Titlebook: Metallogenic Mechanism of the Galinge Polymetallic Iron Skarn Deposit, Qiman Tagh Mountains, Qinghai; Miao Yu Book 2019 Springer Nature Si

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Miao Yuging the brutal past. The collection fills a critical gap in both literary studies, which has largely ignored the issue of race and utopia, and utopian studies, which has said too little about race.978-3-030-19472-7978-3-030-19470-3

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The Qiman Tagh Orogen as a Window to the Crustal Evolution in Northern Qinghai-Tibet Plateau,llision of a collage of terranes during subduction and closure of the Qiman Tagh Ocean, a branch of Paleo-Tethys Ocean from the Neoproterozoic to Early Mesozoic. The orogen is located between the Qaidam Basin and Kumukuri Basin, and cut by the Altun Fault to the west. The early Neoproterozoic (ca. 1

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Thermodynamic Model for the Galinge Fe Skarn Deposit in Qinghai,etite and base-metal sulfide orebodies, and is hosted in dolomitic limestone. It experienced a complete skarn and retrograde stage under varying fluid compositions resulting in thermodynamically controlled formation of magnesian skarn and mineralogical zonation. A series of Mg- and Ca-rich solid sol

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Multistage Skarn-Related Tourmalines from the Galinge Deposit: A Significant Indicator for Varying fluid-rock interactions. It is divided into six ore domains from east to the west. Skarn-related tourmaline is ubiquitous in the V ore domain of the Galinge deposit, occurring both in the altered basaltic andesite (Tour-I) and in the sandstone (Tour-II). The tourmaline composition in both rock type

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Multistage Amphiboles from the Galinge Skarn Deposit: Evidence of Igneous Rocks Replacement,formed by multistage fluid-rock interactions. Mineral analysis of the various amphiboles suggest that they were formed by the replacement of mafic to intermediate igneous rocks. The two alteration phases have formed three generations of compositionally distinct amphiboles: Amp-I: Ferro-edenitic horn

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Formation and Breakdown of Ilvaite in the Large Galinge Skarn Fe Deposit, Western China: A Record ooped Ca-rich retrograde alteration. The ilvaite-bearing skarn associations were studied to determine their physicochemical formation conditions. Petrographic evidence for replacement of garnet and magnetite by ilvaite in the early retrograde stage (Stage I) combined with thermodynamic modeling sugge

Commentary

Fluid Evolution and Stable Isotope Characters,rature and salinity shifts between skarn- and retrograde alteration stage. In the skarn stage of the Galinge deposit, ascending SiO.-bearing NaCl saturated magmatic fluids separated to a hypersaline liquid and a vapor phase at 500~550°C and 300~400bar 1~1.5km paleodepth, at higher lithostatic pressu

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