FAHLORES FROM PORPHYRY Cu-(Mo) DEPOSITS OF THE URALS by O.Yu. Plotinskaya, E.V. Kovalchuk

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Fluid Inclusion and Oxygen Isotope Constraints on the Origin and Hydrothermal Evolution of the Haisugou Porphyry Mo Deposit in the Northern Xilamulun District, NE China by Qihai Shu, Yong Lai

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The Metallogeny of the Tieling Cu-Mo Porphyry Deposit in Eastern Tianshan, NW China: New Insights from Zircon U-Pb, Fluid Inclusion, and H-O-S Stable Isotope Analyses by Ping Li, Ting Liang, Fan Huang, Tongyang Zhao, Zhixin Zhu, Yong Li, Jing Feng, Lei He

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Geological, alteration, mineralogy and geochemical studies of the Copper deposit in the Kalatehno prospect area, northwest of Gonabad (Khorasan Razavi province) by Sedigheh Zirjanizadeh, Roohollah Miri Bydokhti

“…The Kalatehno prospecting area is located at 23 Km northwest of Gonabad, Khorasan Razavi province, and north of the Lut Block. The geology of the area includes subvolcanic units with monzonite, monzodiorite and diorite porphyry, volcanic units, pyroclastic and Quaternary units. …”
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A «necklace» of large clusters of strategic raw materials over a stagnant oceanic slab in East Asia by Natalia Boriskina

“…An analysis of geological-geophysical, metallogenic, geochronological, and seismic tomographic studies in territories joining Southeast Russia, East Mongolia, and Northeast China led to the conclusion that deep geodynamics significantly influenced the formation of highly productive ore-magmatic systems in the Late Jurassic-Early Cretaceous. …”
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Mineralogy, alteration, fluid inclusions microthermometry and genesis of the Cu-Au Kalateh Dasht deposit, south of Shahrood, NE Iran by Mohadeseh Eskandari, Fardin Mousivand, Maryam Sheibi, Bernd Lehmann

“…In close proximity to this ore deposit, an argillic alteration zone and other mineralization systems in this region increase the likelihood of a porphyry system at greater depth. Introduction Despite the abundance of mineralization in the Toroud-Chah Shirin magmatic arc (TCSMA), certain deposits, such as the polymetallic Kalateh Dasht deposit with its post Eocene diorite porphyry host rock, have not yet been thoroughly investigated in terms of their geology, mineralogy, and genesis. …”
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Whole-rock geochemistry and crystal chemistry of apatite at intrusive suites of the Qeynarjeh-Angouran district (west of Zanjan): an approach to the identification of skarn-causati... by Afsoon Dastour, Ebrahim Tale Fazel, Ashraf Torkian

“…The Qeynarjeh granodiorite is an ore-bearing granite and shows evidence of a skarn-causative suite (non-porphyry). …”
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Alteration, mineralization, geochemistry and fluid inclusion investigations in Joftrud prospect area, southwest of Birjand by Omid Shareipour, Azadeh Malekzadeh Shafaroudi, Maryam Javidi Moghaddam

“…Extensive magmatic activity in the Lut Block, is accompanied with numerous mineralization events such as porphyry copper, IOCG, vein and skarn (Karimpour et al., 2012). …”
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Petrology of Oligocene Lalehzar igneous rocks in the southeast of Saveh-Naein-Jiroft magmatic belt by Fatemeh Sepidbar, Bahareh Borouzi Niyat

“…Major oxides and trace/minor elements were analyzed by XRF and PQ2 Turbo ICP-MS methods at Institute of Geology and Geophysics, Chinese Academy of Sciences (IGGCAS) in Beijing. …”
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Geodynamics of basins above subducted slabs: An integrated modelling study of tectonics, sedimentation, and magmatism in the Timok Magmatic Complex by Stojadinović Uroš, Toljić Marinko, Trivić Branislav, Pantović Radoje, Srećković-Batoćanin Danica, Krstekanić Nemanja, Kostić Bojan, Velojić Miloš, Stefanović Jelena, Ranđelović Nikola, Maleš Maja

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Fluid Inclusions and C-H-O-S-Pb Isotope Systematics of the Changfagou Deposit, Jilin Province, Northeast China by Bo Peng, Bile Li, Jun Chen

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The gold content of mafic to felsic potassic magmas by Jia Chang, Andreas Audétat, Thomas Pettke

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A New Density Model of Quartz Solubility in H2O-CO2-NaCl Ternary Systems up to High Temperatures and High Pressures by Weiping Deng, Qing Wei, Xuan Liu

“…In addition, a bisection algorithm for deriving the isopleths of quartz solubilities based on this new model is first proposed, and application perspectives are discussed for various geologic settings including subduction zone, lower crust-upper mantle, migmatite, pegmatite, porphyry, and orogenic deposits.…”
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