RF-RTM成像方法研究新疆西准噶尔地区线性台阵下方地壳结构

doi:10.13745/j.esf.sf.2023.7.16

地学前缘 ›› 2023, Vol. 30 ›› Issue (5): 358-368.DOI: 10.13745/j.esf.sf.2023.7.16

• “印度-欧亚大陆碰撞及其远程效应”专栏之九 • 上一篇下一篇

RF-RTM成像方法研究新疆西准噶尔地区线性台阵下方地壳结构

姜小欢¹^,²(), 黄荣³^,⁴^,^*(), 朱露培⁵, 卢占武⁶, 罗银河³^,⁴, 张荣堂¹, 徐浩¹

1.武汉轻工大学土木工程与建筑学院, 湖北武汉 430023
2.中国科学院精密测量科学与技术创新研究院大地测量与地球动力学国家重点实验室, 湖北武汉 430077
3.中国地质大学(武汉) 地球物理与空间信息学院, 湖北武汉 430074
4.中国地质大学(武汉) 地质过程与矿产资源国家重点实验室, 湖北武汉 430074
5.美国圣路易大学地球与大气科学系, 美国圣路易斯 63108
6.中国地质科学院地质研究所, 北京 100037

收稿日期:2023-07-08 修回日期:2023-07-12 出版日期:2023-09-25 发布日期:2023-10-20
通信作者: *黄荣(1984—),男,博士,讲师,硕士生导师,主要从事地震学研究。E-mail: huangrong@cug.edu.cn
作者简介:姜小欢(1989—),女,博士,讲师,主要从事远震接收函数成像研究。E-mail: xhjiang@whpu.edu.cn
基金资助:
大地测量与地球动力学国家重点实验室2022年基金项目(SKLGED2022-4-2);自然资源部深地科学与探测技术实验室开放课题(202206);地质过程与矿产资源国家重点实验室科技部专项(MSFGPMR2022-4);武汉轻工大学引进人才科研启动资金项目(2022RZ015);湖北巴东地质灾害国家野外科学观测研究站开放基金项目(BNORSG-202214)

Crustal structure beneath a seismic linear array in the Western Junggar, northwestern China by RF-RTM imaging

JIANG Xiaohuan¹^,²(), HUANG Rong³^,⁴^,^*(), ZHU Lupei⁵, LU Zhanwu⁶, LUO Yinhe³^,⁴, ZHANG Rongtang¹, XU Hao¹

1. School of Civil Engineering and Architecture, Wuhan Polytechnic University, Wuhan 430023, China
2. State Key Laboratory of Geodesy and Earth’s Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430077, China
3. School of Geophysics and Geomatics, China University of Geosciences (Wuhan), Wuhan 430074, China
4. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (Wuhan), Wuhan 430074, China
5. Department of Earth and Atmospheric Sciences, Saint Louis University, St. Louis, MO 63108, USA
6. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received:2023-07-08 Revised:2023-07-12 Online:2023-09-25 Published:2023-10-20

摘要/Abstract

摘要：

本文基于2017年7月8日至2017年8月2日在西准噶尔地区布设的一条100 km的线性台阵,从记录的三分量波形数据中计算出P波接收函数,采用接收函数逆时偏移(RF-RTM)方法获得了台阵下方地壳结构成像结果。结果表明测线下方扎伊尔山和准噶尔盆地结构差异较大:扎伊尔山下Moho界面平均深度为42 km,横向连续且起伏较小;准噶尔盆地下方地壳结构成像结果较复杂,盆地基底延伸至3 km深,盆地下方Moho界面沿着测线走向(北西-南东)深度逐渐加深,在测线最南东端达到50 km;另外,在准噶尔盆地下方35 km深处可看出一明显的速度异常界面,推测可能是由古生代大洋岩石圈残片造成。上述研究成果有助于加深对西准噶尔地区的大陆岩石圈形成和演化过程的理解。

关键词: 接收函数, 逆时偏移, 密集台阵, 西准噶尔, 地壳结构

Abstract:

Data used in this paper were obtained from a 100-km long linear seismic array, Western Junggar area, by continuous recording from July 08 to August 02, 2017. We first calculate teleseismic P-wave receiver functions and then apply reverse time migration of teleseismic receiver function (RF-RTM) method to image the Moho variations beneath the linear array. The results show obvious differences in the crustal structure beneath the Zaire Mount and the Junggar Basin. The Moho discontinuity beneath the Zaire Mount flattens to a depth of ~42 km; while the crustal structure beneath the Junggar Basin appears quite complex. The basement of the Junggar Basin extends to a depth of 3 km, and the Moho discontinuity gradually deepens along the trend of the linear array from northwest (NW) to southeast (SE), finally reaching to a depth of 50 km. We also observe especially an obvious velocity anomaly interface at a depth of about 35 km, and infer that it might be generated by a Paleozoic fossil oceanic subducting slab. Our study may shed light on the formation and evolution of continental lithosphere in the Western Junggar area.

Key words: receiver function, reverse time migration, seismic dense array, Western Junggar, crustal structure

中图分类号:

P315.2

姜小欢, 黄荣, 朱露培, 卢占武, 罗银河, 张荣堂, 徐浩. RF-RTM成像方法研究新疆西准噶尔地区线性台阵下方地壳结构[J]. 地学前缘, 2023, 30(5): 358-368.

JIANG Xiaohuan, HUANG Rong, ZHU Lupei, LU Zhanwu, LUO Yinhe, ZHANG Rongtang, XU Hao. Crustal structure beneath a seismic linear array in the Western Junggar, northwestern China by RF-RTM imaging[J]. Earth Science Frontiers, 2023, 30(5): 358-368.

图/表 11

图1 (a) 西准噶尔研究区地质背景图和(b) 线性台阵分布图 Kazakhstan Plate—哈萨克斯坦板块;Tienshan—天山造山带;Zaire Mt.—扎伊尔山;Junggar—准噶尔盆地;Altay—阿尔泰山脉。Hatu fault、Darbut fault和Karamay-Urho fault分别表示哈图断裂、达尔布特断裂和克拉玛依—乌尔禾断裂;Karamay—克拉玛依,Toli—托里,Kuytun—奎屯;实心三角代表地震台站(其中黑色和蓝色为有数据的短周期台站,灰色为无数据的台站)。

Fig.1 (a) Tectonic settings of the western Junggar, and (b) layout of a seismic linear array (AA')

图2 远震事件分布图黑色三角—台站位置;蓝色实心圆—31个远震事件;红色实心圆—5个后续用于成像计算的远震事件。

Fig.2 Azimuth-distance distribution of teleseismic events (circles)

图3 P波初至(图中零时刻)对齐后的2个远震事件(“20170720223111”和“20170723153540”)的沿测线AA'(图1b)上所有台站记录的垂向(Z)和径向(R)分量波形数据示例

Fig.3 Teleseismic waveforms of vertical (Z) and radial (R) components for 2 earthquakes (“20170720223111” and “20170723153540”) aligned with the first P arrival with stations along survey line AA' (see Fig.1b for AA' location)

图4 图3对应的两个远震事件接收函数插值前(a,c)和插值后(b,d)结果图图中椭圆形黑色实线圈定区域中包含低速盆地产生的多次波。

Fig.4 (a, c) RFs and (b, d) interpolated RFs of the two teleseismic events in Fig.3

图5 NA反演用到的2个台站的接收函数波形。(a,b)台站XJ_S11和XJ_WJS41原始接收函数波形;(c,d)NA反演得到的台站XJ_S11和XJ_WJS4接接收函数波形拟合结果图(c,d)中红色波形是由NA反演速度模型计算的理论接收函数波形。

Fig.5 Receiver functions recorded for XJ_S11 and XJ_WJS41 used in NA inversion. (a, b) RFs. (c, d) Receive function waveform fitting results.

表1 台站XJ_S11和XJ_WJS41的接收函数用邻域反演得到的结果

Table 1 Receiver function inversion results for XJ_S11 and XJ_WJS41 using neighborhood algorithm (NA)

Station	Thickness/ km	v_S1/ (km·s^-1)	v_S2/ (km·s^-1)	κ/ (v_P·v_S)
XJ_S11	1.3	0.2	1.8	2.33
XJ_WJS41	3.0	0.5	2.1	2.44

图6 二维S波背景速度模型

Fig.6 A 2-D S-wave velocity background model

图7 图3中两个远震事件利用RF-RTM成像结果

Fig.7 RF-RTM imaging results for the two teleseismic events in Fig.3

图8 成像结果图。(a)RF-RTM叠加成像结果和(b)CCP叠加成像结果图中黑色×线代表Moho界面位置,黑色虚线代表准噶尔盆地基底界面位置。

Fig.8 The imaging results. (a) RF-RTM and (b) CCP stacking results.

图9 RF-RTM方法和CCP方法成像结果在Moho界面处的离散图红色实心圆—RF-RTM得到的Moho界面;蓝色实心圆—CCP得到的Moho界面。

Fig.9 Moho location from RF-RTM and CCP stacking imaging

图10 影响因素分析图。(a)利用1 Hz高斯滤波的接收函数利用RF-RTM方法成像的结果;(b) 利用PPPS震相的RF-RTM成像结果黑色×线为利用PS震相的RF-RTM的Moho位置。

Fig.10 Analysis diagram of influencing factors. (a) RF-RTM stacking images with low-pass filtered RFs using a 1 Hz Gaussian filter. (b) RF-RTM stacking images using PpPs phases. Black cross represents Moho discontinuity location.

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RF-RTM成像方法研究新疆西准噶尔地区线性台阵下方地壳结构

Crustal structure beneath a seismic linear array in the Western Junggar, northwestern China by RF-RTM imaging

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