胶莱盆地白垩系林寺山组砾岩沉积特征及盆地演化意义

章朋; 旷红伟; 柳永清; 彭楠; 许欢; 汪明伟; 安伟; 王能盛

doi:10.14027/j.cnki.cjxb.2016.01.002

ISSN 1000-0550 CN 62-1038/P

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胶莱盆地白垩系林寺山组砾岩沉积特征及盆地演化意义

章朋, 旷红伟, 柳永清, 彭楠, 许欢, 汪明伟, 安伟, 王能盛

文章导航 > 沉积学报 > 2016 > 34(1): 15-32

章朋, 旷红伟, 柳永清, 彭楠, 许欢, 汪明伟, 安伟, 王能盛. 胶莱盆地白垩系林寺山组砾岩沉积特征及盆地演化意义[J]. 沉积学报, 2016, 34(1): 15-32. doi: 10.14027/j.cnki.cjxb.2016.01.002

引用本文:

ZHANG Peng, KUANG HongWei, LIU YongQing, PENG Nan, XU Huan, WANG MingWei, AN Wei, WANG NengSheng. Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution[J]. Acta Sedimentologica Sinica, 2016, 34(1): 15-32. doi: 10.14027/j.cnki.cjxb.2016.01.002

Citation:

ZHANG Peng, KUANG HongWei, LIU YongQing, PENG Nan, XU Huan, WANG MingWei, AN Wei, WANG NengSheng. Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution[J]. Acta Sedimentologica Sinica, 2016, 34(1): 15-32. doi: 10.14027/j.cnki.cjxb.2016.01.002

引用本文:

Citation:

ZHANG Peng, KUANG HongWei, LIU YongQing, PENG Nan, XU Huan, WANG MingWei, AN Wei, WANG NengSheng. Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution[J]. Acta Sedimentologica Sinica, 2016, 34(1): 15-32. doi: 10.14027/j.cnki.cjxb.2016.01.002

胶莱盆地白垩系林寺山组砾岩沉积特征及盆地演化意义

doi: 10.14027/j.cnki.cjxb.2016.01.002

章朋^1,2,
旷红伟^1,,
柳永清¹,
彭楠¹,
许欢¹,
汪明伟³,
安伟¹,
王能盛¹

1.
中国地质科学院地质研究所北京 100037;
2.
中国地质大学(北京)地球科学与资源学院北京 100083;
3.
中国海洋石油总公司湛江分公司广东湛江 524057

基金项目: 国家自然基金项目(41272021, 41372109, 90914003);中国地质调查局项目(1212011085477, 12120114064301)

详细信息

作者简介:
章朋男 1988年出生硕士研究生沉积地质与盆地分析研究 E-mail:zhangp0927@126.com

通讯作者:
旷红伟女教授 E-mail:kuanghw@126.com

中图分类号: P534.53

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文章访问数: 576
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Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution

1.
Institute of Geoolgy, China Academy of Geological Sciences, Beijing 100037, China;
2.
School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China;
3.
Zhanjiang Branch of CNOOC Ltd., Zhanjiang, Guangdong 524057, China

Funds: China Natural Science Foundation, NO.41272021, 41372109, 90914003; China Geological Survey Project, NO.1212011085477, 12120114064301

摘要

摘要: 胶莱盆地下白垩统莱阳群底部林寺山组主要由砾岩组成。通过对盆地及周缘18个地点林寺山组砾岩系统的调查,从砾岩组分、砾径和长轴排列方向的统计分析出发,研究该砾岩沉积相类型、盆地物源区、古水流及林寺山组上覆地层中砂岩碎屑锆石U-Pb年龄谱特点,并进一步讨论了盆地演化的意义。研究表明,林寺山组底部砾岩以冲积扇相为主,但不同地点亚、微相类型又有差异。原型胶莱盆地由莱阳、海阳—即墨和诸城—五莲3个独立盆地组成,被6个隆起区所分隔。莱阳盆地的物源主要来自胶北隆起和苏鲁造山带北部;海阳—即墨盆地以苏鲁造山带北部隆起区、即墨—牟平隆起、胶南隆起为主物源区;诸城—五莲盆地以胶南隆起和马山—李党家低隆起为主要物源区。林寺山组砾岩的出现标志着苏鲁造山带大规模塌陷和胶莱盆地的形成。
- 胶莱盆地 /
- 白垩系 /
- 林寺山组 /
- 砾岩 /
- 沉积特征 /
- 盆地演化
Abstract: The Linsishan Formation, belonging to the bottom of the middl Early Cretaceous Laiyang Group in Jiaolai basin,Eastern Shandong, consists dominantly of a variety of conglomerates.Based on the petrological compositions, grain sizess and orientation of gravels within conglomerates at least 18 observation localities and a combination of detrital zircon dates of sandstones overlying the Linsishan Formation, this research reports a comprehensive results of the sedimentary facies, provenances,paleocurrents and implications of basin evolution.This study indicates that the Linsishan Formation mainly comprises of alluvial fan conglomerates with a variation of sedimentary microfacies in basin scale.The synsedimentary Jiaolai basin in term of paleogeography was constituted by three individual basins,i.e.,the Laiyang, Haiyang-Jimo and Zhucheng-Wulian basins, separated by the six paleo-uplifts.Provenance of the Laiyang basin are derived from Jiaobei uplift and the northern Sulu Orogenic Belt; source of the Haiyang-Jimu basin provided by northern Sulu Orogenic Belt, Jimo-Mouping uplift and Jiaonan uplift; Provenance of the Zhucheng-Wulian basin are derived from Jiaonan uplift and Mashan-Lijiadang low uplift. Finally,initiation of conglomerates of the Linsishan Formation in Eastern Shandong is a sign of formation of the synsedimentary Jiaolai basin and further,implies a large-scale collapse of the Sulu Orogenic Belt resulted from vast extensional crustal detachment and lithosphere thinning in East China because of destruction of North China Craton.
- Jiaolai Basin /
- Cretaceous /
- Linsishan Formation /
- Conglmerate /
- sedimentary characteristics /
- basin evolution

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[1]	李峰峰, 郭睿, 余义常, 宋世琦. 伊拉克M油田白垩系Mishrif组沉积特征及控储机理 . 沉积学报, 2020, 38(5): 1076-1087. doi: 10.14027/j.issn.1000-0550.2019.084
[2]	吕镔, 刘秀铭, 郭晖, 郑兴芬, 陈梓炫, 何梅菊, 赵国永. 福建白垩系沙县组地层磁学特征及其环境意义 . 沉积学报, 2019, 37(3): 519-531. doi: 10.14027/j.issn.1000-0550.2018.155
[3]	乔大伟, 王红亮. 基于粒度小波变换分析的四川盐源盆地沉积特征及其对盆地形成演化的指示意义 . 沉积学报, 2019, 37(4): 713-722. doi: 10.14027/j.issn.1000-0550.2018.165
[4]	魏震, 郭瑞清, 孙敏佳, 吕彪, 金建斌, 王海培, 王明阳. 新疆库鲁克塔格南华系砂岩碎屑组成对其物源及盆地演化的指示 . 沉积学报, 2017, 35(2): 264-278. doi: 10.14027/j.cnki.cjxb.2017.02.006
[5]	王颖, 王晓州, 廖计华, 朱石磊, 蔡露露. 巴西桑托斯盆地白垩系湖相藻叠层石礁特征及主控因素分析 . 沉积学报, 2016, 34(5): 819-829. doi: 10.14027/j.cnki.cjxb.2016.05.002
[6]	. 江西信江盆地白垩系沉积体系及其与丹霞地貌的关系 . 沉积学报, 2013, 31(6): 954-964.
[7]	张荣虎. 塔里木盆地白垩系巴什基奇克组陆相砂岩中碳酸盐岩碎屑特征及其地质意义 . 沉积学报, 2009, 27(3): 410-418.
[8]	景山. 辽西建昌盆地早白垩世义县组沉积环境分析及盆地演化初探 . 沉积学报, 2009, 27(4): 583-591.
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胶莱盆地白垩系林寺山组砾岩沉积特征及盆地演化意义

doi: 10.14027/j.cnki.cjxb.2016.01.002

1. 中国地质科学院地质研究所北京 100037;

2. 中国地质大学(北京)地球科学与资源学院北京 100083;

3. 中国海洋石油总公司湛江分公司广东湛江 524057

基金项目: 国家自然基金项目(41272021, 41372109, 90914003);中国地质调查局项目(1212011085477, 12120114064301)

作者简介:
章朋男 1988年出生硕士研究生沉积地质与盆地分析研究 E-mail:zhangp0927@126.com

通讯作者: 旷红伟女教授 E-mail:kuanghw@126.com

收稿日期: 2015-01-12
修回日期: 2015-04-10
刊出日期: 2016-02-10

中图分类号: P534.53

关键词:

白垩系 /

砾岩 /

摘要: 胶莱盆地下白垩统莱阳群底部林寺山组主要由砾岩组成。通过对盆地及周缘18个地点林寺山组砾岩系统的调查,从砾岩组分、砾径和长轴排列方向的统计分析出发,研究该砾岩沉积相类型、盆地物源区、古水流及林寺山组上覆地层中砂岩碎屑锆石U-Pb年龄谱特点,并进一步讨论了盆地演化的意义。研究表明,林寺山组底部砾岩以冲积扇相为主,但不同地点亚、微相类型又有差异。原型胶莱盆地由莱阳、海阳—即墨和诸城—五莲3个独立盆地组成,被6个隆起区所分隔。莱阳盆地的物源主要来自胶北隆起和苏鲁造山带北部;海阳—即墨盆地以苏鲁造山带北部隆起区、即墨—牟平隆起、胶南隆起为主物源区;诸城—五莲盆地以胶南隆起和马山—李党家低隆起为主要物源区。林寺山组砾岩的出现标志着苏鲁造山带大规模塌陷和胶莱盆地的形成。

English Abstract

Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution

1. Institute of Geoolgy, China Academy of Geological Sciences, Beijing 100037, China;

2. School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China;

3. Zhanjiang Branch of CNOOC Ltd., Zhanjiang, Guangdong 524057, China

Funds: China Natural Science Foundation, NO.41272021, 41372109, 90914003; China Geological Survey Project, NO.1212011085477, 12120114064301

Received Date: 2015-01-12
Rev Recd Date: 2015-04-10
Publish Date: 2016-02-10

Keywords:

Abstract: The Linsishan Formation, belonging to the bottom of the middl Early Cretaceous Laiyang Group in Jiaolai basin,Eastern Shandong, consists dominantly of a variety of conglomerates.Based on the petrological compositions, grain sizess and orientation of gravels within conglomerates at least 18 observation localities and a combination of detrital zircon dates of sandstones overlying the Linsishan Formation, this research reports a comprehensive results of the sedimentary facies, provenances,paleocurrents and implications of basin evolution.This study indicates that the Linsishan Formation mainly comprises of alluvial fan conglomerates with a variation of sedimentary microfacies in basin scale.The synsedimentary Jiaolai basin in term of paleogeography was constituted by three individual basins,i.e.,the Laiyang, Haiyang-Jimo and Zhucheng-Wulian basins, separated by the six paleo-uplifts.Provenance of the Laiyang basin are derived from Jiaobei uplift and the northern Sulu Orogenic Belt; source of the Haiyang-Jimu basin provided by northern Sulu Orogenic Belt, Jimo-Mouping uplift and Jiaonan uplift; Provenance of the Zhucheng-Wulian basin are derived from Jiaonan uplift and Mashan-Lijiadang low uplift. Finally,initiation of conglomerates of the Linsishan Formation in Eastern Shandong is a sign of formation of the synsedimentary Jiaolai basin and further,implies a large-scale collapse of the Sulu Orogenic Belt resulted from vast extensional crustal detachment and lithosphere thinning in East China because of destruction of North China Craton.

引用本文:

Citation:

ZHANG Peng, KUANG HongWei, LIU YongQing, PENG Nan, XU Huan, WANG MingWei, AN Wei, WANG NengSheng. Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution[J]. Acta Sedimentologica Sinica, 2016, 34(1): 15-32. doi: 10.14027/j.cnki.cjxb.2016.01.002

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胶莱盆地白垩系林寺山组砾岩沉积特征及盆地演化意义

doi: 10.14027/j.cnki.cjxb.2016.01.002

作者简介:
章朋男 1988年出生硕士研究生沉积地质与盆地分析研究 E-mail:zhangp0927@126.com

通讯作者:
旷红伟女教授 E-mail:kuanghw@126.com

计量

Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution

计量

目录

胶莱盆地白垩系林寺山组砾岩沉积特征及盆地演化意义

doi: 10.14027/j.cnki.cjxb.2016.01.002

1. 中国地质科学院地质研究所北京 100037;

2. 中国地质大学(北京)地球科学与资源学院北京 100083;

3. 中国海洋石油总公司湛江分公司广东湛江 524057

作者简介:
章朋男 1988年出生硕士研究生沉积地质与盆地分析研究 E-mail:zhangp0927@126.com

通讯作者: 旷红伟女教授 E-mail:kuanghw@126.com

English Abstract

Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution

1. Institute of Geoolgy, China Academy of Geological Sciences, Beijing 100037, China;

2. School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China;

3. Zhanjiang Branch of CNOOC Ltd., Zhanjiang, Guangdong 524057, China

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胶莱盆地白垩系林寺山组砾岩沉积特征及盆地演化意义

doi: 10.14027/j.cnki.cjxb.2016.01.002

作者简介: 章朋 男 1988年出生 硕士研究生 沉积地质与盆地分析研究 E-mail:zhangp0927@126.com

通讯作者: 旷红伟 女 教授 E-mail:kuanghw@126.com

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Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution

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出版历程

目录

胶莱盆地白垩系林寺山组砾岩沉积特征及盆地演化意义

doi: 10.14027/j.cnki.cjxb.2016.01.002

1. 中国地质科学院地质研究所 北京 100037; 2. 中国地质大学(北京)地球科学与资源学院 北京 100083; 3. 中国海洋石油总公司 湛江分公司 广东湛江 524057

作者简介: 章朋 男 1988年出生 硕士研究生 沉积地质与盆地分析研究 E-mail:zhangp0927@126.com

通讯作者: 旷红伟 女 教授 E-mail:kuanghw@126.com

English Abstract

Conglomerates on the Base Linsishan Formation of the Middle Early Cretaceous in Jiaolai Basin of Eastern Shandong, and Implications for Basin Evolution

1. Institute of Geoolgy, China Academy of Geological Sciences, Beijing 100037, China; 2. School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China; 3. Zhanjiang Branch of CNOOC Ltd., Zhanjiang, Guangdong 524057, China

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目录

友情链接

期刊在线

联系我们

作者简介:
章朋男 1988年出生硕士研究生沉积地质与盆地分析研究 E-mail:zhangp0927@126.com

通讯作者:
旷红伟女教授 E-mail:kuanghw@126.com

1. 中国地质科学院地质研究所北京 100037;

2. 中国地质大学(北京)地球科学与资源学院北京 100083;

3. 中国海洋石油总公司湛江分公司广东湛江 524057

作者简介:
章朋男 1988年出生硕士研究生沉积地质与盆地分析研究 E-mail:zhangp0927@126.com

通讯作者: 旷红伟女教授 E-mail:kuanghw@126.com

1. Institute of Geoolgy, China Academy of Geological Sciences, Beijing 100037, China;

2. School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China;

3. Zhanjiang Branch of CNOOC Ltd., Zhanjiang, Guangdong 524057, China