南海东部边缘火山活动所反映的板片窗构造

唐琴琴; 詹文欢; 李健; 冯英辞; 姚衍桃; 孙杰; 黎雨晗

doi:10.16562/j.cnki.0256-1492.2017.02.012

南海东部边缘火山活动所反映的板片窗构造

唐琴琴^1,2,,
詹文欢^1,2, ,,
李健^1,2,
冯英辞^1,2,
姚衍桃¹,
孙杰¹,
黎雨晗^1,2

1.
中国科学院边缘海与大洋地质重点实验室，南海海洋研究所，广州 510301
2.
中国科学院大学，北京 100049

基金项目:

国家自然科学基金项目 41376063

详细信息

作者简介:
唐琴琴(1993—)，女，硕士研究生，研究方向为海洋新构造，E-mail：tangqinqin15@mails.ucas.ac.cn

通讯作者:
詹文欢，男，研究员，研究方向为海洋新构造与地质灾害，E-mail: whzhan@scsio.ac.cn

中图分类号: P736.1
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出版历程
- 收稿日期: 2016-08-09
- 修回日期: 2016-11-28
- 刊出日期: 2017-04-27

VOLCANIC EVIDENCE FOR SLAB WINDOW INDUCED BY FOSSIL RIDGE SUBDUCTION AT EAST EDGE OF SOUTH CHINA SEA

TANG Qinqin^1,2,,
ZHAN Wenhuan^1,2, ,,
LI Jian^1,2,
FENG Yingci^1,2,
YAO Yantao¹,
SUN Jie¹,
LI Yuhan^1,2

1.
CAS Key Laboratory of Ocean and Marginal Sea Geology, Chinese Academy of Sciences, South China Sea Institute of Oceanology, Guangzhou 510301, China
2.
University of Chinese Academy of Sciences, Beijing 100049, China

摘要

摘要: 从全球板块构造环境来看，与洋脊俯冲有关的板片窗占据绝大部分比例，俯冲洋脊板片正处于新生过程，热量大，具有正浮力(< 10 Ma)，在俯冲过程中容易撕裂形成板片窗。南海古扩张脊沿马尼拉海沟向菲律宾海板块俯冲，南海东部边缘火山活动在吕宋岛上表现为东西双火山链，上新世期间，西火山链停止活动，而东火山链内的岩浆活动几乎完全是在第四纪。东西双火山链在20°N向南开始分支，东火山链在17.8°N停止，西火山链往南一直延伸到民都洛岛，东西火山链之间的火山空隙即反映了南海古扩张脊沿马尼拉海沟向菲律宾海板块俯冲形成的板片窗构造。同时，根据吕宋岛晚中新世以来埃达克岩的空间分布空隙和时间空隙特征，反映在吕宋岛17°~17.5°N存在板片窗构造。
- 古洋脊俯冲 /
- 海沟 /
- 火山活动 /
- 板片窗 /
- 南海东部
Abstract: Slab windows are generated from the subducting plate, but not necessarily on the subducting ridge. However, slab windows related to the ocean ridge are taken great proportions in the world. The young subduction ridge, which is usually less than 10 Ma, is much hotter and has positive buoyancy, so there is wide gap between two sides of subducting ridges. The fossil ridge of South China Sea has subducted under the Philippine Sea plate along the Manila Trench. There are double chains of volcanoes in the eastern edge of the South China Sea(Luzon), where the west volcanic chain has stopped eruption since Pliocene, but the east one has a lot of volcanic activities up to now. The two volcanic chains are separated at 20°N, and the east volcanic chain has extinguished at 17.8°N, while the west one has extended to the island of Mindoro. So the volcanic gap between volcanic chains suggest the slab window below Luzon, which was formed by the extinct ridge subduction. Moreover, the characteristics of time and space about adakites after late Holocene also implied that the slab window existed between 17°N and 17.5°N in the Luzon Island.
- fossil ridge subduction /
- trench /
- volcanos /
- slab window /
- eastern South China Sea

HTML全文

图 1 板片窗类型图(修改自文献[4])

Figure 1. Diagram showing Slab Windows(modified from reference[4])

下载: 全尺寸图片幻灯片

图 2 南海东部边缘构造简图

Figure 2. Tectonic map of the region surrounding the eastern South China Sea

下载: 全尺寸图片幻灯片

图 3 南海板片地震层析成像图

红色表示低速，蓝色表示高速，MT表示马尼拉海沟，ELT表示东吕宋海沟，PT表示菲律宾大断层，SCSc表示南海板片，PSP表示菲律宾海板块^[24]

Figure 3. Tomographic images of South China Sea slab^[23]

下载: 全尺寸图片幻灯片

图 4 吕宋岛的双火山链图(修改自文献[33])

Figure 4. Volcanic chains along the Luzon Arc(modified from reference[33])

The tooth-like lines represent subduction zones, the solid lines faults, and the double-dashed line the inferred fossil ridge of SCS

下载: 全尺寸图片幻灯片

图 5 吕宋岛晚中新世以来的埃达克岩时空分布(修改自文献[40])

Figure 5. Map showing the distribution of adakites in Luzon Arc (modified from reference[40])

下载: 全尺寸图片幻灯片

图 6 南海东部板片窗模式图(修改自文献[13])

Figure 6. Proposed schematic morphology of the slab window in eastern South China Sea (modified from Bautista et al. 2001)

下载: 全尺寸图片幻灯片

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