A5030092264- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- High-pressure geophysics and materials
- earthquake and tectonic studies
- Geochemistry and Geochronology of Asian Mineral Deposits
- Hydrocarbon exploration and reservoir analysis
- Educational Reforms and Innovations
- Medical Research and Treatments
- Geology and Paleoclimatology Research
- Gas Sensing Nanomaterials and Sensors
- Pacific and Southeast Asian Studies
- Advanced Photocatalysis Techniques
- Geochemistry and Elemental Analysis
- Archaeology and ancient environmental studies
- Environmental DNA in Biodiversity Studies
- Radioactive element chemistry and processing
- Fusion materials and technologies
- Geoscience and Mining Technology
- Climate Change Policy and Economics
- Banking Systems and Strategies
- Hydrogen embrittlement and corrosion behaviors in metals
- Advanced Computational Techniques and Applications
- COVID-19 and healthcare impacts
- Bone and Dental Protein Studies
- Metallurgical Processes and Thermodynamics
Chinese Academy of Sciences
2015-2024
Institute of Geology and Geophysics
2015-2024
University of Chinese Academy of Sciences
2014-2023
Anhui University of Technology
2021
Institute of Geology and Geophysics
2020
Mineral Resources
2017-2018
Commonwealth Scientific and Industrial Research Organisation
2017-2018
Australian Resources Research Centre
2017-2018
Shanghai University
2017
Shanghai Research Institute of Materials
2017
The Poyi magmatic Ni-Cu sulfide deposit is situated in the Beishan fold belt northeastern rim of Tarim craton. Many Permian deposits, such as those East Tianshan, are present adjacent Central Asian orogenic to north. hosted a small dike-like ultramafic-troctolitic body that was emplaced into much larger gabbroic intrusion. Our new zircon U-Pb isotope data reveal these two intrusions formed ~6 Ma apart. intrusion at 269.9 ± 1.7 Ma, whereas 276.1 1.9 Ma. results show youngest among major...
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The Jinchuan intrusion is the largest single magmatic nickel sulphide deposit in world. Sulphide mineralization mainly occurs two segments (I and II). crystal size distributions (CSDs) of olivines are distinctly different. For all segments, their grain sizes values clustering index R increase with increasing olivine abundance cumulates, illustrating overgrowth trends for Segment II a combination compaction I olivines. Kinked CSDs cumulates suggest presence populations different nucleation...
Abstract The Kalatongke magmatic Ni-Cu deposit features high grades compared with other deposits in the Central Asian orogenic belt. sulfides, mainly hosted by olivine norite and gabbronorite, are characterized Cu/Ni ratios. There is wide variety of textural relationships mineralized rocks, including globular, sulfide matrix, emulsion, disseminated, net-textured, semimassive to massive textures. Quantitative measurements reveal that more than 65 vol % total volume disseminated ore (defined...
Small intrusions dominated by olivine- and pyroxene-rich cumulates are well known to be favourable hosts magmatic Ni-Cu-(Platinum Group Element - PGE) sulfide mineralization. Such common in a variety of settings around the world, but only very small proportion contain economically exploitable sulfides; these tend conduit or chonolith style. If prospectivity could discriminated from sparse sampling at early exploration stages, then discovery rate for deposits this type improved. To end,...
Abstract Olivine is an important mineral in mafic–ultramafic rocks and records various crustal mantle processes basaltic magma. Generally, phosphorus (P) immobile olivine its zoning tends to record magmatic processes. In contrast, lithium (Li) one of the most mobile elements be re-distributed by postcumulus hydrothermal This study reports coupled Li-P oscillatory sector cumulus (Fo > 80 mol%) from Ni-Cu deposits northwest China. The close 1:1 relationship between Li + Na cation P...
The Permian Hulu intrusion is one of several sulphide-bearing mafic–ultramafic intrusions in the eastern part Tianshan located at southern margin Central Asian Orogenic Belt (CAOB) Xinjiang, NW China. composed lherzolite, olivine websterite, gabbro, and gabbro-diorite. Disseminated net-textured Ni-Cu sulphide ores are bottom lopolith complex. Negative Zr, Hf, Nb, Ta anomalies, whole-rock εNd(t) values +5.7 to +8.8, variable (Th/Nb)PM (from 1.06 8.13) suggest that source complexes depleted...
A critical and strategic metal, demand for cobalt (Co) has increased in recent years given its widespread use new energy batteries. This led to the need search Co sources. Porphyry deposits have provided large quantities of Cu, Mo, Au other elements such as Re, Se Te. However, there is a paucity research on occurrence, enrichment mechanisms, metallogenic potential porphyry deposits. The Palaeo-Pacific slab subduction related Jinchang deposit (∼80 t @ 8 g/t Au; Heilongjiang province, NE...