Experiments of magnetotelluric observation network on North China and lithospheric conductivity structure from fast imaging method
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摘要:
关于中国大陆岩石圈导电性结构研究越来越引起人们的重视，而目前研究大陆岩石圈导电性结构的主要方法是大地电磁测深（Magnetotelluric sounding）.为此，在国家项目"深部探测技术与实验研究（SinoProbe）"专项里开展了"大陆电磁参数标准网实验（SinoProbe-01）"研究，完成了华北1°×1°地理坐标网度的大地电磁测深"标准点"阵列（Array）观测.本文详细论述了华北SinoProbe-01项目1°×1°MT"标准点"阵列观测实验的概况，以及通过精细的MT数据处理和一维Niblett-Bostick变换快速成像，所获取的华北地区岩石圈导电性三维成像模型.在分析华北岩石圈导电性结构特征的基础上，从电性结构角度把华北与邻区岩石圈划分为胶辽、燕山、鲁西、太行—吕梁等低导电性（高电阻率）块体，内蒙古、阿拉善和祁连中等导电性块体和黄淮、鄂尔多斯、秦岭良导电性（低电阻率）块体，进一步从导电性的角度证实了华北克拉通是由多个块体集合而成的观点.
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关键词:
- 华北岩石圈 /
- 大地电磁测深“标准点”阵列 /
- Niblett-Bostick变换 /
- 导电性结构 /
- 构造格局
Abstract:The electrical resistivity structure beneath the continent of the Chinese Mainland has triggered worldwide concerns during recent several decades. The main geophysical method of surveying electrical structure of continental lithosphere is Magnetotelluric sounding (MT). Therefore, in the project SinoProbe-01 (i.e., Experimental Study of the Continental Standard Grid of Electromagnetic Parameters) belonging to the national research program SinoProbe (Deep Exploration Tecnology and Experimental Research of China), we have deployed 1°(Latitude)×1°(Longitude) standard MT array covering the entire North China. In this paper, we introduce the general situation of SinoProbe-01. In addition, we achieved the electrical resistivity structure of lithosphere beneath North China through fine data processing and rapid imaging by 1-D Niblett-Bostick transform. Based on the analysis of the lithospheric resistivity structure, the lithosphere beneath North China and its adjacent regions can be divided into several high-resistivity blocks (e.g., Jiaoliao, Yanshan, Luxi and Taihang-Lüliang), mid-conductivity blocks (e.g., Inner Mongolia, Alxa and Qilian) and low-resistivity blocks (e.g., Huanghuai, Ordos, Qinling). This observation further confirm the previous inference that the North China craton was formed though amalgamation of multiple micro-continental blocks.
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图 2
SinoProbe-MT阵列观测网布置示意图
Figure 2.
Schematic diagram of the SinoProbe-MT array observation network
图 5
华北1°×1°MT阵列观测网10839号中心测站及辅助测站宽频大地电磁测深曲线
Figure 5.
Apparent resistivity and phase curves of the 10839 central station and its auxiliaries stations belonging to the North China 1°×1° MT array
图 6
SinoProbe-MT华北阵列观测网大地电磁测深数据质量分布图
Figure 6.
The data quality classification map of the North China SinoProbe-MT observation network
图 7
华北地区地壳等厚度图(He et al., 2013)
Figure 7.
Crustal thickness contour map of the North China Craton (He et al., 2013)
图 8
华北研究区MT视电阻率频率响应结构图
Figure 8.
Apparent resistivity map of the North China at different frequency
图 9
华北大地电磁测深阵列观测网2000 s信号理论探测深度分布图
Figure 9.
Theorical penetrating depths of the 2000 s magnetotelluric signals of the North China Sinoprobe MT array
图 10
“棋盘格”模型测试一维N-B变换电阻率最大值快速成像
Figure 10.
"Checkerboard" model tests for the 1-D N-B fast resistivity imaging
图 11
华北N-B变换岩石圈三维导电性结构图
Figure 11.
Three-dimensional conductivity Structure of North China lithosphere using N-B transform
图 13
华北构造分区略图(Zhao et al., 1998, 2001)
Figure 13.
The North China tectonic map (Zhao et al., 1998, 2001)
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Ai Y S, Zheng T Y. 2003. The upper mantle discontinuity structure beneath eastern China. Geophysical Research Letters, 30(21):2089, doi:10.1029/2003GL017678.
Anderson D L. 1989. Theory of the Earth. Boston:Blackwell Scientific Publications, 348-370, 403-439.
Blundell D J, Freeman R, Mueller S. 1992. A Continent revealed:the European Geotraverse. Cambridge University Press.
Bostick F X. 1977. A Simple and Almost Exact Method of MT Analysis (Abstract). Workshop on Electrical Methods in Geothermal Exploration, Snowbird, Utah.
Chen L S, Booker J R, Jones A G, et al. 1996. Electrically conductive crust in Southern Tibet from INDEPTH magnetotelluric surveying. Science, 274(5293):1694-1696. doi: 10.1126/science.274.5293.1694
Chen L, Ai Y S. 2009. Discontinuity structure of the mantle transition zone beneath the North China Craton from receiver function migratio. Journal of Geophysical Research, 114(B6):B06307, doi:10.1029/2008JB006221.
Chen L, Cheng C, Wei Z G. 2009.Seismic evidence for significant lateral variations in lithospheric thickness beneath the central and western North China Craton. Earth and Planetary Science Letters, 286(1-2):171-183. doi: 10.1016/j.epsl.2009.06.022
Chen L, Tao W, Zhao L, et al.2008. Distinct lateral variation of lithospheric thickness in the Northeastern North China Craton. Earth and Planetary Science Letters, 267(1-2):56-68. doi: 10.1016/j.epsl.2007.11.024
Chen L, Zheng T Y, Xu W W.2006a. A thinned lithospheric image of the Tanlu Fault Zone, eastern China:Constructed from wave equation based receiver function migration. Journal of Geophysical Research, 111(B9):B09312, doi:10.1029/2005JB003974.
Chen L, Zheng T Y, Xu W W. 2006b. Receiver function migration image of the deep structure in the Bohai Bay Basin, eastern China. Geophysical Research Letters, 33(20):L20307, doi:10.1029/2006GL027593.
Chen L. 2009.Lithospheric structure variations between the eastern and central North China Craton from S-and P-receiver function migration. Physics of the Earth and Planetary Interiors, 173(3-4):216-227. doi: 10.1016/j.pepi.2008.11.011
Chen L. 2010.Concordant structural variations from the surface to the base of the upper mantle in the North China Craton and its tectonic implications. Lithos, 120(1-2):96-115. doi: 10.1016/j.lithos.2009.12.007
Clowes R M. 1993. LITHOPROBE Phase Ⅳ Proposal:Studies of the Evolution of a Continent. Vancouver:Lithoprobe Secretariat, University of British Columbia Press, 290.
Clowes R M. 1997. LITHOPROBE Phase Ⅴ Proposal:Evolution of a Continent Revealed. Vancouver:Lithoprobe Secretariat, University of British Columbia Press, 188.
Deng J F, Su S G, Liu C, et al. 2006. Discussion on the Lithospheric thinning of the North China craton:delamination? or thermal erosion and chemical metasomatism?. Earth Science Frontiers (in Chinese), 13(2):105-119. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200602012.htm
Deng J F, Su S G, Zhao H L, et al. 2003. Deep processes of Mesozoic YanShanian Lithosphere thinning in North China. Earth Science Frontiers (in Chinese), 10(3):41-50. http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY200303004.htm
Deng J F, Wei W B, Qiu R Z, et al. 2007. Three-Dimensional Structure of Lithosphere and Its Evolution in North China (in Chinese). Beijing:Geological Publishing House, 6, 29-46, 267-272.
Deng J F, Zhao H L, Mo X X, et al. 1996. Continental Roots-Plume Tectonics of China:Key to the Continental Dynamics (in Chinese). Beijing:Geological Publishing House, 59-64.
Deng Q H, Zhang M S, Zhan Y, et al. 1997. Geoelectrical structure of the crust and upple mantle in the Xingtai earthquake area and its tectonic implications. Seismology and Geology (in Chinese), 19(2):153-163. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZDZ702.007.htm
Egbert G D, Booker J R. 1986. Robust estimation of geomagnetic transfer functions. Geophysical Journal of the Royal Astronomical Society, 87(1):173-194. doi: 10.1111/gji.1986.87.issue-1
Fu C Y, Chen Y T, Qi G Z. 1985. Base of Geophysics (in Chinese). Beijing:Science Press, 1-3, 116-127.
He C, Dong S, Santosh M, et al. 2013. Destruction of the North China Craton:a perspective based on receiver function analysis. Geological Journal, 50(1):93-103. http://www.ingentaconnect.com/content/bpl/gj/2015/00000050/00000001/art00006
Huang H Z, Wu G J, Zhu Y, et al. 1994. Research Dynamics of the Lithosphere (in Chinese). Beijing:Geological Publishing House, 3-5.
Jin S, Wei W, Wang S, et al. 2010 Discussion of the formation and dynamic signification of the high conductive layer in Tibetan crust. Chinese Journal of Geophysics (in Chinese), 53(10):2376-2385. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQWX201010013.htm
Jin S, Ye G F, Wei W B, et al. 2006. The electrical structure and fault feature of crust of south-eastern Tibetan plateau-the result of magnetotelluric prospecting on profile from Xiachayu-Changdu. Earth Science Frontiers (in Chinese), 13(5):408-415. http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY200605015.htm
Jin S, Ye G F, Wei W B, et al. 2007. Electrical structure and fault features of crust and upper mantle beneath the western margin of the Qinghai-Tibet plateau:evidence from the magnetotelluric survey along Zhada-Quanshui lake profile. Journal of China University of Geosciences (in Chinese), 18(4):326-333. doi: 10.1016/S1002-0705(08)60013-8
Jin S, Ye G, Wei W, et al. 2007. The electrical structure and fault feature of crust and mantle of western tibet plateau:based on results of magnetotelluric survey along profile Zhada-Quanshuihu. Earth Science (in Chinese), 32(4):474-480. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200704006.htm
Jones A G. 1983. On the equivalence of the Niblett and Bostick transformations in the magnetotelluric method. J Geophys, 53(1):72-73. http://www.mendeley.com/research/equivalence-niblett-bostick-transformations-magnetotelluric-method/
Karato S. 1990. The role of hydrogen in the electrical conductivity of the upper mantle. Nature, 347(6290):272-273. doi: 10.1038/347272a0
Li S H, Unsworth M J, Booker J R, et al. 2003. Partial melt or aqueous fluid in the mid-crust of Southern Tibet? Constraints from INDEPTH magnetotelluric data. Geophysical Journal International, 153(2):289-304. doi: 10.1046/j.1365-246X.2003.01850.x
Niblett E R. 1960. Variation of electrical conductivity with depth by the magneto-telluric method. Geophysics, 25(5). http://adsabs.harvard.edu/abs/1960Geop...25..998N
Nover G. 2005. Electrical properties of crustal and mantle crust-a review of laboratory measurements and their explanation. Surveys in Geophysics, 26(5):593-651. doi: 10.1007/s10712-005-1759-6
Qin X L, Pedersen L B, Zhao Y L, et al. 1991. Conductivity structure of crust in the Tangshan seismic area and the possibility of exploring potential seismic sources by magnetotelluric method. Acta Seismologica Sinica (in Chinese), 13(3):354-363. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXB199103009.htm
Shi Y J, Liu G D, Wu G Y, et al. 1985. A Course in Magnetotelluric Method (in Chinese). Beijing:Seismology Press, 23-34.
Solon K D, Jones A G, Nelson K D, et al. 2005. Structure of the crust in the vicinity of the Banggong-Nujiang suture in central Tibet from INDEPTH magnetotelluric data. Journal of Geophysical Research, 110(B10):B10102. doi: 10.1029/2003JB002405
Spratt J E, Jones A G, Nelson K D, et al. 2005. Crustal structure of the India-Asia collision zone, southern Tibet, from INDEPTH MT investigations. Physics of the Earth and Planetary Interiors, 150(1-3):227-237. doi: 10.1016/j.pepi.2004.08.035
Unsworth M J, Jones A G, Wei W, et al. 2005. Crustal rheology of the Himalaya and Southern Tibet inferred from magnetotelluric data. Nature, 438(7064):78-81. doi: 10.1038/nature04154
Unsworth M. 2003. Studying continental dynamics with magnetotelluric exploration. Earth Science Frontiers, 10(1):25-38. http://manu39.magtech.com.cn/Geophy/CN/abstract/abstract14562.shtml
Unsworth M, Wei W B, Jones A G, et al. 2004. Crustal and upper mantle structure of Northern Tibet imaged with magnetotelluric data. Journal of Geophysical Research, 109(B2):B02403. http://www.mendeley.com/catalog/crustal-upper-mantle-structure-northern-tibet-imaged-magnetotelluric-data/
Unsworth M. 2003. Studying continental dynamics with magnetotelluric exploration. Earth Science Frontiers, 10(1):25-38. http://manu39.magtech.com.cn/Geophy/CN/abstract/abstract14562.shtml
Wang T, Chen L. 2009. Distinct velocity variations around the base of the upper mantle beneath Northeast Asia. Physics of the Earth and Planetary Interiors, 172(3-4):241-256. doi: 10.1016/j.pepi.2008.09.021
Wei W B, Martyn U, Jin S, et al. 2006a. Conductivity structure of crust and upper mantle beneath the northern Tibetan plateau:Results of super-wide band magnetotelluric sounding. Chinese Journal of Geophysics (in Chinese), 49(4):1098-1110. doi: 10.1002/cjg2.v49.4
Wei W B, Jin S, Ye G F, et al. 2006b. Features of faults in the central and northern Tibetan plateau based on results of INDEPTH (Ⅲ)-MT. Frontiers of Earth Science in China, 1(1):121-128. https://link.springer.com/article/10.1007/s11707-007-0016-3
Wei W B, Tan H D, Deng M, et al. 2002. Electric conductivity of the crust of the Tibetan Plateau: Ubiquitous heat flow in the crust revealed by MT Sounding. //Chen Y C ed. 80th Anniversary of the Geological Society of China Academic Papers (in Chinese). Beijing: Geological Publishing House, 487-493.
Wei W B, Unsworth M, Jones A, et al. 2001. Detection of widespread fluids in the Tibetan Crust by magnetotelluric studies. Science, 292(5517):716-719. doi: 10.1126/science.1010580
Wei W B, Ye G F, Li Y J, et al. 2007. Three-dimensional P-wave velocity structure of the crust of North China. Journal of China University of Geosciences, 18(3):257-268. doi: 10.1016/S1002-0705(08)60006-0
Wu C H, Zhong C T. 1998. The Paleoproterozoic SW-NE Collision model for the central North China Craton. Progr. Precambrian Res. (in Chinese), 21:28-50. http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ199803003.htm
Wu F Y, Ge W C, Sun D Y, et al. 2003. Discussions on the lithospheric thinning in Eastern China. Earth Science Frontiers (in Chinese), 10(3):51-60. http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY200303005.htm
Ye G F, Jin S, Wei W B, et al. 2007. Research of conductive structure of crust and upper mantle beneath the South-central Tibetan Plateau. Journal of China University of Geosciences, 18(4):334-343. doi: 10.1016/S1002-0705(08)60014-X
Zhai M G, Bian A G, Zhao T P. 2000. The amalgamation of the Supercontinent of North China Craton at the end of Neo-Archaean and its breakup during late Palaeoproterozoic and Meso-proterozoic. Science in China Series D:Earth Sciences, 43(S1):219-232. doi: 10.1007/BF02911947
Zhang F Q, Liu J Z, OUYANG, et al. 1998.Greenstone petro-tectonic frameworkof cratonic basement, north China. Chinese Journal of Geophysics (in Chinese), (S1):99-107. http://en.cnki.com.cn/Article_en/CJFDTotal-DQWX1998S1010.htm
Zhao G C, Sun M, Wilde S A, et al.2005. Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited. Precambrian Research, 136(2):177-202. doi: 10.1016/j.precamres.2004.10.002
Zhao G C, Wilde S A, Cawood P A, et al. 1998. Thermal evolution of Archean basement rocks from the eastern part of the North China Craton and its bearing on tectonic setting. International Geology Review, 40(8):706-721. doi: 10.1080/00206819809465233
Zhao G C, Wilde S A, Cawood P A, et al. 2001. Archean blocks and their boundaries in the North China Craton:Lithological, geochemical, Structural andP-T path constraints and tectonic evolution. Precambrian Research, 107(1-2):45-73. doi: 10.1016/S0301-9268(00)00154-6
Zhao G Z, Jiang Z, Liu G D, et al. 1997. Two-dimensional inversion and interpretation of MT data in a seismic active area of northern part of North China. //Proc. 30th Int'l Geol Congr, 20: 69-82.
Zhao G Z, Liu T S, Jiang Z, et al. 1997. Investigation on Mt data along Yanggao Rongcheng profile by two-dimensional inversion. Acta Geophysica Sinica (in Chinese), 40(1):38-46. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQWX199701004.htm
Zhao L, Zheng T Y, Chen L, et al.2007. Shear wave splitting in eastern and central China:implications for upper mantle deformation beneath continental margin. Physics of the Earth and Planetary Interiors, 162(1-2):73-84. doi: 10.1016/j.pepi.2007.03.004
Zhao L, Zheng T Y, Lü G. 2008. Insight into craton evolution:Constraints from shear wave splitting in the North China Craton. Physics of the Earth and Planetary Interiors, 168(3-4):153-162. doi: 10.1016/j.pepi.2008.06.003
Zhao L, Zheng T Y. 2005. Using shear wave splitting measurements to investigate the upper mantle anisotropy beneath the North China Craton:Distinct variation from east to west. Geophysical Research Letters, 32(10):L10309. doi: 10.1029/2005GL022585
Zhao L, Zheng T Y. 2007. Complex upper-mantle deformation beneath the North China Craton:implications for lithospheric thinning. Geophysical Journal International, 170(3):1095-1099. doi: 10.1111/gji.2007.170.issue-3
Zheng T Y, Chen L, Zhao L, et al. 2006.Crust-mantle structure difference across the gravity gradient zone in North China Craton:Seismic image of the thinned continental crust. Physics of the Earth and Planetary Interiors, 159(1-2):43-58. doi: 10.1016/j.pepi.2006.05.004
Zheng T Y, Chen L, Zhao L, et al. 2007.Crustal structure across the Yanshan belt at the northern margin of the North China Craton. Physics of the Earth and Planetary Interiors, 161(1-2):36-49. doi: 10.1016/j.pepi.2007.01.004
Zheng T Y, Zhao L, Xu W W, et al.2008b. Insight into modification of North China Craton from seismological study in the Shandong Province. Geophysical Research Letters, 35(22):L22305, doi:10.1029/2008GL035661.
Zheng T Y, Zhao L, Zhu R X.2008a. Insight into the geodynamics of cratonic reactivation from seismic analysis of the crust-mantle boundary. Geophysical Research Letters, 35(8):L08303, doi:10.1029/2008GL033439.
Zheng T Y, Zhao L, Zhu R X. 2009. New evidence from seismic imaging for subduction during assembly of the North China Craton. Geology, 37(5):395-398. doi: 10.1130/G25600A.1
邓晋福, 苏尚国, 赵海玲等. 2003.华北地区燕山期岩石圈减薄的深部过程.地学前缘, 10(3):41-50. http://www.cqvip.com/Main/Detail.aspx?id=9028727
邓晋福, 魏文博, 邱瑞照等. 2007.中国华北地区岩石圈三维结构及演化.北京:地质出版社, 6, 29-46, 267-272.
邓晋福, 赵海玲, 莫宣学等. 1996.中国大陆根-柱构造:大陆动力学的钥匙.北京:地质出版社, 59-64.
邓前辉, 张木生, 詹艳等. 1997.邢台震区地壳上地幔电性结构及其构造意义.地震地质, 19(2):153-163. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ702.007.htm
傅承义, 陈运泰, 祁贵仲. 1985.地球物理学基础.北京:科学出版社, 1-3, 116-127.
傅良魁.1986.岩性电测深法及其在我国的试用效果.物探与化探, 10(3), 183-192. http://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ402.007.htm
黄怀曾, 吴功建, 朱英等. 1994.岩石圈动力学研究.北京:地质出版社, 3-5.
[CM(29]金胜, 魏文博, 汪硕等. 2010.青藏高原地壳高导层的成因及动力学意义探讨——大地电磁探测提供的证据.地球物理学报, 53(10):2376-2385, doi:10.3969/j.issn.0001-5733.2010.10.011. http://manu39.magtech.com.cn/Geophy/CN/abstract/abstract3337.shtml
金胜, 魏文博, 叶高峰等. 2009.班公-怒江构造带的电性结构特征——大地电磁探测结果.地球物理学报, 52(10):2666-2675, doi:10.3969/j.issn.0001-5733.2009.10.027. http://manu39.magtech.com.cn/Geophy/CN/abstract/abstract1217.shtml
金胜, 叶高峰, 魏文博等. 2006.青藏高原东南部地壳导电性结构与断裂构造特征——下察隅-昌都剖面大地电磁探测结果.地学前缘, 13(5):408-415. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDW200610001541.htm
金胜, 叶高峰, 魏文博等. 2007.青藏高原西缘壳幔电性结构与断裂构造:札达-泉水湖剖面大地电磁探测提供的依据.地球科学-中国地质大学学报, 32(4):474-480. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx200704005
秦馨菱, Pedersen L B, 赵玉林等. 1991.唐山地震区地壳电性结构及MT探索潜在震源的可能性.地震学报, 13(3):354-363. http://www.cqvip.com/QK/93548X/199103/462661.html
石应骏, 刘国栋, 吴广耀等. 1985.大地电磁测深法教程.北京:地震出版社, 23-34.
魏文博, 金胜, 叶高峰等. 2003.大陆岩石圈导电性的研究方法.地学前缘, 10(1):15-23. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200301003
魏文博, 金胜, 叶高峰等. 2006a.藏北高原地壳及上地幔导电性结构——超宽频带大地电磁测深研究结果.地球物理学报, 49(4):1215-1225, doi:10.3321/j.issn:0001-5733.2006.04.038. http://manu39.magtech.com.cn/Geophy/CN/abstract/abstract22.shtml
魏文博, 金胜, 叶高峰等. 2006b.西藏高原中、北部断裂构造特征:INDEPTH(Ⅲ)-MT观测提供的依据.地球科学——中国地质大学学报, 31(2):257-265. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dqkx200602016&dbname=CJFD&dbcode=CJFQ
魏文博, 金胜, 叶高峰等. 2009.藏南岩石圈导电性结构与流变性-超宽频带大地电磁测深研究结果.中国科学D辑:地球科学, 39(11):1591-1601. http://www.doc88.com/p-6843137038833.html
魏文博, 谭捍东, 邓明等. 2002. 西藏高原地壳的导电性-大地电磁深探测发现西藏的地壳普遍存在流体. //陈毓川. 中国地质学会80周年学术文集. 北京: 地质出版社, 487-493.
魏文博, 叶高峰, 金胜等. 2007.华北地区地壳P波三维速度结构.地球科学——中国地质大学学报, 32(4):441-452. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXB201001002.htm
吴昌华, 钟长汀. 1998.华北陆台中段吕梁期SW-NE向碰撞——晋蒙高级区孔兹岩系进入下地壳的构造机制.前寒武纪研究进展, 21 (3):28-50. http://www.doc88.com/p-5943110814695.html
吴福元, 葛文春, 孙德有等. 2003.中国东部岩石圈减薄研究中的几个问题.地学前缘, 10(3):51-60. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200303005.htm
叶高峰, 金胜, 魏文博等. 2007.西藏高原中南部地壳与上地幔导电性结构.地球科学——中国地质大学学报, 32(4):491-498. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dqkx200704009&dbname=CJFD&dbcode=CJFQ
翟明国, 卞爱国. 2000.华北克拉通新太古代末超大陆拼合及古元古代末-中元古代裂解.中国科学:地球科学, 30(s1):129-137. http://mall.cnki.net/magazine/article/JDXK2000S1016.htm
张福勤, 刘建忠, 欧阳自远. 1998.华北克拉通基底绿岩的岩石大地构造学研究.地球物理学报, (s1):99-107. http://manu39.magtech.com.cn/Geophy/CN/abstract/abstract7393.shtml
赵国泽, 刘铁胜, 江钊等. 1997.山西阳高-河北容城剖面大地电磁资料的二维反演解释.地球物理学报, 40(1):38-46. http://manu39.magtech.com.cn/Geophy/CN/abstract/abstract3978.shtml
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