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Metallogenic Mechanism of the Galinge Polymetallic Iron Skarn Deposit, Qiman Tagh Mountains, Qinghai Province

Part of the Springer Theses Book Series

DOI: 10.1007/978-981-10-7907-8

ISBN: 978-981-10-7906-1

Publisher: Springer Singapore - Springer Journals

Feb 16, 2019

1 - 10 of 10 Chapters

LitStream

Chapter 1The Qiman Tagh Orogen as a Window to the Crustal Evolution in Northern Qinghai-Tibet Plateau

Yu, Miao

Pages: 1 –41

[The Qiman Tagh Orogenic Belt (QTOB), located along the northern part of the Qinghai-Tibet plateau, was constructed through protracted accretion and collision of a collage of terranes during subduction and closure of the Qiman Tagh Ocean, a branch of Paleo-Tethys Ocean from the Neoproterozoic to...
LitStream

Chapter 2Skarn Zonation and Mineral Geochemistry of the Galinge Skarn Deposit

Yu, Miao

Pages: 43 –99

[The Galinge deposit can be roughly divided into three proximal to distal skarn zones Based on the mineral assemblages and their compositions; i.e. the magnesian skarn (Mg-SK), the calcic skarn (Ca-SK) and the manganese-calcium skarn (Mn-Ca-SK) zones. The Mg-SK is developed in the II ore domain,...
LitStream

Chapter 3Thermodynamic Model for the Galinge Fe Skarn Deposit in Qinghai

Yu, Miao

Pages: 101 –115

[The Galinge iron deposit in the Qiman Tagh orogen, western part of the East Kunlun, Qinghai province, occurs as lens-shaped magnesian skarn, with magnetite and base-metal sulfide orebodies, and is hosted in dolomitic limestone. It experienced a complete skarn and retrograde stage under varying...
LitStream

Chapter 4Multistage Skarn-Related Tourmalines from the Galinge Deposit: A Significant Indicator for Varying Fluid Composition

Yu, Miao

Pages: 117 –138

[The Galinge skarn deposit, the largest iron polymetallic skarn deposit in the Qiman Tagh metallogenic belt (western China), was formed via multi-stage 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...
LitStream

Chapter 5Multistage Amphiboles from the Galinge Skarn Deposit: Evidence of Igneous Rocks Replacement

Yu, Miao

Pages: 139 –156

[Amphiboles from the Galinge skarn deposit, the largest iron (Fe) polymetallic skarn deposit in the Qiman Tagh metallogenic belt (western China), were formed by multistage fluid-rock interactions. Mineral analysis of the various amphiboles suggest that they were formed by the replacement of mafic...
LitStream

Chapter 6Formation and Breakdown of Ilvaite in the Large Galinge Skarn Fe Deposit, Western China: A Record of Multistage Retrograde Alteration

Yu, Miao

Pages: 157 –175

[The Galinge deposit, the largest Fe skarn deposit in the Qiman Tagh porphyry-skarn metallogenic belt (western China), is noteworthy for its well-developed Ca-rich retrograde alteration. The ilvaite-bearing skarn associations were studied to determine their physicochemical formation conditions....
LitStream

Chapter 7Fluid Evolution and Stable Isotope Characters

Yu, Miao

Pages: 177 –187

[Fluid inclusions are particularly useful in documenting the temporal and spatial evolution of skarn-forming fluids, and provide evidence for the temperature and salinity shifts between skarn- and retrograde alteration stage. In the skarn stage of the Galinge deposit, ascending SiO2-bearing NaCl...
LitStream

Chapter 8Geochronological and Geochemical Constraints on the Galinge Skarn Deposit

Yu, Miao

Pages: 189 –211

[ Galinge, the largest iron (Fe) polymetallic skarn deposit in the Qinghai province (NW China), is located in the Qiman Tagh metallogenic belt. At Galinge, post-collisional calc-alkaline metaluminous intrusions, including granodiorite, diorite and diorite porphyry dikes were emplaced into the...
LitStream

Chapter 9Genesis of Post-collisional Calc-Alkaline and Alkaline Granitoids in Qiman Tagh

Yu, Miao

Pages: 213 –234

[The post-collisional magmatism of Qiman Tagh is characterized by the intrusion of voluminous intermediate to felsic granitoids, including syenogranite, monzogranite, granodiorite, tonalite and diorite. The granitoids can be divided into two magmatic suites: Calc-alkaline (CA) and alkaline (Alk),...
LitStream

Chapter 10Metallogenic Mechanism of the Galinge Polymetallic Iron Skarn Deposit, Qiman Tagh Mountains, Qinghai Province

Yu, Miao

Pages: 235 –248

[In the Qiman Tagh metallogenic belt, Fe, Zn, Pb, Cu and Au skarns and epithermal Cu and Mo deposits are spatially and temporally associated with Triassic granitoid rocks including granodiorite, monzogranite and syenogranite which are only occurred in the South Qiman Tagh Terrane as a result of...

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