印度洋沉积物中火山灰应用研究进展

doi:10.11978/2016114

热带海洋学报 ›› 2017, Vol. 36 ›› Issue (6): 12-18.doi: 10.11978/2016114CSTR: 32234.14.2016114

所属专题：海上丝绸之路专题

印度洋沉积物中火山灰应用研究进展

杜恕环(), 向荣, 陈木宏, 刘建国, 张兰兰, 罗传秀, 苏翔, 张强

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), 广东广州 510301

收稿日期:2016-11-08 修回日期:2016-12-13 出版日期:2017-11-30 发布日期:2018-01-18
作者简介:
作者简介：杜恕环(1982#cod#x02014;), 女, 广东省汕头市人, 副研究员, 博士, 主要从事海洋风成与微体古生物研究。Email: shuhuandu@scsio.ac.cn
基金资助:
中国科学院战略性先导科技专项(A类) (XDA11030104);广东省公益研究与能力建设专项(2015A020216015)

Progress of applied research of tephra in the Indian Ocean sediments

Shuhuan DU(), Rong XIANG, Muhong CHEN, Jianguo LIU, Lanlan ZHANG, Chuanxiu LUO, Xiang SU, Qiang ZHANG

CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Guangzhou 510301, China

Received:2016-11-08 Revised:2016-12-13 Online:2017-11-30 Published:2018-01-18
About author:
Author:QIU Chunhua.E-mail: qiuchh3@mail. sysu.edu.cn
Supported by:
Foundation item: Strategic Priority Research Program of the Chinese Academy of Science (XDA11030104);Guangdong Province Science and Technology Project (2015A020216015)

摘要/Abstract

摘要：

印度洋是我国#cod#x0201c;21世纪海上丝绸之路#cod#x0201d;的重要通道, 更是亚洲季风两个子系统(印度季风和东亚季风)的主要策源地, 在全球变化中扮演着重要角色。海洋沉积物中的火山灰作为一种地层研究工具, 不仅记录了源区、搬运介质和搬运机制的相关信息, 还能有效#cod#x0201c;等时#cod#x0201d;定年, 其含量和成分对研究沉积作用和构造活动具有重要意义。文章对印度洋沉积物中的火山灰应用研究进展进行了综述, 包括: 1)火山灰定义及其在印度洋沉积物中#cod#x0201c;等时面#cod#x0201d;的应用; 2)火山灰(火山玻璃)的测试分析方法及其在追踪物质来源、火山构造与岩浆作用、印度季风演化等方面的运用。今后我国在印度洋开展火山灰研究主要应该聚焦在两方面: 1)表层沉积物中的火山灰及其应用; 2)火山灰与高分辨率古环境记录。可以利用火山灰定年的#cod#x0201c;等时#cod#x0201d;性探讨气候变化的区域差异及驱动因素。

关键词: 印度洋, 深海沉积物, 火山灰, 分析, 应用

Abstract:

The Indian Ocean is the important channel of #cod#x0201c;Maritime Silk Road#cod#x0201d; in the 21st century, and is the main origins of the two sub-systems (the Indian monsoon and the East Asian monsoon) of the Asian monsoon, which plays an important role in the global change. Tephra in marine sediments as a stratigraphic tool not only records the information of source area, transporting medium and mechanism, but also can effectively make isochronal dating. The content and composition of tephra has great significance to study sedimentary and tectonic activity. In this paper, we summarize progress of applied research of tephra in the Indian Ocean sediments, including: 1) the definition of tephra and its isochronal dating in the Indian Ocean sediments; and 2) the analysis method of tephra (volcanic glass) and the effect on trace material sources, volcanic structure and magmatism, the Indian monsoon evolution, etc. Our future work on tephra in the Indian Ocean mainly includes in two tasks: 1) tephra and its application in surface sediments; and 2) tephra and high-resolution paleoenvironment records. Finally, regional climate change and driving factors are discussed by means of tephra isochronal dating.

Key words: Indian Ocean, deep-sea sediments, tephra, analysis, apply

中图分类号:

P736.2

杜恕环, 向荣, 陈木宏, 刘建国, 张兰兰, 罗传秀, 苏翔, 张强. 印度洋沉积物中火山灰应用研究进展[J]. 热带海洋学报, 2017, 36(6): 12-18.

Shuhuan DU, Rong XIANG, Muhong CHEN, Jianguo LIU, Lanlan ZHANG, Chuanxiu LUO, Xiang SU, Qiang ZHANG. Progress of applied research of tephra in the Indian Ocean sediments[J]. Journal of Tropical Oceanography, 2017, 36(6): 12-18.

图/表 4

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图2

表1

图3

参考文献 39

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火山灰层	年代	方法	地点	数据来源
A层 (YTT)	(73.5#cod#x000b1;5.0)ka	K-Ar	苏门答腊	Ninkovich et al, 1978
	(73.0#cod#x000b1;4.0)ka	⁴⁰Ar/³⁹Ar	苏门答腊	Chesner et al, 1991
	(68.0#cod#x000b1;7.0)ka	裂变径迹	马来西亚	Chesner et al, 1991
	(73.0#cod#x000b1;4.0)ka	⁴⁰Ar/³⁹Ar	印度洋	Dehn et al, 1991
	(73.9#cod#x000b1;2.6)ka	氧同位素年龄	苏门答腊	Rampino et al, 1992
	(79.0#cod#x000b1;8.0)ka	裂变径迹	印度及马来西亚	Westgate et al,1998
	(76.0~80.0)ka	氧同位素年龄	印度洋	Qiu et al, 2014
	(70.0~75.0)ka	²³⁰Th_excess	印度洋	Mascarenhas-Pereira et al, 2016
C层(MTT)	(501.0#cod#x000b1;5.0)ka	⁴⁰Ar/³⁹Ar	印度洋	Chesner, 1988
D层	(800#cod#x000b1;20)ka	⁴⁰Ar/³⁹Ar	印度洋	Hall et al, 1995
E层(OTT)	(840#cod#x000b1;300)ka	⁴⁰Ar/³⁹Ar	印度洋	Chesner et al, 1991
I层	(4.43#cod#x000b1;0.03)Ma	⁴⁰Ar/³⁹Ar	印度洋	Hall et al,1995

印度洋沉积物中火山灰应用研究进展

Progress of applied research of tephra in the Indian Ocean sediments

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