How did the Orogenic Gold Deposits Form?
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[1] Goldfarb, R. J., Baker, T., Dubé, B., et al., 2005. Distribution, Character, and Genesis of Gold Deposits in Metamorphic Terran. One Hundredth Anniversary Volume, 407-450. [2] Goldfarb, R. J., Qiu, K. F., Deng, J., et al., 2019. Orogenic Gold Deposits of China. SEG Special Publication, 22: 263-324. [3] Goldfarb, R. J., Groves, D. I., 2015. Orogenic Gold: Common or Evolving Fluid and Metal Sources through Time. Lithos, 233: 2–26. doi: 10.1016/j.lithos.2015.07.011 [4] Groves, D. I., Goldfarb, R. J., Gebre-Mariam, M., et al., 1998. Orogenic Gold Deposits: a Proposed Classification in the Context of Their Crustal Distribution and Relationship to other Gold Deposit Types. Ore Geology Reviews, 13(1): 7-27. [5] Groves, D. I., Santosh, M., Deng, J., et al., 2020. A Holistic Model for the Origin of Orogenic Gold Deposits and Its Implications for Exploration. Mineralium Deposita, 55(2): 275-292. https://doi.org/10.1007/s00126-019-00877-5 [6] Kerrich, R., Goldfarb, R., Groves, D., et al., 2000. The Characteristics, Origins, and Geodynamic Settings of Supergiant Gold Metallogenic Provinces. Science in China Series D: Earth Sciences, 43(1): 1-68. https://doi.org/10.1007/BF02911933 [7] McLeish, D. F., Williams-Jones, A. E., Vasyukova, O. V., et al., 2021. Colloidal Transport and Flocculation are the Cause of the Hyperenrichment of Gold in Nature. Proceedings of the National Academy of Sciences of the United States of America, 118(20): e2100689118. https://doi.org/10.1073/pnas.2100689118 [8] Phillips, G. N., Powell, R., 2009. Formation of Gold Deposits: Review and Evaluation of the Continuum Model. Earth-Science Reviews, 94(1-4): 1-21. https://doi.org/10.1016/j.earscirev.2009.02.002 [9] Weatherley, D. K., Henley, R. W., 2013. Flash Vaporization during Earthquakes Evidenced by Gold Deposits. Nature Geoscience, 6(4): 294-298. https://doi.org/10.1038/ngeo1759 [10] 翟裕生, 王建平, 2011. 矿床学研究的历史观. 地质学报, 85(5): 603-611. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201105003.htm [11] 蒋少涌, 戴宝章, 姜耀辉, 等, 2009. 胶东和小秦岭: 两类不同构造环境中的造山型金矿省. 岩石学报, 25(11): 2727-2738. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200911004.htm [12] 毛景文, 赫英, 丁悌平, 2002. 胶东金矿形成期间地幔流体参与成矿过程的碳氧氢同位素证据. 矿床地质, 21(2): 121-128. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200202003.htm
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