Late Mesozoic porphyry copper deposits in NE China: Post-collisional versus subduction-related magmatic systems

Bizheng Yang , Fanbo Meng , Yuzhou Feng , Xinran Ni , Changzhou Deng , Jingjing Zhu , Runsheng Yin , Huayong Chen

Geoscience Frontiers ›› 2026, Vol. 17 ›› Issue (1) : 102190

PDF
Geoscience Frontiers ›› 2026, Vol. 17 ›› Issue (1) :102190 DOI: 10.1016/j.gsf.2025.102190
research-article
Late Mesozoic porphyry copper deposits in NE China: Post-collisional versus subduction-related magmatic systems
Author information +
History +
PDF

Abstract

Recent discoveries of Late Mesozoic porphyry Cu deposits (PCDs) in Northeast (NE) China reveal a distinct spatial metallogenic zonation, with Late Jurassic PCDs in the north dominated by Cu-Mo and Early Cretaceous PCDs in the east marked by Cu-Au mineralization. However, the mechanisms controlling this metallogenic contrast remain unclear. To tackle this issue, we combined geological, geochronological, and geochemical data to determine the genesis of these deposits and the key factors controlling their distinct Cu-Mo and Cu-Au mineralization. Geochronological data show that the Late Jurassic PCDs were formed during a short-lived mineralization event (ca. 150-147 Ma), in contrast to the Early Cretaceous PCDs, which exhibit a prolonged formation history (ca. 120-95 Ma). Geochemical data demonstrate that the northern Cu-Mo PCDs originate from partial melting of thickened juvenile lower crust, whereas the eastern Cu-Au PCDs result from oceanic crust-derived melts contaminated by mantle wedge materials. Integrated analysis suggests that the Cu-Mo PCDs formed in a post-collisional setting after the Mongol-Okhotsk Ocean closure, while the Cu-Au PCDs formed in a subduction setting associated with Paleo-Pacific oceanic plate subduction. Despite the presence of hydrous and oxidized magmas in both regions, the northern PCDs exhibit higher Sr/Y, La/Yb, and Sm/Yb ratios than the eastern PCDs, indicating greater magma differentiation depths controlled by crustal thickness. We therefore propose that the depths of magma differentiation govern the metallogenic zoning of Late Mesozoic PCDs in NE China.

Keywords

Late Mesozoic / Porphyry copper deposits / NE China / Post-collisional / Subduction

Cite this article

Download citation ▾
Bizheng Yang, Fanbo Meng, Yuzhou Feng, Xinran Ni, Changzhou Deng, Jingjing Zhu, Runsheng Yin, Huayong Chen. Late Mesozoic porphyry copper deposits in NE China: Post-collisional versus subduction-related magmatic systems. Geoscience Frontiers, 2026, 17(1): 102190 DOI:10.1016/j.gsf.2025.102190

登录浏览全文

4963

注册一个新账户 忘记密码

CRediT authorship contribution statement

Bizheng Yang: Conceptualization, Investigation, Methodology, Data curation, Formal analysis, Writing - original draft. Fanbo Meng: Conceptualization, Investigation, Writing - original draft. Yuzhou Feng: Conceptualization, Data curation, Writing - original draft, Writing - review & editing. Xinran Ni: Investigation, Writing - original draft. Changzhou Deng: Conceptualization, Data curation, Formal analysis, Funding acquisition, Project administration, Investigation, Methodology, Writing - original draft, Writing - review & editing. Jingjing Zhu: Data curation, Writing - review & editing. Runsheng Yin: Investigation, Data curation, Writing - review & editing. Huayong Chen: Conceptualization, Data curation, Writing - original draft, Writing - review & editing.

Declaration of competing interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Acknowledgements

This work was supported by the National Natural Science Foundation of China (42273072), the Natural Science Foundation of Heilongjiang Province (LH2022D028). We are grateful to Dr. Mingliang Huang for his valuable comments and suggestions on this paper.

Appendix A. Supplementary data

Supplementary data to this article can be found online at https://doi.org/10.1016/j.gsf.2025.102190.

References

[1]

Asadi, S., Moore, F., Zarasvandi, A., 2014. Discriminating productive and barren porphyry copper deposits in the southeastern part of the central Iranian volcano-plutonic belt, Kerman region, Iran: a review. Earth Sci. Rev. 138, 25-46.

[2]

Ballard, J.R., Palin, M.J., Campbell, I.H., 2002. Relative oxidation states of magmas inferred from Ce (IV)/Ce (III) in zircon: application to porphyry copper deposits of northern Chile. Contrib. Mineral. Petrol. 144, 347-364.

[3]

Bao, X.S., He, W.Y., Mao, J.W., Liang, T., Wang, H., Zhou, Y.M., Wang, J.J., 2023. Redox states and genesis of Cu- and Au-mineralized granite porphyries in the Jinshajiang Cu-Au metallogenic belt, SW China: studies on the zircon chemistry. Mineral. Depos. 58, 1123-1142.

[4]

Blichert-Toft, J., 2008. The Hf isotopic composition of zircon reference material 91500. Chem. Geol. 253, 252-257.

[5]

Bureau of Geology and Mineral Resources of Heilongjiang Province, 2022. Regional Geology of China (Heilongjiang Volume). Geological Publishing House, Beijing (in Chinese).

[6]

Cai, K.D., Sun, M., Yuan, C., Zhao, G.C., Xiao, W.J., Long, X.P., Wu, F.Y., 2011. Geochronology, petrogenesis and tectonic significance of peraluminous granites from the Chinese Altai, NW China. Lithos 127, 261-281.

[7]

Cai, W.Y., Wang, Z.G., Li, J., Fu, L.J., Wang, K.Y., Konare, Y., 2019. Zircon U-Pb and molybdenite Re-Os geochronology and geochemistry of Jinchang porphyry gold-copper deposit, NE China: two-phase mineralization and the tectonic setting. Ore Geol. Rev. 107, 735-753.

[8]

Cao, M.J., Hollings, P., Evans, N.J., Cooke, D.R., McInnes, B.I.A., Zhao, K.D., Qin, K.Z., Li, D.F., Sweet, G., 2020. In situ elemental and Sr isotopic characteristics of magmatic to hydrothermal minerals from the Black Mountain porphyry deposit, Baguio District, Philippines. Econ. Geol. 115, 927-944.

[9]

Castillo, P.R., 2012. Adakites petrogenesis. Lithos 134 (135), 304-316.

[10]

Chen, J.L., Xu, J.F., Ren, J.B., Huang, X.X., Wang, B.D., 2014. Geochronology and geochemical characteristics of Late Triassic porphyritic rocks from the Zhongdian arc, eastern Tibet, and their tectonic and metallogenic implications. Gondwana Res. 26, 492-504.

[11]

Chen, J.P., Zhang, Y., Wang, J.X., Xiao, K.Y., Lou, D.B., Ding, J.H., Yin, J.N., Xiang, J., 2013. On present situation and potential analysis of copper resources in China. J. Geol. 37, 358-365.

[12]

Chiaradia, M., 2022. Distinct magma evolution processes control the formation of porphyry Cu-Au deposits in thin and thick arcs. Earth Planet. Sci. Lett. 599, 117864.

[13]

Chu, X.L., 2022. Mesozoic porphyry copper mineralization in the eastern continental margin of Jilin and Heilongjiang Province. Ph.D. thesis, Jilin University (in Chinese with English abstract).

[14]

Chung, S.L., Chu, M.F., Ji, J.Q., O’Reilly, S.Y., Pearson, N.J., Liu, D.Y., Lee, T.Y., Lo, C.H., 2009. The nature and timing of crustal thickening in Southern Tibet. Tectonophysics 477, 36-48.

[15]

Chung, S.L., Liu, D., Ji, J., Chu, M.F., Lee, H.Y., Wen, D.J., Lo, C.H., Lee, T.Y., Qian, Q., Zhang, Q., 2003. Adakites from continental collision zones: melting of thickened lower crust beneath southern Tibet. Geology 31, 1021-1024.

[16]

Cooke, D.R., Hollings, P., Walsh, J.L., 2005. Giant porphyry deposits: characteristics, distribution, tectonic controls. Econ. Geol. 100, 801-818.

[17]

Cooke, D.R., Hollings, P., Chang, Z., 2011. Philippine porphyry and epithermal deposits: an introduction. Econ. Geol. 106, 1253-1256.

[18]

Defant, M.J., Drummond, M.S., 1990. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature 347, 662-665.

[19]

Deng, C.Z., Fu, A.Z., Geng, H.Y., Sun, D.Y., Zhao, G.C., Mao, G.Z., Moynier, F., Lehmann, B., Yin, R.S., 2023. Low- d 18 O and negative- D 199 Hg felsic igneous rocks in NE China: implications for early Cretaceous orogenic thinning. Chem. Geol. 633, 121569.

[20]

Deng, C.Z., Sun, D.Y., Han, J.S., Chen, H.Y., Li, G.H., Xiao, B., Li, R.C., Feng, Y.Z., Li, C.L., Lu, S., 2019a. Late-stage southwards subduction of the Mongol-Okhotsk oceanic slab and implications for porphyry Cu-Mo mineralization: constraints from igneous rocks associated with the Fukeshan deposit, NE China. Lithos 326, 341-357.

[21]

Deng, C.Z., Sun, D.Y., Han, J.S., Li, G.H., Feng, Y.Z., Xiao, B., Li, R.C., Shi, H.L., Xu, G.Z., Yang, D.G., 2019b. Ages and petrogenesis of the Late Mesozoic igneous rocks associated with the Xiaokele porphyry Cu-Mo deposit, NE China and their geodynamic implications. Ore Geol. Rev. 107, 417-433.

[22]

Ding, J.S., Deng, C.Z., Feng, Y.Z., Yang, Y.B., Zhao, R.J., 2022. Contrasting tectonic regimes between Late Jurassic and early Cretaceous porphyry-epithermal Cu-Mo-Au mineralization in NE China: a perspective from the petrogenesis of the adakitic rocks in the Sishanlinchang porphyry Cu-Mo deposit. Ore Geol. Rev. 148, 105035.

[23]

Dokuz, A., Tanyolu, E., Genc, S., 2006. A mantle- and a lower crust-derived bimodal suite in the Yusufeli (Artvin) area, NE Turkey: trace element and REE evidence for subduction-related rift origin of Early Jurassic Demirkent intrusive complex. Int. J. Earth Sci. 95, 370-394.

[24]

Drummond, M.S., Defant, M.J., Kepezhinskas, P.K., 1996. Petrogenesis of slab-derived trondhjemite-tonalite-dacite/adakite magmas. Earth Environ. Sci. Trans. R. Soc. Edinb. 87 (1-2), 205-215.

[25]

Du, A.D., Wu, S.Q., Sun, D.Z., Wang, S.X., W.J., Markey, R., Stein, H., Morgan, J.W., Malinovskiy, D., 2004. Preparation and certification of Re-Os dating reference materials: molybdenite HLP and JDC. Geostand. Geoanal. Res. 28, 41-52.

[26]

Feng, Y.Z., Chen, H.Y., Xiao, B., Li, R.C., Deng, C.Z., Han, J.S., Li, G.H., Shi, H.L., Lai, C., 2020a. Late Mesozoic magmatism at Xiaokelehe Cu-Mo deposit in Great Xing’an Range, NE China: geodynamic and metallogenic implications. Lithos 374-375, 105713.

[27]

Feng, Y.Z., Chi, G.X., Deng, C.Z., Xiao, B., 2022. Ore-forming fluid evolution of a porphyry Cu-Mo deposit coexisting with porphyry Mo systems in a post-collisional setting, Xiaokelehe, NE China. Ore Geol. Rev. 149, 105061.

[28]

Feng, Y.Z., Deng, C.Z., Chen, H.Y., Li, G.H., Xiao, B., Li, R.C., Shi, H.L., 2020b. Re-Os Isotopic Dating of Sulfides from the Xiaokelehe Cu-Mo Deposit in the Northern Part of the Great Xing’an Range, NE China, and its Geological Implications. Geotecton. Metallog. 3, 465-475 (in Chinese with English abstract).

[29]

Gao, J., Klemd, R., Zhu, M.T., Wang, X.S., Li, J.L., Wan, B., Xiao, W.J., Zeng, Q.D., Shen, P., Sun, J.G., Qin, K.Z., Campos, E., 2018. Large-scale porphyry-type mineralization in the Central Asian metallogenic domain: a review. J. Asian Earth Sci. 165, 7-36.

[30]

Gao, Y.F., Hou, Z.Q., Kamber, B.S., Wei, R.H., Meng, X.J., Zhao, R.S., 2007. Adakite-like porphyries from the southern Tibetan continental collision zone: evidence from slab melt metamomorphism. Contrib. Mineral. Petrol. 153, 105-120.

[31]

Guo, J.F., Ma, Q., Xu, Y.G., Zheng, J.P., Zhou, Z.Y., Ma, L., Bai, X.J., 2022. Migration of Middle-Late Jurassic volcanism across the northern North China Craton in response to subduction of Paleo-Pacific Plate. Tectonophysics 833, 229338.

[32]

Hao, H.D., Park, J.W., Campbell, I.H., 2022. Role of magma differentiation depth in controlling the Au grade of giant porphyry deposits. Earth Planet. Sci. Lett. 593, 117640.

[33]

HIGS (Heilongjiang Institute of Geological Sciences), 2022. Regional Geology of China (Heilongjiang Volume). Geological Publishing House, Beijing (in Chinese with English abstract).

[34]

Hoskin, P.W.O., Black, L.P., 2000. Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon. J. Metamorph. Geol. 18, 423-439.

[35]

Hoskin, P.W.O., Schaltegger, U., 2003. The composition of zircon and igneous and metamorphic petrogenesis. Rev. Mineral. Geochem. 53, 27-62.

[36]

Hou, Z.Q., Gao, Y.F., Qu, X.M., Rui, Z.Y., Mo, X.X., 2004. Origin of adakitic intrusives generated during mid-Miocene east-west extension in southern Tibet. Earth Planet. Sci. Lett. 220, 139-155.

[37]

Hou, Z.Q., Pan, X., Li, Q., 2013. The giant Dexing porphyry Cu-Mo-Au deposit in east China: product of melting of juvenile lower crust in an intracontinental setting. Mineral. Depos. 48, 1019-1045.

[38]

Hou, Z.Q., Yang, Z.M., Lu, Y.J., Kemp, A., Zheng, Y.C., Li, Q.Y., Tang, J.X., Yang, Z.S., Duan, L.F., 2015. A genetic linkage between subduction- and collision-related porphyry Cu deposits in continental collision zones. Geology 43, 247-250.

[39]

Hou, Z.Q., Yang, Z.M., Qu, X.M., Meng, X.J., Li, Z.Q., Beaudoin, G., Rui, Z.Y., Gao, Y.F., Zaw, K., 2009. The Miocene Gangdese porphyry copper belt generated during post-collisional extension in the Tibetan Orogen. Ore Geol. Rev. 36, 25-51.

[40]

Huang, H., Wang, T., Guo, L., Tong, Y., He, Z.Y., Yin, J.Y., Wu, H.H., 2024. Crustal modification influenced by multiple convergent systems: insights from Mesozoic magmatism in northeastern China. Earth Sci. Rev. 252, 104737.

[41]

Hunen, J.V., Berg, A.P.V.D., Vlaar, N.J., 2002. On the role of subducting oceanic plateaus in the development of shallow flat subduction. Tectonophysics 352, 317-333.

[42]

Jahn, B.M., 2004. The central Asian orogenic belt and growth of the continental crust in the Phanerozoic. Geol. Soc. Lond. Spec. Publ. 226, 73-100.

[43]

Jahn, B.M., Wu, F.Y., Capdevila, R., Martineau, F., Zhao, Z.H., Wang, Y.X., 2001. Highly evolved juvenile granites with tetrad REE patterns: the Woduhe and Baerzhe granites from the Great Xing’an Mountains in north eastern China. Lithos 59, 171-198.

[44]

Ji, Z., Meng, Q.A., Wan, C.B., Zhu, D.F., Ge, W.C., Zhang, Y.L., Yang, H., Dong, Y., 2019. Geodynamic evolution of flat-slab subduction of Paleo-Pacific Plate: constraints from Jurassic adakitic lavas in the Hailar Basin, NE China. Tectonics 38, 4301-4319.

[45]

Jiang, Y., Jiang, S.H., Li, S.Z., Wang, G., Zhang, W., Lu, L.L., Guo, L.L., Liu, Y.J., Santosh, M., 2022. Paleozoic to Mesozoic micro-block tectonics in the eastern Central Asian Orogenic Belt: insights from magnetic and gravity anomalies. Gondwana Res. 102, 229-251.

[46]

Khain, E.V., Bibikova, E.V., Kröner, A., Zhuravlev, D.Z., Sklyarov, E.V., Fedotova, A.A., Kravchenko-Berezhnoy, I.R., 2002. The most ancient ophiolite of the Central Asian fold belt: U-Pb and Pb-Pb zircon ages for the Dunzhugur Complex, Eastern Sayan, Siberia, and geodynamic implications. Earth Planet. Sci. Lett. 199, 311-325.

[47]

Kiminami, K., Imaoka, T., 2013. Spatiotemporal variations of Jurassic-Cretaceous magmatism in eastern Asia (Tan-Lu fault to SW Japan): evidence for flat-slab subduction and slab rollback. Terra Nova 25, 414-422.

[48]

Lamont, T.N., Loader, M.A., Roberts, N.M.W., Cooper, F.J., Wilkinson, J.J., Bevan, D., Gorecki, A., Kemp, A., Elliott, T., Gardiner, N.J., Tapster, S., 2024. Porphyry copper formation driven by water-fluxed crustal melting during flat-slab subduction. Nat. Geosci. 17, 1306-1315.

[49]

Li, L.L., Shu, Q.H., Xing, K., Zhao, Z.H., Niu, X.D., 2021. Geochronology, geochemistry and Sr-Nd-Hf isotopes of the Heihuashan granite porphyry, NE China, and implications for Cu-Mo mineralization. Ore Geol. Rev. 139, 104435.

[50]

Li, P.Z., Yu, J.S., 1993. Nianzishan miarolitic alkaline granite stock, Heilongjiang—its ages and geological implications. Geochimica 4, 389-398 (in Chinese with English abstract).

[51]

Li, X.H., Tang, G.Q., Guo, B., Yang, Y.H., Hou, K.J., Hu, Z.C., Li, Q.L., Liu, Y., Li, W.X., 2013. Qinghu zircon: A working reference for microbeam analysis of U-Pb age and Hf and O isotopes. Chin. Sci. Bull. 58, 4647-4654.

[52]

Li, Y., Xu, W.L., Tang, J., Pei, F.P., Wang, F., Sun, C.Y., 2018. Geochronology and geochemistry of Mesozoic intrusive rocks in the Xing’an Massif of NE China: implications for the evolution and spatial extent of the Mongol-Okhotsk tectonic regime. Lithos 304-307, 57-73.

[53]

Liu, J.L., Li, Z.M., Zhou, Y.H., Dong, C.J., 2025. Geological setting, spatiotemporal distribution of predominant metal deposits in eastern section of China, Mongolia and Russia. Geol. China 52, 945-971.

[54]

Liu, S., Hu, R., Gao, S., Feng, C., Feng, G., Coulson, I.M., Li, C., Wang, T., Qi, Y., 2010a. Zircon U-Pb age and Sr-Nd-Hf isotope geochemistry of Permian granodiorite and associated gabbro in the Songliao Block, NE China and implications for growth of juvenile crust. Lithos 114, 423-436.

[55]

Liu, S.A., Li, S.G., He, Y.S., Huang, F., 2010b. Geochemical contrasts between early Cretaceous ore-bearing and ore-barren high-Mg adakites in central-eastern China: implications for petrogenesis and Cu-Au mineralization. Geochim. Cosmochim. Acta 74, 7160-7178.

[56]

Liu, Y., Sun, J.G., Wang, Q.H., Pan, Y.D., Xu, Z.K., Lei, F.Z., Li, X.P., Zhang, X.W., Liu, Y. M., 2021. Petrogenesis and oxygen fugacity of the Xintian complex associated with the Naozhi-Xintian porphyry epithermal system in the Yanbian area NE China. Ore Geol. Rev. 134, 104138.

[57]

Liu, Y.S., Hu, Z.C., Zong, K.Q., Gao, C.G., Gao, S., Xu, J., Chen, H.H., 2010c. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS. Chin. Sci. Bull. 55, 1535-1546.

[58]

Loucks, R.R., 2014. Distinctive composition of copper-ore-forming arc magmas. Aust. J. Earth Sci. 61, 5-16.

[59]

Loucks, R.R., 2021. Deep entrapment of buoyant magmas by orogenic tectonic stress: its role in producing continental crust, adakites, and porphyry copper deposits. Earth Sci. Rev. 220, 103744.

[60]

Loucks, R.R., Fiorentini, M.L., 2023a. Early zircon saturation in adakitic magmatic differentiation series and low Zr content of porphyry copper magmas. Mineral. Deposita 58, 1381-1393.

[61]

Loucks, R.R., Fiorentini, M.L., 2023b. Oxidation of magmas during gain and loss of H 2 O recorded by trace elements in zircon. Earth Planet. Sci. Lett. 622, 118377.

[62]

Loucks, R.R., Fiorentini, M.L., Henríquez, G.J., 2020. New magmatic oxybarometer using trace elements in zircon. J. Petrol. 61, egaa034.

[63]

Loucks, R.R., Henríquez, G.J., Fiorentini, M.L., 2024. Zircon and whole-rock trace element indicators of magmatic hydration state and oxidation state discriminate copper ore-forming from barren arc magmas. Econ. Geol. 119, 511-523.

[64]

Ludwig, K.R., 2012. User’s Manual for Isoplot Version 3.75-4.15: a Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, Special Publication 5, pp. 1-75.

[65]

Mafra, C., Loucks, R., Fiorentini, M., 2024. Distinctive source and hydration state of gold-ore-forming arc magmas. Geology 53, 195-200.

[66]

Maniar, P.D., Piccoli, P.M., 1989. Tectonic discrimination of granitoids. Geol. Soc. Am. Bull. 101, 635-643.

[67]

Mao, J.W., Cheng, Y.B., Chen, M.H., Pirajno, F., 2013. Major types and time-space distribution of Mesozoic ore deposits in South China and their geodynamic settings. Mineral. Depos. 48, 267-294.

[68]

Mao, J.W., Liu, P., Goldfarb, R.J., Goryachev, N.A., Pirajno, F., Zheng, W., Zhou, M.F., Zhao, C., Xie, G.Q., Yuan, S.D., Liu, M., 2021a. Cretaceous large-scale metal accumulation triggered by post-subductional large-scale extension, East Asia. Ore Geol. Rev. 136, 104270.

[69]

Mao, J.W., Zheng, W., Xie, G.Q., Lehmann, B., Goldfarb, R., 2021b. Recognition of a Middle-Late Jurassic arc-related porphyry copper belt along the southeast China coast: geological characteristics and metallogenic implications. Geology 49, 592-596.

[70]

Matjuschkin, V., Blundy, J.D., Brooker, R.A., 2016. The effect of pressure on sulphur speciation in mid- to deep-crustal arc magmas and implications for the formation of porphyry copper deposits. Contrib. Mineral. Petrol. 171, 66.

[71]

Martin, H., Smithies, R.H., Rapp, R., Moyen, J.F., Champion, D., 2005. An overview of adakite, tonalite-trondhjemite-granodiorite (TTG), and sanukitoid: relationships and some implications for crustal evolution. Lithos 79, 1-24.

[72]

Men, L.J., 2011. An ore-forming fluid study on Late Mesozoic epithermal Au-Cu deposits in Yanbian-Dongning area: implication for the metallogenic mechanism. Ph.D. thesis, Jilin University (in Chinese with English abstract).

[73]

Meng, Q.R., 2003. What drove late Mesozoic extension of the northern China-Mongolia tract? Tectonophysics 369, 155-174.

[74]

Middlemost, E.A.K., 1994. Naming materials in the magma/igneous rock system. Earth Sci. Rev. 37, 215-224.

[75]

Mihalasky, M.J., Ludington, S., Hammarstrom, J.M., Alexeiev, D.V., Frost, T.P., Light, T. D., Robinson, G.R., Briggs, D.A., Wallis, D., Miller, R.J., Bookstrom, A.A., Panteleyev, A., Chitalin, A., Seltmann, R., Yan, G.S., Lian, C.Y., Mao, J.W., Li, J.Y., Xiao, K.Y., Qiu, R.Z., Shao, J.B., Shai, G.Y., Du, Y.L., 2015. Porphyry copper assessment of the Central Asia orogenic belt and eastern Tethysides—China, Mongolia, Russia, Pakistan, Kazakhstan, Tajikistan, and India. In: Zientek M.L., Hammarstrom J.M., Johnson K.M., Pierce F.W. (Eds.),Global Mineral Resource Assessment. U.S. Geol. Surv, Reston, Virginia, p. 122.

[76]

Mungall, J.E., 2002. Roasting the mantle: slab melting and the genesis of major Au and Au-rich Cu deposits. Geology 30, 915-918.

[77]

Murakami, H., Seo, J.H., Heinrich, C., 2010. The relation between Cu/Au ratio and formation depth of porphyry-style Cu-Au ± Mo deposits. Mineral. Depos. 45, 11-21.

[78]

Park, J.W., Campbell, I.H., Chiaradia, M., Hao, H.D., Lee, C.T., 2021. Crustal magmatic controls on the formation of porphyry copper deposits. Nat. Rev. Earth Environ. 2, 542-557.

[79]

Peccerillo, A., Taylor, S.R., 1976. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey. Contrib. Mineral. Petrol. 58, 63-81.

[80]

Pei, F.P., Xu, W.L., Yang, D.B., Yu, Y., Meng, E., Zhao, Q.G., 2011. Petrogenesis of late Mesozoic granitoids in southern Jilin province, northeastern China: geochronological, geochemical, and Sr-Nd-Pb isotopic evidence. Lithos 125, 27-39.

[81]

Profeta, L., Ducea, M.N., Chapman, J.B., Paterson, S.R., Gonzales, S.M.H., Kirsch, M., Petrescu, L., DeCelles, P.G., 2015. Quantifying crustal thickness over time in magmatic arcs. Sci. Rep. 5, 17786.

[82]

Qi, L., Hu, J., Gregoire, D.C., 2000. Determination of trace elements in granites by inductively coupled plasma mass spectrometry. Talanta 51, 507-513.

[83]

Richards, J.P., 2003. Tectono-magmatic precursors for porphyry Cu-(Mo-Au) deposit formation. Econ. Geol. 98, 1515-1533.

[84]

Richards, J.P., 2009. Postsubduction porphyry Cu-Au and epithermal Au deposits: products of remelting of subduction-modified lithosphere. Geology 37, 247-250.

[85]

Richards, J.P., 2018. A shake-up in the porphyry world? Econ. Geol. 113, 1225-1233.

[86]

Richards, J.R., Kerrich, R., 2007. Adakite-like rocks: their diverse origins and questionable role in metallogenesis. Econ. Geol. 102, 537-576.

[87]

Seltmann, R., Porter, T.M., Pirajno, F., 2014. Geodynamics and metallogeny of the central Eurasian porphyry and related epithermal mineral systems: a review. J. Asian Earth Sci. 79, 810-841.

[88]

Shan, P.F., Cao, M.J., Evans, N.J., Gao, H.X., Mao, Y.J., Gao, Y.L., Salazar, L., Zhao, Y.S., Qin, K.Z., 2023. Automated quantitative mineralogy analysis reveals characteristics of Co occurrence in the Jinchang porphyry deposit, NE China. Ore Geol. Rev. 158, 105524.

[89]

Shan, P.F., Cao, M.J., Tang, D.M., Qiu, Z.J., Evans, N.J., Lazarov, M., Wang, D.C., Hu, W., Qin, K.Z., Horn, I., Weyer, S., 2025. Cobalt-rich porphyry deposits derived from multiple mafic magma injections. Geochim. Cosmochim. Acta 399, 125-143.

[90]

Shan, P.F., Cao, M.J., Evans, N.J., Hollings, P., Jourdan, F., Wang, L., Qin, K.Z., 2024. In-situ geochronology combined with geochemical and isotopic signatures record mineralization and fluid characteristics at the Xiaoxinancha porphyry Au-Cu deposit, NE China. Mineral. Depos. 59, 1703-1719.

[91]

Shen, P., Pan, H.D., Hattori, K., Cooke, D.R., Seitmuratova, E., 2018. Large Paleozoic and Mesozoic porphyry deposits in the Central Asian Orogenic Belt: geodynamic settings, magmatic sources, and genetic models. Gondwana Res. 58, 161-194.

[92]

Shen, S.Z., Zhang, H., Shang, Q.H., Li, W.Z., 2006. Permian stratigraphy and correlation of Northeast China: a review. J. Asian Earth Sci. 26, 304-326.

[93]

Shu, Q.H., Chang, Z.S., Lai, Y., Hu, X.L., Wu, H.Y., Zhang, Y., Wang, P., Zhai, D.G., Zhang, C., 2019. Zircon trace elements and magma fertility: Insights from porphyry (-skarn) Mo deposits in NE China. Mineral. Depos. 54, 645-656.

[94]

Shu, Q.H., Chang, Z.S., Lai, Y., Zhou, Y.T., Sun, Y., Yan, C., 2016. Regional metallogeny of Mo-bearing deposits in northeastern China, with new Re-Os dates of porphyry Mo deposits in the northern Xilamulun district. Econ. Geol. 111, 1783-1798.

[95]

Sillitoe, R.H., 2010. Porphyry copper systems. Econ. Geol. 105, 3-41.

[96]

Sláma, J., Kosler, J., Condon, D.J., Crowley, J.L., Gerdes, A., Hanchar, J.M., Horstwood, M.S.A., Morris, G.A., Nasdala, L., Norberg, N., Schaltegger, U., Schoene, B., Tubrett, M.N., Whitehouse, M.J., 2008. Plesovice zircon—a new natural reference material for U-Pb and Hf isotopic microanalysis. Chem. Geol. 249, 1-35.

[97]

Smoliar, M.I., Walker, R.J., Morgan, J.W., 1996. Re-Os ages of group IIA, IIIA, IVA and VIB iron meteorites. Science 271, 1099-1102.

[98]

Stein, H.J., Markey, R.J., Morgan, M.J., Du, A., Sun, Y., 1997. Highly precise and accurate Re-Os ages for molybdenite from the East Qinling molybdenum belt, Shaanxi Province, China. Econ. Geol. 92, 827-835.

[99]

Sun, D.Y., Gou, J., Wang, T.H., Ren, Y.S., Liu, Y.J., Guo, H.Y., Liu, X.M., Hu, Z.C., 2013a. Geochronological and geochemical constraints on the Erguna massif basement, NE China—subduction history of the Mongol-Okhotsk oceanic crust. Int. Geol. Rev. 55, 1801-1816.

[100]

Sun, J.G., Han, S.J., Zhang, Y., Xing, S.W., Bai, L.A., 2013b. Diagenesis and metallogenetic mechanisms of the Tuanjiegou gold deposit from the Lesser Xing’an Range, NE China: Zircon U-Pb geochronology and Lu-Hf isotopic constraints. J. Asian Earth Sci. 62, 373-388.

[101]

Sun, M.D., Chen, H.L., Zhang, F.Q., Wilde, S.A., Dong, C.W., Yang, S.F., 2013c. A 100 Ma bimodal composite dyke complex in the Jiamusi block, northeastern China: an indication for lithospheric extension driven by Paleo-Pacific roll-back. Lithos 162-163, 317-330.

[102]

Sun, S.S., Mcdonough, W.F., 1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. Geol. Soc. Lond. Spec. Publ. 42, 313-345.

[103]

Sun, W.D., Ding, X., Hu, Y.H., Li, X.H., 2007. The golden transformation of the Cretaceous plate subduction in the west Pacific. Earth Planet. Sci. Lett. 262, 533-542.

[104]

Sun, W.D., Ling, M.X., Yang, X.Y., Fan, W.M., Ding, X., Liang, H.Y., 2010. Ridge subduction and porphyry copper-gold mineralization: an overview. Sci. China Earth Sci. 53, 475-484.

[105]

Sun, W.D., Liu, L.J., Hu, Y.B., Ding, W., Liu, J.Q., Ling, M.X., Fan, W.M., 2018. Post-ridge-subduction acceleration of the Indian plate induced by slab rollback. Solid Earth Sci. 3, 1-7.

[106]

Sun, W.D., Zhang, H., Ling, M.X., Ding, X., Chung, S.L., Zhou, J.B., Yang, X.Y., Fan, W.M., 2011. The genetic association of adakites and Cu-Au ore deposits. Int. Geol. Rev. 53, 691-703.

[107]

Sun, Y.G., Ding, Q.F., Meng, F.B., Chen, X.S., Qian, Y., Wang, L., Wang, L.L., Xu, Q.L., 2022. Timing and ore formation of the Xiaokele porphyry Cu (-Mo) deposit in the northern Great Xing’an Range, NE China: constraints from geochronology, fluid inclusions, and H-O-S-Pb isotopes. Ore Geol. Rev. 143, 104806.

[108]

Sun, Y.G., Jin, H.Y., Wang, Y.S., Zhang, X.P., Wang, C.K., Li, H.J., 2024. Chemical characteristics of major sulfides in porphyry-type molybdenum (copper) deposits in the Northern Greater Khingan Mountains and their geological significance—a case study of 770 molybdenum (copper) deposit. Gold 45, 27-33.

[109]

Tafti, R., Lang, J.R., Mortensen, J.K., Oliver, J.L., Rebagliati, C.M., 2014. Geology and geochronology of the Xietongmen (Xiongcun) Cu-Au porphyry district, Southern Tibet, China. Econ. Geol. 109, 1967-2001.

[110]

Tafti, R., Mortensen, J.K., Lang, J.R., Rebagliati, M., Oliver, J.L., 2009. Jurassic U-Pb and Re-Os ages for the newly discovered Xietongmen Cu-Au porphyry district, Tibet, PRC: implications for metalogenic epochs in the southern Gangdese belt. Econ. Geol. 104, 127-136.

[111]

Thieblemont, D., Stein, G., Lescuyer, J.L., 1997. Epithermal and porphyry deposits: The adakite connection. C. R. Acad. Sci. Ser. IIA Earth Planet. Sci. 325, 103-109.

[112]

Wainwright, A.J., Tosdal, R.M., Wooden, J.L., Mazdab, F.K., Friedman, R.M., 2011. U-Pb (zircon) and geochemical constraints on the age, origin, and evolution of Paleozoic arc magmas in the Oyu Tolgoi porphyry Cu-Au district, southern Mongolia. Gondwana Res. 19, 764-787.

[113]

Wang, C.W., Sun, Y.W., Li, N., Zhao, G.W., Ma, X.Q., 2009. Tectonic implications of Late Paleozoic stratigraphic distribution in Northeast China and adjacent region. Sci. China Ser. D Earth Sci. 52, 619-626.

[114]

Wang, D.Z., Zhu, J.J., Hu, R.Z., Chiaradia, M., Bi, X.W., Huang, M.L., 2025. Optimal magmatic oxidation conditions for giant porphyry copper deposits. Sci. Bull. 70, 960-969.

[115]

Wang, Q., Wyman, D.A., Xu, J.F., Dong, Y.H., Vasconcelos, P.M., Pearson, N., Wan, Y.S., Dong, H., Li, C.F., Yu, Y.S., Zhu, T.X., Feng, X.T., Zhang, Q.Y., Zi, F., Chu, Z.Y., 2008. Eocene melting of subducting continental crust and early uplifting of central Tibet: evidence from central-western Qiangtang high-K calc-alkaline andesites, dacites and rhyolites. Earth Planet. Sci. Lett. 272, 158-171.

[116]

Wang, Q., Xu, J.F., Jian, P., Bao, Z.W., Zhao, Z.H., Li, C.F., Xiong, X.L., Ma, J.L., 2006. Petrogenesis of adakitic porphyries in an extensional tectonic setting, Dexing, South China: implications for the genesis of porphyry copper mineralization. J. Petrol. 47, 119-144.

[117]

Wang, R., Richards, J.P., Hou, Z.Q., Yang, Z.M., DuFrane, S.A., 2014a. Increased magmatic water content-the key to Oligo-Miocene porphyry Cu-Mo±Au formation in the eastern Gangdese belt. Tibet. Econ. Geol. 109, 1315-1339.

[118]

Wang, R., Richards, J.P., Hou, Z.Q., Yang, Z.M., Gou, Z.B., DuFrane, S.A., 2014b. Increasing magmatic oxidation state from Paleocene to Miocene in the eastern Tibetan Gangdese belt: implication for collision-related porphyry Cu-Mo±Au mineralization. Econ. Geol. 109, 1943-1965.

[119]

Wang, R., Zhu, D.Z., Wang, Q., Hou, Z.Q., Yang, Z.M., Zhao, Z.D., Mo, X.X., 2020. Porphyry mineralization in the Tethyan orogen. Sci. China Earth Sci. 63, 2042-2067.

[120]

Wang, S.S., Liu, J.Y., Ji, H.W., Lv, J., Zhou, S., Liu, J.L., 2017. Geochronology and geochemistry of the andesites of Longjiang Formation in the Sandaowanzi gold deposit, Heilongjiang Province. Acta Petrol. Sin. 33, 2604-2618 (in Chinese with English abstract).

[121]

Wang, T., Tong, Y., Xiao, W.J., Guo, L., Windley, B.F., Donskaya, T., Li, S., Narantsetseg, T., Zhang, J.J., 2022. Rollback, scissor-like closure of the Mongol- Okhotsk Ocean and formation of an orocline: magmatic migration based on a large archive of age data. Natl. Sci. Rev. 9, nwab210.

[122]

Wang, Y.H., Zhao, C.B., Zhang, F.F., Liu, J.J., Wang, J.P., Peng, R.M., Liu, B., 2015. SIMS zircon U-Pb and molybdenite Re-Os geochronology, Hf isotope, and whole-rock geochemistry of the Wunugetushan porphyry Cu -Mo deposit and granitoids in NE China and their geological significance. Gondwana Res. 28, 1228-1245.

[123]

Watanabe, Y., Stein, H.J., 2000. Re-Os ages for the Erdenet and Tsagaan Suvarga porphyry Cu-Mo deposits, Mongolia, and tectonic implications. Econ. Geol. 95, 1537-1542.

[124]

Weis, D., Kieffer, B., Maerschalk, C., Barling, J., Jong, J.D., Williams, G.A., Hanano, D., Pretorius, W., Mattieli, N., Scoates, J.S., Goolaerts, A., Friedman, R.M., Mahoney, J. B., 2013. High-precision isotopic characterization of USGS reference materials by TIMS and MC-ICP-MS. Geochem. Geophys. Geosyst. 7, 139-149.

[125]

Wilde, S.A., 2015. Final amalgamation of the Central Asian orogenic belt in NE China: Paleo-Asian Ocean closure versus Paleo-Pacific plate subduction—a review of the evidence. Tectonophysics 662, 345-362.

[126]

Wilkinson, J.J., 2013. Triggers for the formation of porphyry ore deposits in magmatic arcs. Nat. Geosci. 6, 917-925.

[127]

Woodhead, J.D., Hergt, J.M., 2005. Preliminary appraisal of seven natural zircon reference materials for in situ Hf isotope determination. Geostand. Geoanal. Res. 7, Q08006.

[128]

Wu, C., Chen, H.Y., Lu, Y.J., 2022. Crustal structure control on porphyry copper systems in accretionary orogens: insights from Nd isotopic mapping in the Central Asian Orogenic Belt. Mineral. Depos. 57, 631-641.

[129]

Wu, F.Y., Jahn, B.M., Wilde, S.A., Sun, D.Y., 2000. Phanerozoic continental crustal growth: U-Pb and Sr-Nd isotopic evidence from the granites in northeastern China. Tectonophysics 328, 89-113.

[130]

Wu, F.Y., Jahn, B.M., Wilde, S.A., Lo, C.H., Yui, T.F., Lin, Q., Ge, W.C., Sun, D.Y., 2003a. Highly fractionated I-type granites in NE China (I): geochronology and petrogenesis. Lithos 66, 241-273.

[131]

Wu, F.Y., Jahn, B.M., Wilde, S.A., Lo, C.H., Yui, T.F., Lin, Q., Ge, W.C., Sun, D.Y., 2003b. Highly fractionated I-type granites in NE China (II): isotopic geochemistry and implications for crustal growth in the Phanerozoic. Lithos 67, 191-204.

[132]

Wu, F.Y., Sun, D.Y., Ge, W.C., Zhang, Y.B., Grant, M.L., Wilde, S.A., Jahn, B.M., 2011. Geochronology of the Phanerozoic granitoids in northeastern China. J. Asian Earth Sci. 41, 1-30.

[133]

Wu, F.Y., Yang, J.H., Xu, Y.G., Wilde, S.A., Walker, R.J., 2019. Destruction of the North China Craton in the Mesozoic. Annu. Rev. Earth Planet. Sci. 47, 173-195.

[134]

Wu, M.Q., Samson, I.M., Qiu, K.F., Zhang, D.H., 2021. Concentration mechanisms of rare earth element-Nb-Zr-Be mineralization in the Baerzhe deposit, Northeast China: insights from textural and chemical features of amphibole and rare metal minerals. Econ. Geol. 116, 651-679.

[135]

Xiao, L., Clemens, J.D., 2007. Origin of potassic (C-type) adakite magmas: experimental and field constraints. Lithos 95, 399-414.

[136]

Xiao, W.J., Huang, B.C., Han, C.M., Sun, S., Li, J.L., 2010. A review of the western part of the Altaids: a key to understanding the architecture of accretionary orogens. Gondwana Res. 18, 253-273.

[137]

Xu, W.C., Zhang, H.F., Guo, L., Yuan, H.L., 2010. Miocene high Sr/Y magmatism, south Tibet: product of partial melting of subducted Indian continental crust and its tectonic implication. Lithos 114, 293-306.

[138]

Xu, W.L., Pei, F.P., Wang, F., Meng, E., Ji, W.Q., Yang, D.B., Wang, W., 2013. Spatial-temporal relationships of Mesozoic volcanic rocks in NE China: constraints on tectonic overprinting and transformations between multiple tectonic regimes. J. Asian Earth Sci. 74, 167-193.

[139]

Yang, J.H., Wu, F.Y., Shao, J.A., Wilde, S.A., Xie, L.W., Liu, X.M., 2006. Constrains on the timing of Uplift of the Yanshan Fold and Thrust Belt, North China. Earth Planet. Sci. Lett. 246, 336-352.

[140]

Yang, J.H., Xu, L., Sun, J.F., Zeng, Q., Zhao, Y.N., Wang, H., Zhu, Y.S., 2021. Geodynamics of decratonization and related magmatism and mineralization in the North China Craton. Sci. China Earth Sci. 64, 1409-1427.

[141]

Yang, Z.M., Cao, K., 2024. Post-collisional porphyry copper deposits in Tibet: An overview. Earth Sci. Rev. 258, 104954.

[142]

Yang, Z.M., Cooke, D.R., 2019. Porphyry copper deposits in China. Econ. Geol. 22, 133-187.

[143]

Yang, Z.M., Goldfarb, R., Chang, Z.S., 2016. Generation of post-collisional porphyry copper deposits in southern Tibet triggered by subduction of the Indian continental plate. Soc. Econ. Geol. Spec. Publ. 19, 279-300.

[144]

Yuan, C., Sun, M., Wilde, S., Xiao, W.J., Xu, Y.G., Long, X.P., Zhao, G.C., 2010. Post-collisional plutons in the Balikun area, East Chinese Tianshan: evolving magmatism in response to extension and slab break-off. Lithos 119, 269-288.

[145]

Zeng, Q.D., Wang, Y.B., Yang, J.H., Guo, Y.P., Yu, B., Zhou, L.L., Qiu, H.C., 2020. Spatial-temporal distribution and tectonic setting of gold deposits in the northern margin gold belt of the North China Craton. Int. Geol. Rev. 63, 941-972.

[146]

Zhai, D.G., Liu, J.J., Ripley, E.M., Wang, J.P., 2015. Geochronological and He-Ar-S isotopic constraints on the origin of the Sandaowanzi gold-telluride deposit, northeastern China. Lithos 212, 338-352.

[147]

Zhai, D.G., Williams-Jones, A.E., Liu, J.J., Tombros, S.F., Cook, N.J., 2018. Mineralogical, fluid inclusion, and multiple isotope (H-O-S-Pb) constraints on the genesis of the Sandaowanzi epithermal Au-Ag-Te deposit, NE China. Econ. Geol. 113, 1359-1382.

[148]

Zhai, M.G., Zhou, Y.Y., 2015. General Precambrian Geology in China. In: Zhai M.G. (Ed.), Precambrian Geology of China. Springer, Berlin Heidelberg, pp. 3-56.

[149]

Zhang, P., Huang, X.W., Cui, B., Wang, B.C., Yin, Y.F., Wang, J.R., 2016. Re-Os isotopic and trace element compositions of pyrite and origin of the Cretaceous Jinchang porphyry Cu- Au deposit, Heilongjiang Province, NE China. J. Asian Earth Sci. 129, 67-80.

[150]

Zhang, X.H., Li, T.S., Pu, Z.P., 2002a. 40 Ar- 39 Ar thermochronology of two ductile shear zones from Yiwulüshan, West Liaoning region: age constraints on the Mesozoic tectonic events. Chin. Sci. Bull. 47, 1113-1118.

[151]

Zhang, X.H., Li, T.S., Pu, Z.P., Wang, H., 2002b. 40 Ar- 39 Ar ages of the Louzidian-Dachengzi ductile shear zone near Chifeng, Inner Mongolia and their tectonic significance. Chin. Sci. Bull. 47, 1292-1297.

[152]

Zhao, P., Xu, B., Chen, Y., 2023. Evolution and final closure of the Mongol-Okhotsk Ocean. Sci. China Earth Sci. 66, 2497-2513.

[153]

Zhu, J.J., Richards, J.P., Rees, C., Creaser, R., DuFrane, S.A., Locock, A., Petrus, J.A., Lang, J., 2018. Elevated magmatic sulfur and chlorine contents in ore-forming magmas at the Red Chris porphyry Cu-Au deposit, northern British Columbia, Canada. Econ. Geol. 113, 1047-1075.

PDF

4

Accesses

0

Citation

Detail

Sections
Recommended

/