Titlebook: Geology and Geochemistry of Molybdenum Deposits in the Qinling Orogen, P R China; YanJing Chen,Franco Pirajno,YongFei Yang Book 2022 The E

喃喃而言

,Porphyry–Skarn Mo Systems, small-sized Qiushuwan Mo–Cu deposit hosted in the Qinling Group marbles. The mineralization process commonly includes four stages: (1) skarnization and hornfelsing, associated with scheelite and magnetite; (2) stockworks of quartz?+?molybdenite?±?other sulfides; (3) stockworks of quartz?+?polymetal

Prophylaxis

Magmatic-Hydrothermal Vein Systems,ugh purple fluorite-molybdenite-pyrite and sulfide-calcite veins, to late carbonate ones. The 0.85-Ga mineralization is synchronous with a syenite event. They are a prelude of the Rodinia supercontinent breakup occurring in the postcollisional extension setting..The Triassic Huanglongpu carbonatite

Dorsal-Kyphosis

柱廊

Mineralization and Its Controls,orphyry Cu deposits; and so do the Yanshanian PMDs relative to the pre-Yanshanian. The pure carbonic, carbonic-aqueous, and daughter mineral-bearing carbonic-aqueous inclusions are present in PMDs in continental rifts or collision belts, but absent in continental arcs, indicating that they result fr

vasospasm

Book 2022mal class includes porphyries, skarns, and intrusion-related veins (carbonatite, fluorite and quartz). The porphyry Mo systems in Qinling Orogen are predominated by Dabie-type formed in continental collision setting, followed by Endako- and Climax-types formed in continental arcs and rifts, respecti

Semblance

Geology and Geochemistry of Molybdenum Deposits in the Qinling Orogen, P R China

thrombosis

畢業(yè)典禮

https://doi.org/10.1007/978-94-009-0087-5he continental arc and continental rift, respectively. (3) Triassic Qinling Orogen was analogous to the present Mediterranean Sea, accommodating transition from oceanic plate subduction to continental collision, but not a post-collisional extension. (4) The Yanshanian Orogeny in Qinling Orogen was a

Canyon

含糊其辭

Brain Trauma and Nutritional Support,nd fluorite alteration, but weak phyllic and propylitic alteration, and thus assigned to Dabie-type. Four giant PMDs are introduced, which are hosted in granite (Yuchiling), high-grade metamorphic rocks (Leimengou), unmetamorphosed volcanics (Donggou), and volcanic-sedimentary rocks (Jinduicheng). L