南海的“山根拆沉成因观”——南海成因新议

刘海龄; 周洋; 王印; 朱荣伟; 黎雨晗

doi:10.16562/j.cnki.0256-1492.2017.06.002

南海的“山根拆沉成因观”——南海成因新议

1.
中国科学院边缘海与大洋地质重点实验室，中国科学院南海海洋研究所，广州 510301

2.
中国科学院广州地球化学研究所，广州 510640

3.
中国科学院大学，北京 100049

基金项目:
国家自然科学基金项目(41776072, 41476039, 91328205, 41576068)

详细信息

作者简介: 刘海龄(1958—)，男，研究员，博导，主要从事南中国海和东南亚区域大地构造研究，Email: liuh82@126.com

中图分类号: P736.1

文凤英编辑

收稿日期: 2017-11-30

修回日期: 2017-12-15

刊出日期: 2017-12-28

"MOUNTAIN ROOT DELAMINATION":A NEW MECHANISM FOR ORIGIN OF THE SOUTH CHINA SEA

1.
CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

2.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

3.
University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 30 November 2017

Revised Date: 15 December 2017

Publish Date: 28 December 2017

摘要

摘要:
南海成因问题至今仍众说纷纭。作者以寻求南海形成演化的内因为着眼点，在大量地震剖面地质解释的基础上，运用构造解析法对南海南北陆缘前新生代基底地质构造变形形迹进行了系统的构造恢复和组合分析，发现了残存于南海南北陆缘中生代基底中的断层褶皱具有碰撞造山带特有的背冲断褶构造特征，指出该古造山带的中轴位置大致沿现今双峰笔架海山连线分布，并称之为古双峰笔架碰撞造山带。结合南海地区新生代岩浆岩地球化学特征分析和南北陆缘新生代伸展构造特征分析，提出该造山带在新生代发生了山根拆沉的解体过程，并明确提出了该“山根拆沉”机制是诱发南海形成的根本原因。
- 南海成因 /
- 中生界 /
- 古双峰-笔架碰撞造山带 /
- 山根拆沉 /
- 造山带解体
Abstract:
The origin of the South China Sea (SCS) still remains a dispute. With emphasis on internal mechanisms for the formation and evolution of the SCS, based on geological interpretation of a large number of seismic profiles, and using tectonic analysis as the method, the authors carried out systematic tectonic restoration of the structural deformation features of the Pre Cenozoic basements on the northern and southern continental margins of SCS. Back thrust fold structures are found remained in the basements, which are endemic to collision orogenic belt. The axis of the paleo orogenic belt is distributed roughly along the modern Shuangfeng Bijia seamount line. We name it "Paleo Shuangfeng Bijia collision orogenic belt" hereafter in this paper. Together with the analyses of Cenozoic magmatite geochemical characteristics of SCS region and the Cenozoic extensional tectonic characteristics of northern and southern continental margins, the authors proposed that the orogenic belt underwent a mountain root delamination process in Cenozoic. And the mechanism of "mountain root delamination" is the fundamental origin of the SCS.
- origin of the South China Sea /
- Mesozoic /
- Papeo Shuangfeng Bijia collision orogenic belt /
- mountain root delamination /
- disintegration of orogenic belt

HTML全文

图 1 南海成因“山根拆沉观”示意图

Figure 1.

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图 2 用于本文分析的南海北缘地震测线分布图

Figure 2.

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图 3 用于本文分析的南海南缘地震测线分布

Figure 3.

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图 4 南海北缘79pr1884地震剖面及其地质解释

Figure 4.

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图 5 南海北缘过LF35-1-1井的a-b地震剖面及其地质解释

Figure 5.

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图 6 07ns-6测线地震剖面及其地质解释

Figure 6.

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图 7 古双峰-笔架碰撞造山带山根形成-拆沉过程与南海的打开

Figure 7.

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南海的“山根拆沉成因观”——南海成因新议

1. 中国科学院边缘海与大洋地质重点实验室，中国科学院南海海洋研究所，广州 510301 2. 中国科学院广州地球化学研究所，广州 510640 3. 中国科学院大学，北京 100049

作者简介: 刘海龄(1958—)，男，研究员，博导，主要从事南中国海和东南亚区域大地构造研究，Email: liuh82@126.com

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"MOUNTAIN ROOT DELAMINATION":A NEW MECHANISM FOR ORIGIN OF THE SOUTH CHINA SEA

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1.
中国科学院边缘海与大洋地质重点实验室，中国科学院南海海洋研究所，广州 510301

2.
中国科学院广州地球化学研究所，广州 510640

3.
中国科学院大学，北京 100049