者: 杨风丽,女,教授,E-mail:yangfl@tongji.edu.cn

收稿日期: 2018-04-20
修回日期: 2018-06-28
刊出日期: 2019-02-10

中图分类号: P618.13;P534.31

关键词:

灯影组 /

古地理演化 /

拉张背景 /

汉南— /

川东北

摘要: 古地理面貌的呈现往往是构造演化与沉积充填共同作用的结果。通过对野外露头系统的观察与分析，在汉南—川东北地区进行了晚震旦世灯影期沉积相分析，识别出古隆起、局限台地、开阔台地和台缘斜坡4种类型的古地理单元；确定了汉南—川东北地区地势南高北低、各沉积单元呈南北向和北东向展布，且在平面上呈现“一隆两凹”的古地理面貌特征。在露头及盆地内钻井岩芯识别出的同沉积断层等特征，反映了沉积区处于拉张构造背景；且古地理研究中所确定的沉积坳陷区与隆起区的位置与重磁震等地球物理资料中识别出的裂陷/坳陷和古隆起位置相吻合，证实了四川盆地内绵竹—乐至—隆昌—长宁拉张槽/裂陷槽和万源—达州裂陷槽的存在，表明灯影期汉南—川东北地区处于拉张的构造背景，反映古地理背景发生了由稳定沉积到活动拉张的变化，并且经历了稳定沉积、拉张前奏和主体拉张三个阶段，进一步印证了沉积演化与构造背景之间的耦合关系。

English Abstract

Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian

1. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;

2. School of Ocean and Earth Science, Tongji University, Shanghai 200092, China;

3. Oil & Gas Survey, China Geology Survey, Beijing 100083, China

Received Date: 2018-04-20
Rev Recd Date: 2018-06-28
Publish Date: 2019-02-10

Keywords:

Abstract: The appearance of paleogeography is the result of the joint action of tectonic evolution and sedimentary filling. In this study, which was based on previous research and exploration results, systematic observations and analyses of the field outcrops in Hannan-Northeastern Sichuan Basin were conducted. The results reveal that there are four types of paleogeographic units in Dengying Formation in the Late Sinian: ancient Hannan paleo-uplift， restricted platforms open platforms and slopes. The terrain in the northeastern part of the Hannan-Northeastern Sichuan Basin is lowest in the south and highest in the north; the depositional elements are distributed in the north-south and northeasterly directions. The paleogeographic appearance in the study area was of “one uplift, two depressions”. It is suggested that the study area was in an extensional setting, which is reflected by the characteristics of co-sedimentary faults identified from outcrops and drillings. In addition, the location of the rift/depression identified in the geophysical data is consistent with the location of the ancient land on the paleogeographic map. This confirms the existence of the Mianzhu-Lezhi-Longchang-Changning pull/rift and Wanyuan-Dazhou rift in Sichuan Basin, and also indicates an extensional setting in the study area during the Dengying period. The paleogeographic background was transformed from one of stable deposition to active extension, and experienced stable deposition, prelude and main extension. Thus, this study further indicates the coupling relationship between sedimentary evolution and tectonic setting.

引用本文:

Citation:

YANG RuiQing, YANG FengLi, ZHOU XiaoFeng, ZHOU Zhi. Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian[J]. Acta Sedimentologica Sinica, 2019, 37(1): 189-199. doi: 10.14027/j.issn.1000-0550.2018.146

全文HTML

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

汉南—川东北灯影组古地理演化：晚震旦世扬子西北缘拉张背景的沉积学证据

doi: 10.14027/j.issn.1000-0550.2018.146

作者简介:
杨瑞青,女,1993年出生,硕士,沉积古环境,E-mail:rqyang@tongji.edu.cn

通讯作者:
杨风丽,女,教授,E-mail:yangfl@tongji.edu.cn

计量

Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian

计量

目录

汉南—川东北灯影组古地理演化：晚震旦世扬子西北缘拉张背景的沉积学证据

doi: 10.14027/j.issn.1000-0550.2018.146

1. 同济大学海洋地质国家重点实验室, 上海 200092;

2. 同济大学海洋与地球科学学院, 上海 200092;

3. 中国地质调查局油气资源调查中心, 北京 100083

作者简介:
杨瑞青,女,1993年出生,硕士,沉积古环境,E-mail:rqyang@tongji.edu.cn

通讯作者: 杨风丽,女,教授,E-mail:yangfl@tongji.edu.cn

English Abstract

Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian

1. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;

2. School of Ocean and Earth Science, Tongji University, Shanghai 200092, China;

3. Oil & Gas Survey, China Geology Survey, Beijing 100083, China

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

汉南—川东北灯影组古地理演化：晚震旦世扬子西北缘拉张背景的沉积学证据

doi: 10.14027/j.issn.1000-0550.2018.146

作者简介: 杨瑞青,女,1993年出生,硕士,沉积古环境,E-mail:rqyang@tongji.edu.cn

通讯作者: 杨风丽,女,教授,E-mail:yangfl@tongji.edu.cn

计量

出版历程

Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian

计量

出版历程

目录

汉南—川东北灯影组古地理演化：晚震旦世扬子西北缘拉张背景的沉积学证据

doi: 10.14027/j.issn.1000-0550.2018.146

1. 同济大学海洋地质国家重点实验室, 上海 200092; 2. 同济大学海洋与地球科学学院, 上海 200092; 3. 中国地质调查局油气资源调查中心, 北京 100083

作者简介: 杨瑞青,女,1993年出生,硕士,沉积古环境,E-mail:rqyang@tongji.edu.cn

通讯作者: 杨风丽,女,教授,E-mail:yangfl@tongji.edu.cn

English Abstract

Paleogeographic Evolution of the Dengying Formation in Hannan-Northeastern Sichuan Basin: Sedimentary evidence of the extensional tectonic setting for the northwest margin of the Yangtze Block in the Late Sinian

1. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China; 2. School of Ocean and Earth Science, Tongji University, Shanghai 200092, China; 3. Oil & Gas Survey, China Geology Survey, Beijing 100083, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
杨瑞青,女,1993年出生,硕士,沉积古环境,E-mail:rqyang@tongji.edu.cn

通讯作者:
杨风丽,女,教授,E-mail:yangfl@tongji.edu.cn

1. 同济大学海洋地质国家重点实验室, 上海 200092;

2. 同济大学海洋与地球科学学院, 上海 200092;

3. 中国地质调查局油气资源调查中心, 北京 100083

作者简介:
杨瑞青,女,1993年出生,硕士,沉积古环境,E-mail:rqyang@tongji.edu.cn

1. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;

2. School of Ocean and Earth Science, Tongji University, Shanghai 200092, China;

3. Oil & Gas Survey, China Geology Survey, Beijing 100083, China