喃喃而言
发表于 2025-3-23 12:00:44
,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
发表于 2025-3-23 13:53:07
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
发表于 2025-3-23 21:13:45
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柱廊
发表于 2025-3-24 00:16:37
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
发表于 2025-3-24 04:57:16
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
发表于 2025-3-24 08:57:33
Geology and Geochemistry of Molybdenum Deposits in the Qinling Orogen, P R China
thrombosis
发表于 2025-3-24 13:24:36
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毕业典礼
发表于 2025-3-24 15:35:58
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
发表于 2025-3-24 21:01:15
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含糊其辞
发表于 2025-3-24 23:37:05
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