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6 FAQs about [Jinchuan open pit rock drill]
How deep is the Jinchuan intrusion?
The Jinchuan intrusion was formed by the injection of high yield-strength, relatively viscous, high-density olivine- and sulphide-laden mushes from a depth estimated to be >4 km into nearby planar fractures/faults.
Where is the Jinchuan ultramafic intrusion located?
The Jinchuan ultramafic intrusion, which hosts a nickel-copper-PGE deposit, is located at 38°28′18″N, 102°10′59″E, some 300 km NNW of Lanzhou and 1200 km to the west of Beijing, in the city of Jinchang, north-central Gansu Province, China.
How did the Jinchuan deposit form?
The Jinchuan deposit formed at a depth of over 4 km when sulphide-rich magma passed through the structure and settled as cumulus deposits to create this intrusion. The resultant intrusion contains disseminated and net-textured sulphides in sulphide-dunite cores within a larger lherzolite sill complex.
How did the Longshoushan uplift affect the Jinchuan deposit?
The Longshoushan Uplift, an elongate, downward tapering faulted wedge, was uplifted by over 4 km during the Cenozoic shortening to expose the Jinchuan deposit in a window penetrating younger cover rocks. During this same event, the intrusion was tilted and fragmented into four structural segments.
What is the Jinchuan intrusion?
The Jinchuan intrusion is a 6500 m long and a few to 500 m wide geological feature that dips at 50° to 80°SW. It is composed of dunite, lherzolite, and pyroxenite, and has an indicated crystallisation age of 827 ± 8 Ma (U-Pb SHRIMP dating of zircon and baddeleyite; Li et al., 2004, Li et al., 2005).
Where is Jinchuan Group located?
Jinchuan Group of Gansu Province is located in the northwest of China and is referred to as “China’s most advanced mines”, It is, within the scope of mining and technology of China, one of the most advanced, high degree of mechanization mining (see Figure 3 a) . Figure 3.