 | Xu, Xing-Wang, Zhang, Bao-Lin, Qin, Ke-Zhang, Mao, Qian, Cai, Xin-Ping (2007) Origin of lamprophyres by the mixing of basic and alkaline melts in magma chamber in Beiya area, western Yunnan, China. Lithos, 99 (3) 339-362 doi:10.1016/j.lithos.2007.06.011 | Journal (article/letter/editorial) | | alkaline melts in magma chamber in Beiya area, western Yunnan, China Xing-Wang Xu ⁎, Bao-Lin Zhang, Ke-Zhang...Chinese Academy of Sciences, Beijing 100029, PR China Received 10 October 2006; accepted 15 June 2007...formed in the early Tertiary around 60 Ma in the Beiya area and are characterized by low SiO2 ± 46–50 wt...melts, (7) the occurrence of olivine, high-MgO ilmenite and spinel inclusions within earlier formed diopside...porphyries in the Beiya area and the western Yunnan and Tertiary basalt in the western Yunnan indicate that |  | Fu, Yu, Sun, Xiaoming, Zhou, Haoyang, Lin, Hai, Yang, Tianjian (2016) In-situ LA–ICP–MS U–Pb geochronology and trace elements analysis of polygenetic titanite from the giant Beiya gold–polymetallic deposit in Yunnan Province, Southwest China. Ore Geology Reviews, 77. 43-56 doi:10.1016/j.oregeorev.2016.02.001 | Journal (article/letter/editorial) | | titanite from the giant Beiya gold–polymetallic deposit in Yunnan Province, Southwest China Yu Fu, Xiaoming Sun...titanite from the giant Beiya gold–polymetallic deposit in Yunnan Province, Southwest China, Ore Geology Reviews...from the giant Beiya gold–polymetallic IP T deposit in Yunnan Province, Southwest China SC R Yu Fu...Sciences, Sun Yat-sen University, Guangzhou 510006, China NU b. Guangdong Provincial Key Laboratory of Marine...Resources and Coastal Engineering, Guangzhou 510275, China MA c. School of Earth Science and Geological Engineering |  | Meng, Xuyang, Mao, Jingwen, Zhang, Changqing, Zhang, Dongyang, Liu, Huan (2018) Melt recharge, f O2-T conditions, and metal fertility of felsic magmas: zircon trace element chemistry of Cu-Au porphyries in the Sanjiang orogenic belt, southwest China. Mineralium Deposita, 53 (5) 649-663 doi:10.1007/s00126-017-0768-y | Journal (article/letter/editorial) | | porphyries in the Sanjiang orogenic belt, southwest China Xuyang Meng 1 & Jingwen Mao 2 & Changqing Zhang...hydrothermal Pulang Cu deposit (Triassic) and the Beiya Au-Cu deposits (Eocene) are located in the Sanjiang...Sanjiang copper porphyry belt, southwest China. Zircon chemistry was used to constrain the magmatic evolution...porphyries. The results show that porphyries of the Beiya district formed from an early oxidized melt and...average temperature of 709 ± 6 °C compared to the Beiya porphyries (ΔFMQ + 0.6–3.5, average = 1.9 ± 1.3 |  | | Journal (article/letter/editorial) | | significance of the Eocene adakite-like rocks in western Yunnan, southeastern Tibetan Plateau Huixia Ding a,⁎,...Sciences, Beijing 100037, PR China School of Earth Science and Resources, China University of Geosciences...Geosciences, Beijing 100083, PR China a r t i c l e i n f o Article history: Received 12 March 2015 Accepted...Juvenile lower crust Collisional orogeny Western Yunnan Southeastern Tibet a b s t r a c t Eocene magmatic...magmatic rocks are widespread in western Yunnan, southeastern Tibetan Plateau. However, their petrogenesis |  | Zhu, J.-j., Hu, R., Richards, J. P., Bi, X., Zhong, H. (2015) Genesis and Magmatic-Hydrothermal Evolution of the Yangla Skarn Cu Deposit, Southwest China. Economic Geology, 110 (3) 631-652 doi:10.2113/econgeo.110.3.631 | Journal (article/letter/editorial) | | Evolution of the Yangla Skarn Cu Deposit, Southwest China Jing-jing Zhu,1,2,† Ruizhong Hu,1,† Jeremy P. Richards...Chinese Academy of Sciences, Guiyang 550002, PR China 2 Department of Earth and Atmospheric Sciences...within the Sanjiang (Three Rivers) region, southwest China. Skarn orebodies are mainly developed between different... and 208Pb/204Pb = 38.367–38.942) in the mining area. Taken together, these geologic, geochemical, and...one of the most important polymetallic belts in China, hosting numerous ore deposits, including several |  | | Journal (article/letter/editorial) | | elements in the Lala Fe-Cu-(Mo, REE) deposit, SW China—Wei Terry Chen and Mei-Fu Zhou 671 Noble gases...cassiterite vein type mineralization of the Kalima area (Maniema, Democratic Republic of Congo)— S. Dewaele...Tongkuangyu Cu deposit (Palaeoproterozoic), North China craton—Xuan Liu, Hong-Rui Fan, M. Santosh, Kui-Feng...mineralization in stream sediment samples in Gharachaman area, northwest of Iran— Abbas Darehshiri, Maryam Panji...origin of the Banbanqiao Zn-Pb deposit, southwest China—Bo Li, Jia-Xi Zhou, Zhi-Long Huang, Zai-Fei Yan |  | | Book | | Special Issue Editor Liqiang Yang China University of Geosciences China Editorial Office MDPI St. Alban-Anlage...and Metallogenesis in Liaodong Peninsula, North China Craton: Insights from Zircon Hf-Nd Isotope Mapping...Sanshandao Gold Deposit, Jiaodong Peninsula, Eastern China Reprinted from: Minerals 2019, 9, 189, doi:10.3390/min9030189...Sizhuang Orogenic Gold Deposit, Jiaodong Peninsula, China Reprinted from: Minerals 2019, 9, 190, doi:10.3390/min9030190...the Jinqingding Gold Deposit, Jiaodong Peninsula, China: Implications for the Gold Precipitation Mechanism |  | Elitok, Ömer, Özgür, Nevzat, Drüppel, Kirsten, Dilek, Yildirim, Platevoet, Bernard, Guillou, Hervé, Poisson, Andre, Scaillet, Stéphane, Satır, Muharrem, Siebel, Wolfgang, Bardintzeff, Jacques-Marie, Deniel, Catherine, Yılmaz, Kamil (2010) Origin and geodynamic evolution of late Cenozoic potassium-rich volcanism in the Isparta area, southwestern Turkey. International Geology Review, 52 (4) 454-504 doi:10.1080/00206810902951411 | Journal (article/letter/editorial) | | Cenozoic potassium-rich volcanism in the Isparta area, southwestern Turkey a b c Ömer Elitok , Nevzat...Cenozoic potassium-rich volcanism in the Isparta area, southwestern Turkey, International Geology Review...Cenozoic potassium-rich volcanism in the Isparta area, southwestern Turkey Ömer Elitoka*, Nevzat Özgürb...potassic-rich volcanism of Gölcük Volcano in the Isparta area of southwestern Turkey consists of two groups: (i)...Antalya nappes in the north (Figure 2). The study area is covered by authochtonous and allochthonous units |
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