东海到南海晚中生代岩浆弧及陆缘汇聚体制综述

doi:10.11867/j.issn.1001-8166.2019.09.0950

地球科学进展 ›› 2019, Vol. 34 ›› Issue (9): 950 -961. doi: 10.11867/j.issn.1001-8166.2019.09.0950

张成晨 ¹(

),许长海 ¹(

),何敏 ²,高顺莉 ³

1. 同济大学海洋与地球科学学院海洋地质国家重点实验室，上海 200092
2. 中海石油(中国)有限公司深圳分公司，广东深圳 518054
3. 中海石油(中国)有限公司上海分公司，上海 200335

收稿日期:2019-02-20 修回日期:2019-07-19 出版日期:2019-09-10
通讯作者: 许长海 E-mail:1632964@tongji.edu.cn;xchxch@tongji.edu.cn
基金资助:
国家自然科学基金项目“东海陆架到南海北部晚中生代东亚汇聚边缘演变的岩浆弧记录”(41876045);国家科技重大专项课题“海相盆地构造热体制与资评选区评价平台开发研究”(2017ZX05005001-005)

Late Mesozoic Convergent Continental Margin with Magmatic Arc from East to South China Seas: A Review

Chengchen Zhang ¹( ),Changhai Xu ¹( ),Min He ²,Shunli Gao ³

1. State Key Laboratory of Marine Geology, School of Ocean and Earth Science, Tongji University, Shanghai 200092, China
2. CNOOC China Limited-Shenzhen, Shenzhen 518054, China
3. CNOOC China Limited-Shanghai, Shanghai 200335, China

Received:2019-02-20 Revised:2019-07-19 Online:2019-09-10 Published:2019-11-15
Contact: Changhai Xu E-mail:1632964@tongji.edu.cn;xchxch@tongji.edu.cn
About author:Zhang Chengchen （1988-）， female， Changji City， Xinjiang Uygur Autonomous Region， Master student. Research areas include regional geological structure. E-mail： 1632964@tongji.edu.cn
Supported by:
the the National Natural Science Foundation of China “Late-Mesozoic arc-subduction-related igneous rocks from SW East China Sea to N South China Sea: Key constraints on East Asia convergent margin”(41876045);The National Science and Technology Major Project “Tectonothermal evolution of marine basin and platform development of resource evaluation”(2017ZX05005001-005)

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晚中生代是古太平洋板块俯冲汇聚东亚大陆的重要时期，这一构造期促发了华南强烈的岩浆活动和陆内变形，相关俯冲杂岩残留在日本西南、中国台湾到婆罗洲一线。华南大陆特别是岩浆岩研究已取得了丰富的成果认识，但缺乏与典型岩浆弧相关的中性岩浆岩发现。位于海陆结合部的东海到南海区域，将是开展晚中生代岩浆弧和弧前盆地等研究的优选地区，目前已陆续发现了相关岩浆岩和沉积记录。开展东海到南海这一区域性的岩浆弧和弧前盆地等研究，同时结合东部俯冲杂岩和华南大陆岩浆岩等成果资料，将有助于形成和完善晚中生代古太平洋俯冲体制和东亚活动大陆边缘的演变模式，也是深化认识我国海域中生界沉积盆地性质及其油气潜力的重要环节。

关键词: 岩浆弧, 汇聚大陆边缘, 晚中生代, 东海到南海

The Late Mesozoic is an important tectonic period for subduction of Paleo-Pacific slab beneath East Asia continent. It intensely led to Jurassic to Cretaceous magmatism associated with intracontinental deformation in South China. Subduction-related accretionary complexes remained regionally from SW Japan, E Taiwan to the W Philippines and Borneo. Studies on geology in South China, especially in magmatism, have been performed with good data, results, and sufficient understandings; whereas those arc-related intermediate igneous rocks have been less found. The areas from East to South China Seas which are located at the junction between sea and land will be the preferred areas for the study of the Late Mesozoic magmatic arc and the forearc basin. The relevant arc-related magmatic rocks and forearc sedimentary records have been increasingly discovered. Studies of magmatic arc and forearc basin combined with subdction complex will be essential to the reconstruction of the convergent continental margin in South China. Analyses of magmatic arc identification from South to East China Seas, arc to forearc relationship, and assembly between arc and regional faults will become necessary to improve the knowledge of the model of East Asia convergent continental margin, and as well help to develop the understanding of Late Mesozoic forearc basin and resource potentials in the southeast sea areas.

Key words: Magamatic arc, Active continental margin, Late Mesozoic, South to East China Seas.

中图分类号:

P736.11

图1 南海北部到东海陆架钻遇的前新生代基底岩石分布图

Fig.1 Pre-Cenozoic various lithologies drilled from South to East China Seas

图2 南海及华南东部晚中生代花岗岩类 (Y+Nb)-Rb构造环境对比（数据引自文献[35，43，44~52]）

Fig.2 (Y+Nb)-Rb discrimination of Late Mesozoic granitoids from eastern South China Block to northern South China Sea
（ Data from references[35，43，44~52]）

图3 东海陆架晚中生代花岗岩类锆石元素构造环境分析

Fig.3 Tectonic environment indicated by zircon trace elements of Late Mesozoic granitoids from East China Sea

图4 华南侏罗纪早期汇聚大陆边缘构造模式(据参考文献[ 43 ]修改)

Fig. 4 A cartoon showing an early Jurassic subduction-related architecture of East Asian continental margin (modified after reference [ 43 ])

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