藏北羌塘盆地中部地壳低速层分布与动力学意义

严江勇; 郑洪伟; 贺日政; 李娱兰; 李瑶; 牛潇

doi:10.3799/dqkx.2018.355

藏北羌塘盆地中部地壳低速层分布与动力学意义

doi: 10.3799/dqkx.2018.355

严江勇^1,2, ,,
郑洪伟²,
贺日政^1,2, ,,
李娱兰^1,2,3,
李瑶^1,4,
牛潇¹

1.
中国地质科学院深部探测中心, 国土资源部深部探测与地球动力学重点实验室, 北京 100037
2.
中国地质科学院地质研究所, 北京 100037
3.
中国地震局地球物理研究所地震观测与地球物理成像重点研究室, 北京 100081
4.
中国地震局地球物理研究所, 北京 100081

基金项目:

国家重点研发计划 2016YFC0600301

科技部深地资源勘查开采 2016YCF0600301

科技部深地资源勘查开采 2018YCF0604102

国家自然基金 41574086

国家自然基金 41761134094

中国地质调查项目 DD20160022-05

详细信息

作者简介:
严江勇(1992-), 硕士研究生, 主要从事地震学研究

通讯作者:
贺日政

中图分类号: P611
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- 文章访问数: 4868
- HTML全文浏览量: 1983
- PDF下载量: 48
- 被引次数: 0
出版历程
- 收稿日期: 2018-08-27
- 刊出日期: 2019-06-15

Low Velocity Layer Investigation in Central Qiangtang in North Tibet and Its Dynamic Implications

Yan Jiangyong^{1,2
,
,},
Zheng Hongwei²,
He Rizheng^{1,2
, ,},
Li Yulan^1,2,3,
Li Yao^1,4,
Niu Xiao¹

1.
China Deep Exploration Center of the Chinese Academy of Geological Sciences, Key Laboratory of Earth Probe and Geodynamics, Beijing 100037, China
2.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Key Laboratory of Seismic Observation and Geophysical Imaging, Institute of Geophysics, China Earthquake Administration, Beijing 100081, China
4.
Institute of Geophysics, China Earthquake Administration, Beijing 100081, China

摘要

摘要: 为了调查羌塘盆地中部壳内低速层分布特征，对布设在羌塘盆地的TITAN-Ⅰ宽频带地震台站所记录的远震波形数据进行接收函数分析，并引入时频域相位滤波技术改善接收函数信噪比，反演得到各台站下方100 km深度范围内的一维S波速度结构.结果表明，时频域相位滤波方法能够显著提高信噪比；羌塘盆地Moho深度为58±6 km，具有较高的泊松比值；中下地壳壳内低速层广泛分布，横向不连续，埋深在20~30 km，层厚6~12 km，剪切波速度为3.4±0.1 km/s；部分地区在埋深为10 km的中上地壳存在一层厚约4 km的低速薄层.羌塘盆地中下地壳壳内低速层是由于上涌的深部软流圈物质与下地壳发生大范围的接触，造成壳内及上地幔部分熔融引起的.
- 羌塘盆地 /
- 接收函数分析 /
- 时频域相位滤波 /
- 非线性反演一维S波速度结构 /
- 壳内低速层 /
- 地球物理
Abstract: In order to investigate the distribution characteristics of the low velocity layer in the central Qiangtang basin, this study conducted the TITAN-Ⅰ teleseismic receiver functions across the Qiangtang basin. And the signal-to-noise ratio of the receiver function was improved by the phase filtering technique in the time frequency domain. Finally, the one-dimensional S wave velocity structure in the depth of 100 km below each station is obtained by the nonlinear inversion of conjugate gradients algorithm for the complex spectrum ratios of receiver function. The results show that the phase filtering method in the time frequency domain can significantly improve the signal-to-noise ratio and make the one-dimensional S wave velocity structure of the subsequent inversion more reliable. The Moho depth of the Qiangtang basin is 58 ±6 km, and where has a higher Poisson's ratio. The low velocity layer in the mid-lower crust is widely distributed. The transverse discontinuity is discontinuous, and the depth is between 20 and 30 km, the thickness of the layer is 6-12 km, the shear wave velocity is 3.4±0.1 km/s. In some areas, there is a thin layer of 4 km thin layer in the mid-upper crust with a depth of 10 km. The low velocity layer in the mid-lower crust of the Qiangtang basin is caused by the deep mantle derived magma upwelling along the tectonic weak zone, resulting in partial melting in the mid-lower crust and upper mantle.
- Qiangtang basin /
- receive function analysis /
- time-frequency domain phase filter /
- nonlinear inversion of one-dimensional S wave velocity structure /
- crustal low-velocity layer /
- geophysics

HTML全文

图 1 羌塘盆地宽频带地震台站分布

图中三角形表示TITAN⁃Ⅰ项目台站，将其分为88.5°线、89.5°线以及东西线，其中蓝色三角形代表中下地壳存在低速层的台站；黑色粗实线表示INDEPTH⁃Ⅲ项目台站；BNS.班公湖⁃怒江缝合带，LSS.龙木错-双湖缝合带，LT.拉萨地体，SQT.南羌塘盆地，NQT.北羌塘盆地

Fig. 1. Distribution of seismological study in Qiangtang

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图 2 本文研究中远震事件震中分布

中间红色三角形为本文研究区；周围蓝色圆点为地震事件

Fig. 2. The earthquake distribution in this study

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图 3 时频域相位滤波前后对比

a.C008号台站接收函数；b. C008号台；站时频域相位滤波后接收函数C008号台站R分量P波接收函数S相位滤波前（a）后（b）对比

Fig. 3. (a) The receive function of P wave R component of C008; (b) shows phase filter in time⁃frequency domain output of the data from (a)

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图 4 时频域相位滤波前后细节对比

a1、b1、c1为时频域滤波前的记录，分别对应图 3a方框中的部分；a2、b2、c2为滤波后的记录，分别对应图 3b方框中的部分

Fig. 4. Detail contrast before and after phase filtering

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图 5 羌塘中部泊松比分布

黑色圆点是本文的结果；红色菱形是李永华等（2006）用INDEPTH⁃Ⅲ得到的结果；蓝色三角形是刘国成等（2014）H⁃K扫描得到的结果

Fig. 5. Poisson ratio in central Qiangtang

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图 6 部分台站接收函数波形拟合结果

上方波形是垂直分量（V）拟合结果，下方波形是径向分量（R）拟合结果.红色波形是原始波形，黑色波形是拟合波形，上面的数值代表拟合系数

Fig. 6. The result of nonlinear inversion for some seismic stations

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图 7 沿88.5°线台站下方地壳S波速度结构

黑线表示反演的速度结构，红线表示IASPEI91速度模型，台站由南向北排列

Fig. 7. The S wave velocity structure along the 88.5° line

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图 8 沿东西线台站下方S波速度结构

黑线表示反演的速度结构，红线表示IASPEI91速度模型，台站由西向东排列

Fig. 8. The S wave velocity structure along the west⁃east line

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图 9 沿89.5°线台站下方地壳S波速度结构

黑线表示反演的速度结构，红线表示IASPEI91速度模型，台站由南向北排列

Fig. 9. The S wave velocity structure along the 89.5° line

下载: 全尺寸图片幻灯片

表 1 台站位置及Moho深度和泊松比

Table 1. Locations of broadband stations and measured Moho depth and σ

台站	经度(°E)	纬度(°N)	Moho(±2 km)	σ(±0.001)	接收函数数量	台站	经度(E)	纬度(N)	Moho(±2 km)	σ(±0.001)	接收函数数量
C008	88.49	33.37	61.2	0.265	54	NQT04	89.26	33.12	58.6	0.335	33
C009	88.39	33.30	61.3	0.215	56	NQT06	89.19	33.20	58.6	0.335	48
C010	88.59	33.32	58.4	0.270	61	NQT08	88.48	33.47	58.3	0.305	30
C011	88.33	33.23	58.6	0.250	66	NQT10	88.53	33.56	58.4	0.260	34
C012	88.08	33.23	53.2	0.350	82	NQT12	88.54	33.66	61.2	0.310	32
C013	88.22	33.19	55.8	0.325	66	NQT14	88.78	33.83	53.9	0.350	21
C015	88.30	33.05	61.2	0.295	47	NQT16	88.78	33.93	53.8	0.335	31
C016	88.45	33.02	58.5	0.350	29	NQT18	88.71	33.96	61.1	0.250	22
C017	88.47	32.97	53.1	0.345	35	NQT20	88.63	34.03	61.1	0.310	21
C018	88.42	32.87	53.1	0.340	30	NQT22	88.64	34.11	61.1	0.270	45
C019	88.48	32.75	61.3	0.285	56	NQT24	88.62	34.23	61.2	0.275	54
C111	87.90	33.23	61.3	0.310	68	NQT26	88.58	34.31	61.2	0.285	52
C112	87.92	33.16	64.1	0.265	28	NQT28	88.56	34.41	61.3	0.290	51
C113	88.74	33.27	60.9	0.300	43	NQT30	88.62	34.50	55.9	0.340	53
C114	88.67	33.08	61.3	0.280	52	NQT32	88.66	34.61	55.8	0.345	64
EQT02	88.96	33.11	52.9	0.335	60	NQT34	88.46	34.71	61.3	0.295	52
EQT04	89.37	33.13	55.7	0.235	64	SEQT02	89.54	32.97	53.9	0.345	23
EQT06	89.53	33.08	61.1	0.315	44	SEQT04	89.64	32.88	53.0	0.350	24
EQT08	89.55	33.19	63.9	0.335	41	SEQTO6	89.70	32.78	58.8	0.345	31
EQT10	89.51	33.32	58.4	0.350	36	SEQT08	89.72	32.68	52.9	0.345	31
EQT12	89.53	33.41	53.2	0.350	39	SEQT10	89.76	32.59	61.2	0.295	29
EQT14	89.69	33.09	53.0	0.335	25	SEQT12	89.70	32.48	53.2	0.345	25
EQT16	89.81	33.13	61.3	0.285	27	SQT01	88.63	32.20	58.8	0.345	106
EQT18	89.88	33.20	58.5	0.305	26	SQT02	88.64	32.35	61.6	0.275	60
EQT20	90.02	33.23	61.2	0.295	21	SQT03	88.61	32.47	64.2	0.270	51
EQT22	90.15	33.25	61.1	0.290	21

下载: 导出CSV

表 2 中下地壳低速层分布情况

Table 2. Low velocity layer distribution in the mid⁃lower crust

台站号	顶面埋深(±0.5 km)	底面埋深(±0.5 km)	厚度(±1.0 km)	台站号	顶面埋深(±0.5 km)	底面埋深(±0.5 km)	厚度(±1.0 km)
SQT01	20	30	10	NQT20	20	30	10
SQT02	22	30	8	NQT22	20	29	9
SQT03	22	30	8	NQT26	20	30	10
C018	18	29	11	NQT28	24	34	10
C017	24	30	6	NQT32	19	30	11
C016	21	32	11	NQT34	19	29	10
C015	25	35	10	C012	20	30	10
C011	21	31	10	C013	22	30	8
C010	20	29	9	NQT06	20	28	8
C008	23	35	12	NQT04	22	31	9
NQT08	19	25	6	EQT10	19	31	12
NQT16	22	30	8

下载: 导出CSV

参考文献(54)

Ammon, C. J., Randall, G. E., Zandt, G., 1990. On the Nonuniqueness of Receiver Function Inversions. Journal of Geophysical Research, 95(B10):15303-15318. doi: 10.1029/JB095iB10p15303
Ammon, C.J., Zandt, G., 1993.Receiver Structure beneath the Southern Mojave Block, California. Bulletin of the Seismological Society of America, 83(3):737-755.
Chi, X.G., Zhang, R., Fan, L.F., et al., 2017.The Formatting Mechanism of Cenozoic Basaltic Volcanic Rocks in the Northern Tibet:Continental Subduction and Slab Breakoff Driven by Mantle Convection and Upwelling. Acta Petrologica Sinica, 33(10):3011-3026(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201710003.htm
Cui, Z. Z., Yin, Z. X., Gao, E. Y., et al., 1990. The Structure and Tectonics of the Crust and Their Relation with Earthquakes in the Qinghai-Xizang Plateau.Acta Geoscientica Sinica, 11(2):215-232(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB199002020.htm
Gao, R., Chen, C., Lu, Z.W., et al., 2013.New Constraints on Crustal Structure and Moho Topography in Central Tibet Revealed by SinoProbe Deep Seismic Reflection Profiling. Tectonophysics, 606:160-170. https://doi.org/10.1016/j.tecto.2013.08.006
Gao, X., Wang, W.M., Yao, Z.X., et al., 2005.Crustal Structure of China Mainland and Its Adjacent Regions. Chinese Journal of Geophysics, 48(3):591-601(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqwlxb200503017
Guo, X.F., Zhang, Y.C., Cheng, Q.Y., et al., 1990.Magnetotelluric Studies along Yadong-Golmud Geosciences Transect in Qinghai-Xizang Plateau.Acta Geoscientia Sinica, 22(2):191-202(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dqxb199002018.htm
Haines, S. S., Klemperer, S. L., Brown, L., et al., 2003. INDEPTH Ⅲ Seismic Data:From Surface Observations to Deep Crustal Processes in Tibet. Tectonics, 22(1):1001. https://doi.org/10.1029/2001tc001305
He, R.Z., Gao, R., Hou, H.S., et al., 2009.Deep Structure of the Central Uplift Belt in the Qiangtang Terrane, Tibet Plateau from Broadband Seismic Observations and Its Implications. Progress in Geophysics, 24(3):900-908(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqwlxjz200903012
Huang, J. J., 2001. Structural Characteristics of the Basement of the Qiangtang Basin. Acta Geologica Sinica, 75(3):333-337(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Conference/8633148
Jiménez-Munt, I., Fernàndez, M., Vergés, J., et al., 2008.Lithosphere Structure underneath the Tibetan Plateau Inferred from Elevation, Gravity and Geoid Anomalies.Earth and Planetary Science Letters, 267(1-2):276-289. https://doi.org/10.1016/j.epsl.2007.11.045
Kind, R., Ni, J., Zhao, W., et al., 1996. Evidence from Earthquake Data for a Partially Molten Crustal Layer in Southern Tibet. Science, 274(5293):1692-1694. https://doi.org/10.1126/science.274.5293.1692
Li, C., Dong, Y.S., Zhai, Q.G., et al., 2008.Discovery of Eopaleozoic Ophiolite in the Qiangtang of Tibet Plateau:Evidence from SHRIMP U-Pb Dating and Its Tectonic Implications.Acta Petrologica Sinica, 24(1):31-36(in Chinese with English abstract).
Li, Y.H., Tian, X.B., Wu, Q.J., et al., 2006.The Poisson Ratio and Crustal Structure of the Central Qinghai-Xizang Inferred from INDEPTH-Ⅲ Teleseismic Waveforms:Geological and Geophysical Implications. Chinese Journal of Geophysics, 49(4):1037-1044(in Chinese with English abstract).
Liu, Q, Y., 1996.Maximal Likelihood Estimation and Nonlinear Inversion of the Complex Receiver Runction Spectrum Ratio. Chinese Journal of Geophysics, 39(4):500-511(in Chinese with English abstract).
Liu., G.C., Shang, X.F., He, R.Z., et al., 2014.Topography of Moho beneath the Central Qiangtang in North Tibet and Its Geodynamic Implication.Chinese Journal of Geophysics, 57(7):2043-2053(in Chinese with English abstract).
Mechie, J., Sobolev, S.V., Ratschbacher, L., et al., 2004.Precise Temperature Estimation in the Tibetan Crust from Seismic Detection of the α-β Quartz Transition.Geology, 32(7):601-604. https://doi.org/10.1130/g20367.1
Nelson, K. D., Zhao, W., Brown, L. D., et al., 1996. Partially Molten Middle Crust beneath Southern Tibet:Synthesis of Project INDEPTH Results.Science, 274(5293):1684-1688. https://doi.org/10.1126/science.274.5293.1684
Qu, Z.D., He, R.Z., Zhang, X.H., et al., 2017.The Time-Frequency Domain Phase Filter and Its Application in Noise Suppression of Teleseismic Receiver Functions. Chinese Journal of Geophysics, 60(4):1389-1397(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQWX201704013.htm
Replumaz, A., Negredo, A.M., Guillot, S., et al., 2010.Multiple Episodes of Continental Subduction during India/Asia Convergence:Insight from Seismic Tomography and Tectonic Reconstruction.Tectonophysics, 483(1-2):125-134. https://doi.org/10.1016/j.tecto.2009.10.007
Shi, D. N., Zhao, W. J., Brown, L., et al., 2004. Detection of Southward Intracontinental Subduction of Tibetan Lithosphere along the Bangong-Nujiang Suture by P-to-S Converted Waves. Geology, 32(3):209. https://doi.org/10.1130/g19814.1
Stockwell, R.G., 1999.S-Transform Analysis of Gravity Wave Activity from a Small Scale Network of Airglow Imagers.The University of Western Ontario, Canada, 4662.
Sun, M., Chen, W., Qu, X.M., et al., 2018.Petrogenesis of the Late Cretaceous Jiangba Volcanic Rocks and Its Indications for the Thinning of the Thickened Crust in Xiongmei Area, Tibet.Earth Science, 43(9):3234-3251(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201809022
Tarantola, A. P., 1987. Inverse Problem Theory:Methods for Data Fitting and Model Parameter Estimation.Physics of the Earth & Planetary Interiors, 57(3):350-351.
Teng, J.W., Ruan, X.M., Zhang, Y.Q., et al., 2012.The Stratifficational Velocity Structure of Crust and Covering Strata of Upper Mantle and the Orbit of Deep Interaquifer Substance Locus of Movement for Tibetan Plateau.Acta Petrologica Sinica, 28(12):4077-4100(in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201212022.htm
Wang, C.S., Hu, C.Z., Wu, R.Z., et al., 1987.Significance of the Discovery of Chasang-Chabu Rift in Northern Xizang(Tibet). Journal of Chengdu College of Geology, 14(2):33-46(in Chinese with English abstract).
Wang, W., Gao, X., Li, Y. Y., et al., 2011. Crustal Velocity Structure of S-Wave beneath Tibetan Plateau with Transform Function Method-Hi-Climb Profile. Chinese Journal of Geophysics, 54(6):766-776. https://doi.org/10.1002/cjg2.1660
Watanabe, T., 1993.Effects of Water and Melt on Seismic Velocities and Their Application to Characterization of Seismic Reflectors. Geophysical Research Letters, 20(24):2933-2936. https://doi.org/10.1029/93gl03170
Wu, G. J., Xiao, X. C., Li, T. D., 1989. The Yadong-Golmud Geoscience Section on the Qinghai-Tibet Plateau. Acta Geologica Sinica, 63(4):285-296(in Chinese with Eng-lish abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZXE198904000.htm
Wu, Q.J., Zeng, R.S., 1998.The Crustal Structure of QinghaiXizang Plateau Inferred from Broadband Teleseismic Waveform. Chinese Journal of Geophysics, 41(5):669-679(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQWX199805010.htm
Wu, W., Liu, Q. Y., He, R. Z., et al., 2017. Waveform Inversion of S-Wave Velocity Model in the Central Qiangtang in North Tibet and Its Geological Implications. Chinese Journal of Geophysics, 60(3):941-952(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DQWX201703010.htm
Zhang, S. Y., Zhang, X. J., 1996. Magnetotelluric Sounding in the Qiangtang Basin of Xizang (Tibet).Earth Science, 21(2):98-102(in Chinese with English abstract).
Zhao, Z., Lu, L., Wu, Z.H., et al., 2018.Charactreistics of the Late Triassic Jiangai Granite Mass and the Slab Breakoff in Central Qiangtang, Tibet. Earth Science, 43(Suppl.1):225-242(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX2018S1021.htm
Zou, C.Q., He, R.Z., Gao, R., et al., 2012.Deep Structure of the Central Uplift Belt in the Qiangtang Terrane Tibetan Plateau from Teleseismic P-Wave Tomography.Chinese Science Bulletin, 57(28-29):2729-2739(in Chinese). doi: 10.1360/972011-2430
迟效国, 张蕊, 范乐夫, 等, 2017.藏北新生代玄武质火山岩起源的深部机制:大陆俯冲和板片断离驱动的地幔对流上涌模式.岩石学报, 33(10):3011-3026. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201710003
崔作舟, 尹周勋, 高恩元, 等, 1990.青藏高原地壳结构构造及其与地震的关系.地球学报, 11(2):221-232. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=HY000001812316
高星, 王卫民, 姚振兴, 等, 2005.中国及邻近地区地壳结构.地球物理学报, 48(3):591-601. doi: 10.3321/j.issn:0001-5733.2005.03.017
郭新峰, 张元丑, 程庆云, 等, 1990.青藏高原亚东-格尔木地学断面岩石圈电性研究.地球学报, 22(2):191-202. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=HY000002240792
贺日政, 高锐, 侯贺晟, 等, 2009.羌塘中央隆起带深部结构特征研究及其意义.地球物理学进展, 24(3):900-908. doi: 10.3969/j.issn.1004-2903.2009.03.012
黄继钧, 2001.羌塘盆地基底构造特征.地质学报, 75(3):333-337. doi: 10.3321/j.issn:0001-5717.2001.03.006
李才, 董永胜, 翟庆国, 等, 2008.青藏高原羌塘早古生代蛇绿岩:堆晶辉长岩的锆石SHRIMP定年及其意义.岩石学报, 24(1):31-36. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200801002
李永华, 田小波, 吴庆举, 等, 2006.青藏高原INDEPTH-Ⅲ剖面地壳厚度与泊松比:地质与地球物理含义.地球物理学报, 49(4):1037-1044. doi: 10.3321/j.issn:0001-5733.2006.04.015
刘国成, 尚学峰, 贺日政, 等, 2014.藏北羌塘盆地中部莫霍面形态及其动力学成因.地球物理学报, 57(7):2043-2053.
刘启元, 1996.接收函数复谱比的最大或然性估计及非线性反演.地球物理学报, 39(4):500-511. doi: 10.3321/j.issn:0001-5733.1996.04.008
曲中党, 贺日政, 张训华, 等, 2017.时频域相位滤波在远震接收函数噪声压制中的应用.地球物理学报, 60(4):1389-1397. http://www.cnki.com.cn/Article/CJFDTotal-DQWX201704013.htm
孙渺, 陈伟, 曲晓明, 等, 2018.西藏雄梅地区晚白垩世江巴组火山岩岩石成因及对加厚地壳减薄的指示.地球科学, 43(9):3234-3251. http://earth-science.net/WebPage/Article.aspx?id=3939
滕吉文, 阮小敏, 张永谦, 等, 2012.青藏高原地壳与上地幔成层速度结构与深部层间物质的运移轨迹.岩石学报, 28(12):4077-4100. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201212022
王成善, 胡承祖, 吴瑞忠, 等, 1987.西藏北部查桑-茶布裂谷的发现及其地质意义.成都地质学院学报, 14(2):33-46. http://www.cnki.com.cn/Article/CJFDTotal-CDLG198702003.htm
吴功建, 肖序常, 李廷栋, 1989.青藏高原亚东-格尔木地学断面.地质学报, 63(4):285-296. doi: 10.3321/j.issn:0001-5717.1989.04.003
吴庆举, 曾融生, 1998.用宽频带远震接收函数研究青藏高原的地壳结构.地球物理学报, 41(5):669-679. doi: 10.3321/j.issn:0001-5733.1998.05.010
吴蔚, 刘启元, 贺日政, 等, 2017.羌塘盆地中部地区地壳S波速度结构及构造意义.地球物理学报, 60(3):941-952. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201703010.htm
张胜业, 张先觉, 1996.西藏羌塘盆地大地电磁测深研究.地球科学, 21(2):98-102. http://earth-science.net/WebPage/Article.aspx?id=369
赵珍, 陆露, 吴珍汉, 等, 2018.羌塘中部晚三叠世江爱岩体特征与板片断离作用.地球科学, 43(增刊1):225-242. http://earth-science.net/WebPage/Article.aspx?id=3961
邹长桥, 贺日政, 高锐, 等, 2012.远震P波层析成像研究羌塘中央隆起带深部结构.科学通报, 57(28-29):2729-2739. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb201228009