|本期目录/Table of Contents|

[1]张天继,金明培,刘自凤,等.滇西北地区地壳厚度与泊松比分布及其意义*[J].地震研究,2020,43(01):10-18.
 ZHANG Tianji,JIN Mingpei,LIU Zifeng,et al.Distribution and Significance of Crustal Thickness and Poisson's Ratio in Northwestern Yunnan[J].Journal of Seismological Research,2020,43(01):10-18.
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滇西北地区地壳厚度与泊松比分布及其意义*(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
43
期数:
2020年01期
页码:
10-18
栏目:
出版日期:
2020-01-30

文章信息/Info

Title:
Distribution and Significance of Crustal Thickness and Poisson's Ratio in Northwestern Yunnan
作者:
张天继金明培刘自凤程宇豪
(云南省地震局,云南 昆明 650224)
Author(s):
ZHANG TianjiJIN MingpeiLIU ZifengCHENG Yuhao
(Yunnan Earthquake Agency,Kunming 650224,Yunnan,China)
关键词:
滇西北地区 地震亚失稳 接收函数 地壳厚度 泊松比
Keywords:
northwestern Yunnan seismic meta-instability receiver function crustal thickness Poisson's ratio
分类号:
P315.2
DOI:
-
摘要:
利用滇西北地震亚失稳观测实验区43个密集观测台站记录的2018年4月5日—12月30日远震三分量波形数据,计算并分析滇西北地区的地壳厚度和泊松比变化情况。结果表明:①研究区的地壳厚度总体呈现北深南浅的变化特征,且形成以云龙、蝴蝶泉—阳和、岩曲—羊窝棚—哨横为中心的3个莫霍面隆起区,在26°N附近形成一个向南的舌状突出,呈现两隆两凹状的莫霍面结构; ②研究区泊松比为0.209~0.328,整体被2条对角线分隔呈四象限分布,北、南两区是高泊松比(σ>0.28)地区,推测地壳物质富含铁镁质成分,西、东区为低泊松比(σ<0.26)区域,地壳物质可能富集长英质成分; ③云龙、蝴蝶泉—阳和以及南涧—红土坡地区的高泊松比(σ>0.3)可能是上地幔物质底侵致使下地壳物质部分熔融引起; 维西—乔后—巍山断裂北段的通甸—建基村,其与龙蟠—乔后断裂交汇的丰乐—禾头,以及维西—乔后—巍山断裂中段的脉地—紫阳村—瓦窑—太邑—岔河,是泊松比高梯度带,具备发生中强以上地震的孕震环境。
Abstract:
Using teleseismic waveform data recorded by 43 stations in meta-instability observation experiment area of northwestern Yunnan from April 5 to December 30,2018,we calculated and analyzed the changes of crustal thickness and Poisson's ratio in northwestern Yunnan.The results showed:the crustal thicknesses in this area are generally the variation characteristics of deeper in north and shallower in south; the three areas of Yunlong,Hudiequan-Yanghe,and Yanqu-Yangwopeng-Shaoheng are mantle uplifting sites,and the Moho surface is characterized as a tongue shape protruding southward and basically featuring two uplifts and two depressions near 26°N.The Poisson's ratio ranges from 0.209 to 0.328 in the study area,which is divided into four quadrants by two diagonal lines,the north and south regions are high Poisson's ratios(σ>0.28),the crust maybe enriched with iron and magnesium; the west and east regions are low Poisson's ratios(σ<0.26),the crust maybe rich in felsic.Very high Poisson's ratios(σ>0.3)are found in Yunlong,Hudiequan-Yanghe,and Nanjian-Hongtupo areas maybe the partial melting of lower crustal material caused by the bottom intrusion of upper mantle material.The Tongdian-Jianji,Fengle-Hetou,and Maidi-Ziyangcun-Wayao-Taiyi-Chahe areas are high gradient zones of Poisson's ratio and are seismogenic environments with moderate to strong earthquakes.

参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2019-04-01
基金项目:国家重点研发计划子专题(2018YFC150330303)资助.
通讯作者:金明培(1969-),正研级高级工程师,主要从事地震监测预报、接收函数、震源模型等研究.E-mail:jmp69@263.net

更新日期/Last Update: 2020-01-30