Fluid Inclusion and H–O–S–Pb Isotope Geochemistry of the Yuka Orogenic Gold Deposit, Northern Qaidam, China by Pengjie Cai, Rongke Xu, Youye Zheng, Yueming Yin, Xin Chen, Xianbin Fan, Chao Ma

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Geofluids Assessment of the Ayub and Shafa Hot Springs in Kopet-Dagh Zone (NE Iran): An Isotopic Geochemistry Approach by Hossein Mohammadzadeh, Majid Kazemi

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Sulfur partitioning between aqueous fluids and felsic melts at high pressures: Implications for sulfur migration in subduction zones by Lanqin Li, Xingcheng Liu, Ting Xu, Xiaolin Xiong, Jintuan Wang, Li Li

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Fluids, Metals, and Mineral/Ore Deposits by Xing Ding, Daniel E. Harlov, Bin Chen, Weidong Sun

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An Areal Assessment of Subseafloor Carbon Cycling in Cold Seeps and Hydrate-Bearing Areas in the Northern South China Sea by Yanping Zhang, Min Luo, Yu Hu, Hongbin Wang, Duofu Chen

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High-temperature structural disorders stabilize hydrous aluminosilicates in the mantle transition zone by Baoyun Wang, Jin Liu, Yanyao Zhang, Baisheng Nie, Wei Yang, Jialong Hao, Xing Ding, Yongjun Tian

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Petrogenetic evidences in geodynamics and placement of Nordoz intrusive masses in Alborz-Azerbaijan structural zone by Shahryar Mahmoudi, Shiva Lavi, Shohreh Hassanpour, Amir Ali Tabakh Shabani, Mehran Yegane Far

“…The presence of disequilibrium textures, such as sieve texture and zoning in plagioclase, suggests the existence of multiple magma chambers and mixing between them. The isotopic geochemistry indicates that a closed system process and crystal differentiation are the primary processes of formation, with a combination of DMM and EMII identified as the principal sources for magmas in the region. …”
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