Abstract
The North Himalayan gneiss domes (NHGD), as one of the extensional structures widely distributed across the southern Tibetan Plateau, are an important window for studying post-collisional diastrophism and magmation as well as polymetallic mineralization. However, the deep mechanism for the formation of NHGD remains controversial. The magneto-telluric (MT) method was adopted to study the deep structure of the Cuonadong dome in the Northern Himalayas. The characteristics of the dome were explored by using the MT sounding curves and phase tensors. Three-dimensional (3D) MT inversion was performed to determine the electrical resistivity structure beneath the Cuonadong dome. The preferred 3D electrical resistivity model shows that an obvious low-resistivity anomaly develops beneath the Cuonadong dome which is overlaid by a high-resistivity body and surrounded by an apparent subcircular zone of low-resistivity anomalies. The integrated conductivity (longitudinal conductance) from depths of 1–20 km indicates that the average longitudinal conductance at the core of the Cuonadong dome is about 10,000 S. The high-conductivity anomaly at the core is found to be analogous to that of lava, mainly resulting from the crustal partial melting, and the estimated melt content is 11.0–17.3%. The high conductance surrounding the dome reaches 20,000 S on average, which is mainly attributed to saline fluids. MT results in this study support that the Cuonadong dome experienced magmatic diapirism. Taken together with previous geological and geochemical studies, we suggest that under the east-west (E-W) extensional tectonic setting in southern Tibet, deep crustal partial melting constantly accumulated beneath the dome, and therefore the magmatic diapirism resulted in the formation of the Cuonadong dome. In addition, the MT results also indicate that the development of the Cuonadong dome provides abundant mineralizing fluids and the space for migration of metallogenic fluids for (rare-metal) polymetallic mineralization.
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References
Armijo R, Tapponnier P, Mercier J L, Han T L. 1986. Quaternary extension in southern Tibet: Field observations and tectonic implications. J Geophys Res, 91: 13803–13872
Bai D, Unsworth M J, Meju M A, Ma X B, Teng J W, Kong X R, Sun Y, Sun J, Wang L F, Jiang C S, Zhao C P, Xiao P F, Liu M. 2010. Crustal deformation of the eastern Tibetan Plateau revealed by magnetotelluric imaging. Nat Geosci, 3: 358–362
Bao X W, Sun X X, Xu M J, Eaton D W, Song X D, Wang L S, Ding Z F, Mi N, Li H, Yu D Y, Huang Z C, Wang P. 2015. Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions. Earth Planet Sci Lett, 415: 16–24
Beaumont C, Jamieson R A, Nguyen M H, Lee B. 2001. Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation. Nature, 414: 738–742
Beaumont C, Jamieson R A, Nguyen M H, Medvedev S. 2004. Crustal channel flows: 1. Numerical models with applications to the tectonics of the Himalayan-Tibetan orogen. J Geophys Res-Solid Earth, 109: B06406
Bibby H M, Caldwell T G, Brown C. 2005. Determinable and non-determinable parameters of galvanic distortion in magnetotellurics. Geophys J Int, 163: 915–930
Booker J R. 2014. The magnetotelluric phase tensor: A critical review. Surv Geophys, 35: 7–40
Burchfiel B C, Royden L H. 1985. North-south extension within the convergent Himalayan region. Geology, 13: 679–682
Burg J P, Brunel M, Gapais D, Chen G M, Liu G H. 1984. Deformation of leucogranites of the crystalline Main Central Sheet in southern Tibet (China). J Struct Geol, 6: 535–542
Cai J C, Wei W, Hu X Y, Wood D A. 2017. Electrical conductivity models in saturated porous media: A review. Earth-Sci Rev, 171: 419–433
Caldwell T G, Bibby H M, Brown C. 2004. The magnetotelluric phase tensor. Geophys J Int, 158: 457–469
Chen J Y, Gaillard F, Villaros A, Yang X S, Laumonier M, Jolivet L, Unsworth M, Hashim L, Scaillet B, Richard G. 2018. Melting conditions in the modern Tibetan crust since the Miocene. Nat Commun, 9: 3515
Chen X B, Ye T, Cai J T, Wang L F. 2019. Refined techniques for data processing and two-dimensional inversion in magnetotelluric (VII): Structure and seismogenic environment of Yingjiang-Longling seismic area (in Chinese). Chin J Geophys, 62: 1377–1393
Clark M K, Royden L H. 2000. Topographic ooze: Building the eastern margin of Tibet by lower crustal flow. Geology, 28: 703–706
Comeau M J, Unsworth M J, Ticona F, Sunagua M. 2015. Magnetotelluric images of magma distribution beneath Volcán Uturuncu, Bolivia: Implications for magma dynamics. Geology, 43: 243–246
Dong H, Wei W B, Jin S, Ye G F, Zhang L T, Jing J E, Yin Y T, Xie C L, Jones A G. 2016. Extensional extrusion: Insights into south-eastward expansion of Tibetan Plateau from Magnetotelluric array data. Earth Planet Sci Lett, 454: 78–85
Dong H, Wei W B, Jin S, Ye G F, Jones A G, Zhang L T, Jing J E, Xie C L, Yin Y T. 2020. Shaping the surface deformation of central and south Tibetan Plateau: Insights from magnetotelluric array data. J Geophys Res-Solid Earth, 125: e19206
Dong L, Li G M, Wang Y, Xiang A P, Cao H W, Huang B. 2020. Geochronology, geochemistry and their geological significances of hornblende schists from the Yardoi dome, Southern Tibet, China (in Chinese). Acta Mineral Sin, 40: 556–568
Dong X, Li W H, Lu Z W, Huang X F, Gao R. 2020. Seismic reflection imaging of crustal deformation within the eastern Yarlung-Zangbo suture zone. Tectonophysics, 780: 228395
Egbert G D. 1997. Robust multiple-station magnetotelluric data processing. Geophys J Int, 130: 475–496
Egbert G D, Kelbert A. 2012. Computational recipes for electromagnetic inverse problems. Geophys J Int, 189: 251–267
Fu J G, Li G M, Wang G H, Huang Y, Zhang L K, Dong S L, Liang W. 2017. First field identification of the Cuonadong dome in southern Tibet: Implications for EW extension of the North Himalayan gneiss dome. Int J Earth Sci-Geol Rundsch, 106: 1581–1596
Fu J G, Li G M, Wang G H, Zhang L K, Liang W, Zhang Z, Zhang X Q, Huang Y. 2018. Synchronous granite intrusion and E-W extension in the Cuonadong dome, southern Tibet, China: Evidence from field observations and thermochronologic results. Int J Earth Sci-Geol Rundsch, 107: 2023–2041
Gao J, Zhang H J, Zhang S Q, Xin H L, Li Z W, Tian W, Bao F, Cheng Z P, Jia X F, Fu L. 2020. Magma recharging beneath the Weishan volcano of the intraplate Wudalianchi volcanic field, northeast China, implied from 3-D magnetotelluric imaging. Geology, 48: 913–918
Gao L E, Gao J H, Zhao L H, Hou K J, Tang S H. 2017. The Miocene leucogranite in the Nariyongcuo Gneiss Dome, southern Tibet: Products from melting metapelite and fractional crystallization (in Chinese). Acta Petrol Sin, 33: 2395–2411
Gao R, Lu Z W, Klemperer S L, Wang H Y, Dong S W, Li W H, Li H Q. 2016. Crustal-scale duplexing beneath the Yarlung Zangbo suture in the western Himalaya. Nat Geosci, 9: 555–560
Guo L, Zhang J, Zhang B. 2008. Structures, kinematics, thermochronology and tectonic evolution of the Ramba gneiss dome in the northern Himalaya. Prog Nat Sci, 18: 851–860
Ha G H, Wu Z H, He L. 2018. Late Cenozoic sedimentary strata of Qiongduojiang Graben, south Tibet: Preliminary constraint on the initial rifting age of the S-N trending rift (in Chinese). Acta Geol Sin, 92: 2051–2067
Harris N, Massey J. 1994. Decompression and anatexis of Himalayan metapelites. Tectonics, 13: 1537–1546
Harrison T M, Lovera O M, Grove M. 1997. New insights into the origin of two contrasting Himalayan granite belts. Geology, 25: 899–902
Hashim L, Gaillard F, Champallier R, Le Breton N, Arbaret L, Scaillet B. 2013. Experimental assessment of the relationships between electrical resistivity, crustal melting and strain localization beneath the Himalayan-Tibetan Belt. Earth Planet Sci Lett, 373: 20–30
Heise W, Pous J. 2003. Anomalous phases exceeding 90° in magneto-tellurics: Anisotropic model studies and a field example. Geophys J Int, 155: 308–318
Hill G J, Bibby H M, Ogawa Y, Wallin E L, Bennie S L, Caldwell T G, Keys H, Bertrand E A, Heise W. 2015. Structure of the Tongariro Volcanic system: Insights from magnetotelluric imaging. Earth Planet Sci Lett, 432: 115–125
Hill G J, Caldwell T G, Heise W, Chertkoff D G, Bibby H M, Burgess M K, Cull J P, Cas R A F. 2009. Distribution of melt beneath Mount St Helens and Mount Adams inferred from magnetotelluric data. Nat Geosci, 2: 785–789
Hou Z Q. 2010. Metallogensis of Continental Collision (in Chinese). Acta Geol Sin, 84: 30–58
Hou Z Q, Cook N J. 2009. Metallogenesis of the Tibetan collisional orogen: A review and introduction to the special issue. Ore Geol Rev, 36: 2–24
Hou Z Q, Qu X M, Yang Z S, Meng X J, Li Z Q, Yang Z M, Zheng M P, Zheng Y Y, Nie F J, Gao Y F, Jiang S H, Li G M. 2006. Metallogenesis in Tibetan collisional orogenic belt: III, Mineralization in post-collisional extension setting (in Chinese). Mineral Deposit, 25: 629–651
Hou Z Q, Zheng Y C, Zeng L S, Gao L E, Huang K X, Li W, Li Q Y, Fu Q, Liang W, Sun Q Z. 2012. Eocene-Oligocene granitoids in southern Tibet: Constraints on crustal anatexis and tectonic evolution of the Himalayan orogen. Earth Planet Sci Lett, 349–350: 38–52
Hu X Y, Lin W L, Yang W C, Yang B. 2020. A review on developments in the electrical structure of craton lithosphere. Sci China Earth Sci, 63: 1661–1677
Jiao Y J, Huang X R, Li G M, Liang S X, Guo J. 2019. Deep structure and mineralization of Zhaxikang ore-concentration Area, South Tibet: Evidence from geophysics (in Chinese). Earth Sci, 44: 2117–2128
Jin S, Wei W B, Wang S, Ye G F, Deng M, Tan H D. 2010. Distribution of the formation and dynamic signification of the high conductive layer in Tibetan crust (in Chinese). Chin J Geophys, 53: 2376–2385
Le Fort P, Cuney M, Deniel C, France-Lanord C, Sheppard S M F, Upreti B N, Vidal P. 1987. Crustal generation of the Himalayan leucogranites. Tectonophysics, 134: 39–57
Lee J, Hacker B R, Dinklage W S, Wang Y, Gans P, Calvert A, Wan J L, Chen W, Blythe A E, McClelland W. 2000. Evolution of the Kangmar Dome, southern Tibet: Structural, petrologic, and thermochronologic constraints. Tectonics, 19: 872–895
Lee J, McClelland W, Wang Y, Blythe A, McWilliams M. 2006. Oligocene-Miocene middle crustal flow in southern Tibet: Geochronology of Mabja Dome. Geol Soc London Spec Publ, 268: 445–469
Li D W, Liu D M, Liao Q A, Zhang X H, Yuan Y M. 2003. Definition and significance of the Lhagoi Kangri metamorphic core complexes in Sagya, southern Tibet (in Chinese). Geol Bull China, 22: 303–307
Li G M, Zhang L K, Jiao Y J, Xia X B, Dong S L, Fu J G, Liang W, Zhang Z, Wu J Y, Dong L, Huang Y. 2017. First discovery and implications of Cuonadong superlarge Be-W-Sn polymetallic deposit in Himalayan metallogenic belt, southern Tibet (in Chinese). Mineral Deposit, 36: 1003–1008
Li H L, Li G M, Li Y X, Dong S L, Qing C S, Fu J G, Liu H, Huang H X. 2017. A study on ore geological characteristics and fluid inclusions of Jienagepu gold deposit in Zhaxikang ore concentration district, Southern Tibet, China (in Chinese). Acta Mineral Sin, 37: 684–696
Li H Q, Gao R, Li W H, Carbonell R, Yelisetti S, Huang X F, Shi Z X, Lu Z W. 2021. The Mabja dome structure in southern Tibet revealed by deep seismic reflection data and its tectonic implications. J Geophys Res-Solid Earth, 126: e20265
Li S, Weng A, Li J, Shan X, Han J, Tang Y, Zhang Y, Wang X. 2020. Deep origin of Cenozoic volcanoes in Northeast China revealed by 3-D electrical structure. Sci China Earth Sci, 63: 533–547
Liang H D, Jin S, Wei W B, Gao R, Ye G F, Zhang L T, Yin Y T, Lu Z W. 2018. Lithospheric electrical structure of the middle Lhasa terrane in the south Tibetan Plateau. Tectonophysics, 731–732: 95–103
Liang W. 2019. Characteristics of ore-forming fluids in Himalayan Au−Sb−Pb−Zn polymetallic belt: Constraints from H-O isotopes (in Chinese). Earth Sci, 44: 2308–2318
Liang W, Li G M, Zhang L K, Fu J G, Huang Y, Zhang Z. 2020. Cuonadong Be-rare polymetallic metal deposit: Constraints from Ar-Ar age of hydrothermal muscovite (in Chinese). Sediment Geol Tethyan Geol, 40: 76–81
Lin B, Tang J X, Zheng W B, Leng Q F, Lin X, Wang Y Y, Meng Z, Tang P, Ding S, Xu Y F, Yuan M. 2016. Geochemical characteristics, age and genesis of Cuonadong leucogranite, Tibet (in Chinese). Acta Petrol ET Mineral, 35: 391–406
Lou Y L, Chen W, Yuan Y S, Yang T. 2018. Fluid inclusion and H, O, and S isotopic composition of Qiaga stibnite deposit in Longzi County, Tibet (in Chinese). Mineral Deposit, 37: 1124–1140
Meqbel N M, Egbert G D, Wannamaker P E, Kelbert A, Schultz A. 2014. Deep electrical resistivity structure of the northwestern U.S. derived from 3-D inversion of USArray magnetotelluric data. Earth Planet Sci Lett, 402: 290–304
Meqbel N M, Weckmann U, Muñoz G, Ritter O. 2016. Crustal metamorphic fluid flux beneath the Dead Sea Basin: Constraints from 2-D and 3-D magnetotelluric modelling. Geophys J Int, 207: 1609–1629
Nábělek J, Hetényi G, Vergne J, Sapkota S, Kafle B, Jiang M, Su H, Chen J, Huang B S, the Hi-Climb Team. 2009. Underplating in the Himalaya-Tibet collision zone revealed by the Hi-CLIMB experiment. Science, 325: 1371–1374
Ni H W, Keppler H, Behrens H. 2011. Electrical conductivity of hydrous basaltic melts: Implications for partial melting in the upper mantle. Contrib Mineral Petrol, 162: 637–650
Nie F J, Hu P, Jiang S H, Li Z Q, Liu Y, Zhou Y Z. 2005. Type and temporal-spatial distribution of gold and antimony deposits (prospects) in Southern Tibet, China (in Chinese). Acta Geol Sin, 79: 373–385
Ogawa Y, Ichiki M, Kanda W, Mishina M, Asamori K. 2014. Three-dimensional magnetotelluric imaging of crustal fluids and seismicity around Naruko volcano, NE Japan. Earth Planet Sp, 66: 158
Pang Y J, Zhang H, Gerya T V, Liao J, Cheng H H, Shi Y L. 2018. The mechanism and dynamics of N-S rifting in southern Tibet: Insight from 3-D thermomechanical modeling. J Geophys Res-Solid Earth, 123: 859–877
Spratt J E, Jones A G, Nelson K D, Unsworth M J. 2005. Crustal structure of the India-Asia collision zone, southern Tibet, from INDEPTH MT investigations. Phys Earth Planet Inter, 150: 227–237
Sun X Y, Zhan Y, Unsworth M M, Egbert G, Zhang H P, Chen X B, Zhao G Z, Sun J B, Zhao L Q, Cui T F, Liu Z Y, Han J. 2020. 3-D magnetotelluric imaging of the easternmost Kunlun Fault: Insights into strain partitioning and the seismotectonics of the Jiuzhaigou Ms7.0 earthquake. J Geophys Res-Solid Earth, 125: e19731
Tapponnier P, Xu Z, Roger F, Meyer B, Arnaud N, Wittlinger G, Yang J. 2001. Oblique stepwise rise and growth of the Tibet Plateau. Science, 294: 1671–1677
Ten Grotenhuis S M, Drury M R, Spiers C J, Peach C J. 2005. Melt distribution in olivine rocks based on electrical conductivity measurements. J Geophys Res, 110: B12201
Unsworth M J, Wei W B, Jones A G, Li S H, Bedrosian P, Booker J, Sheng J, Ming D, Tan H D. 2004. Crustal and upper mantle structure of northern Tibet imaged with magnetotelluric data. J Geophys Res, 109: B02403
Unsworth M J, Jones A G, Wei W B, Marquis G, Gokarn S G, Spratt J E, The INDEPTH-MT Team. 2005. Crustal rheology of the Himalaya and Southern Tibet inferred from magnetotelluric data. Nature, 438: 78–81
Wang R C, Wu F Y, Xie L, Liu X C, Wang J M, Yang L, Lai W, Liu C. 2017. A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts, South Tibet. Sci China Earth Sci, 60: 1655–1663
Wang X B, Zhang G, Zhou J, Li D W, Luo W, Hu Y B, Cai X L, Guo Z M. 2018. Crust and upper mantle electrical resistivity structure in the Longmenshan tectonic belt and its relationship with Wenchuan and Lushan earthquakes (in Chinese). Chin J Geophys, 61: 1984–1995
Wang X X, Zhang J J, Yan S Y, Liu J. 2016. Age and geochemistry of the Cuona leucogranite in southern Tibet and its geological implications (in Chinese). Geol Bull China, 35: 91–103
Wu F Y, Liu Z C, Liu X C, Ji W Q. 2015. Himalayan leucogranite: Petrogenesis and implications to orogenesis and plateau uplift (in Chinese). Acta Petrol Sin, 31: 1–36
Wu F Y, Liu X C, Liu Z C, Wang R C, Xie L, Wang J M, Ji W Q, Yang L, Liu C, Khanal G P, He S X. 2020. Highly fractionated Himalayan leucogranites and associated rare-metal mineralization. Lithos, 352–353: 105319
Wu Z H, Zhang Y S, Hu D G, Zhao X T, Ye P S. 2007. Late Cenozoic normal faulting of the Qungdo’gyang graben in the central segment of the Cona-Oiga rift, southeastern Tibet (in Chinese). J Geomech, 13: 297–306
Xia X B, Li G M, Cao H W, Liang W, Fu J G. 2019. Petrogenic age and geochemical characteristics of the mother rock of skarn type ore body in the Cuonadong Be-W-Sn polymetallic deposit, Southern Tibet (in Chinese). Earth Sci, 44: 2207–2223
Xiao Q B, Zhang J, Zhao G Z, Wang J J. 2013. Electrical resistivity structures northeast of the Eastern Kunlun Fault in the Northeastern Tibet: Tectonic implications. Tectonophysics, 601: 125–138
Xie C L, Jin S, Wei W B, Ye G F, Zhang L T, Dong H, Yin Y T. 2017. Varying Indian crustal front in the southern Tibetan Plateau as revealed by magnetotelluric data. Earth Planets Space, 69: 147
Xie Y L, Li L M, Wang B G, Li G M, Liu H F, Li Y X, Dong S L, Zhou J J. 2017. Genesis of the Zhaxikang epithermal Pb-Zn-Sb deposit in southern Tibet, China: Evidence for a magmatic link. Ore Geol Rev, 80: 891–909
Xu Y, Yang X, Zheng J, Xia Q. 2019. The origins and geodynamic implications of mid-lithospheric discontinuities (in Chinese). Chin Sci Bull, 64: 2305–2315
Xu Z Q, Yang J S, Qi X X, Cui J W, Li H B, Chen F Y. 2006. India-Asia collision: A further discussion of N-S and E-W trending detachments and the orogenic mechanism of the modern Himalayas (in Chinese). Geol Bull China, 25: 1–14
Xue S, Bai D, Chen Y, Ma X, Chen L, Li X, Yan Y. 2019. Contrasting crustal deformation mechanisms in the Longmenshan and West Qinling orogenic belts, NE Tibet, revealed by magnetotelluric data. J Asian Earth Sci, 176: 120–128
Xue S, Chen Y, Liang H D, Li X, Liang X F, Ma X B, Lu Z W, Bai D H, Yan Y L. 2021. Deep electrical resistivity structure across the Gyaring Co Fault in Central Tibet revealed by magnetotelluric data and its implication. Tectonophysics, 809: 228835
Yang Z S, Hou Z Q, Gao W, Wang H P, Li Z Q, Meng X J, Qu X M. 2006. Metallogenic characteristics and genetic model of antimony and gold deposits in south Tibetan detachment system (in Chinese). Acta Geol Sin, 80: 1377–1391
Ye T, Huang Q H, Chen X B, Zhang H Q, Chen Y J, Zhao L, Zhang Y. 2018. Magma chamber and crustal channel flow structures in the Tengchong volcano area from 3-D MT inversion at the intracontinental block boundary southeast of the Tibetan Plateau. J Geophys Res-Solid Earth, 123: 11112–11126
Yin A. 2006. Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation. Earth-Sci Rev, 76: 1–131
Yin C C, Liu Y H, Xiong B. 2020. Status and prospect of 3D inversions in EM geophysics. Sci China Earth Sci, 63: 452–455
Yu N, Unsworth M, Wang X B, Li D W, Wang E C, Li R H, Hu Y B, Cai X L. 2020. New insights into crustal and mantle flow beneath the Red River Fault zone and adjacent areas on the southern margin of the Tibetan Plateau revealed by a 3-D magnetotelluric study. J Geophys Res-Solid Earth, 125: e19396
Zeng L S, Gao L E, Xie K J, Liu-Zeng J. 2011. Mid-Eocene high Sr/Y granites in the Northern Himalayan Gneiss Domes: Melting thickened lower continental crust. Earth Planet Sci Lett, 303: 251–266
Zeng L S, Liu J, Gao L, Xie K J, Wen L. 2009. Early Oligocene anatexis in the Yardoi gneiss dome, southern Tibet and geological implications (in Chinese). Chin Sci Bull, 54: 104–112
Zhang B, Zhang J J, Guo L, Wang W L. 2005. Structural characteristics and deformation analysis of mylonite belt in the detachment fault system of Yalashabpo metamorphic core complex in the bending-uplift belt of the Northern Himalayas (in Chinese). Progr Nat Sci, 15: 692–699
Zhang H Q, Huang Q H, Zhao G Z, Guo Z, Chen Y S. 2016. Three-dimensional conductivity model of crust and uppermost mantle at the northern Trans North China Orogen: Evidence for a mantle source of Datong volcanoes. Earth Planet Sci Lett, 453: 182–192
Zhang J J. 2007. A review on the extensional structures in the northern Himalaya and southern Tibet (in Chinese). Geol Bull China, 26: 639–649
Zhang J J, Guo L. 2007. Structure and geochronology of the southern Xainza-Dinggye rift and its relationship to the south Tibetan detachment system. J Asian Earth Sci, 29: 722–736
Zhang J J, Santosh M, Wang X X, Guo L, Yang X Y, Zhang B. 2012. Tectonics of the northern Himalaya since the India-Asia collision. Gondwana Res, 21: 939–960
Zhang L K, Zhang Z, Li G M, Dong S L, Xia X B, Liang W, Fu J G, Cao H W. 2018. Rock assemblage, structural characteristics and genesis mechanism of the Cuonadong Dome, Tethys Himalaya (in Chinese). Earth Sci, 43: 2664–2683
Zhang Z, Zhang L K, Li G M, Liang W, Xia X B, Fu J G, Dong S L, Ma G T. 2017. The Cuonadong Gneiss Dome of North Himalaya: A new member of gneiss dome and a new proposition for the ore-controlling role of North Himalaya gneiss domes (in Chinese). Acta Geosci Sin, 38: 754–766
Zhao G Z, Unsworth M J, Zhan Y, Wang L F, Chen X B, Jones A G, Tang J, Xiao Q B, Wang J J, Cai J T, Li T, Wang Y Z, Zhang J H. 2012. Crustal structure and rheology of the Longmenshan and Wenchuan Mw7.9 earthquake epicentral area from magnetotelluric data. Geology, 40: 1139–1142
Acknowledgements
The in-situ data were collected with assistance of Haoping HONG, Jiawei WU, and Zhehan LIU from China University of Geosciences (Beijing). Sincere thanks are given to the two anonymous reviewers for their constructive comments. This work was supported by the National Natural Science Foundation of China (Grant Nos. 91962109, 42174094), the Second Tibetan Plateau Scientific Expedition and Research Program (STEP) (Grant No. 2019QZKK0701), the Fund of Chinese Geological Survey (Grant No. DD20190016), and the Basic Scientific Research Fund of the Institute of Geology, Chinese Academy of Geological Sciences (Grant No. J2015).
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Xue, S., Lu, Z., Li, W. et al. Three-dimensional electrical resistivity structure beneath the Cuonadong dome in the Northern Himalayas revealed by magnetotelluric data and its implication. Sci. China Earth Sci. 65, 1538–1553 (2022). https://doi.org/10.1007/s11430-021-9900-y
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DOI: https://doi.org/10.1007/s11430-021-9900-y