Permian mafic-ultramafic magmatism and sulfide mineralization in the Central Asian Orogenic Belt: A review

JF Gao, HH Wang - Journal of Asian Earth Sciences, 2024 - Elsevier
Abstract World-class magmatic Ni-Cu-(PGE) deposits have been extensively studied and
are thought to occur in extensional intraplate settings. Recent reports indicate significant …

[HTML][HTML] Geochemistry and genesis of magmatic Ni-Cu-(PGE) and PGE-(Cu)-(Ni) deposits in China

Y Lu, CM Lesher, J Deng - Ore Geology Reviews, 2019 - Elsevier
Magmatic sulfide deposits can be subdivided into 1) Ni-Cu-PGE deposits, which have
relatively smooth mantle-normalized metal patterns, 2) Ni-Cu-(PGE) deposits, which are …

The giant **arihamu Ni-Co sulfide deposit in the East Kunlun orogenic belt, northern Tibet plateau, China

XY Song, JN Yi, LM Chen, YW She… - Economic …, 2016 - pubs.geoscienceworld.org
Abstract The **arihamu Ni-Co deposit, located in the East Kunlun orogenic belt, northern
Tibet plateau, is the secondary largest Ni deposit in China and contains~ 157 million metric …

The roles of various types of crustal contamination in the genesis of the **chuan magmatic Ni-Cu-PGE deposit: New mineralogical and CS-Sr-Nd isotope constraints

S Xue, Q Wang, Y Wang, W Song… - Economic …, 2023 - pubs.geoscienceworld.org
Addition of crustal sulfur to the **chuan magma or oxidation of the magma associated with
carbonate assimilation has been considered to be the main cause of sulfide saturation in the …

The giant **chuan Ni-Cu-(PGE) deposit: Tectonic setting, magma evolution, ore genesis, and exploration implications

C Li, EM Ripley - 2011 - pubs.geoscienceworld.org
Abstract The **chuan Ni-Cu-(PGE) deposit is the largest single magmatic Ni deposit in the
world. It is hosted by a small ultramafic intrusion in the Longshoushan terrane located in the …

Zircon dating, Hf–Sr–Nd–Os isotopes and PGE geochemistry of the Tianyu sulfide-bearing mafic–ultramafic intrusion in the Central Asian Orogenic Belt, NW China

D Tang, K Qin, C Li, L Qi, B Su, W Qu - Lithos, 2011 - Elsevier
The Tianyu mafic–ultramafic intrusion is one of many important sulfide-bearing mafic–
ultramafic intrusions in the eastern Tianshan terrane located in the southern margin of the …

Precise U–Pb zircon–baddeleyite age of the **chuan sulfide ore-bearing ultramafic intrusion, western China

M Zhang, SL Kamo, C Li, P Hu, EM Ripley - Mineralium Deposita, 2010 - Springer
The **chuan ultramafic intrusion in western China hosts the third-largest magmatic Ni–Cu
deposit in the world. The crystallization age of the intrusion has long been debated. Here …

Three-dimensional mineral prospectivity modeling with geometric restoration: Application to the **chuan Ni–Cu–(PGE) Sulfide Deposit, Northwestern China

X Mao, Z Su, H Deng, Z Liu, L Li, Y Wang… - Natural Resources …, 2024 - Springer
Structural deformation is ubiquitous throughout geological history. For a mineral deposit that
underwent structural deformation after its formation, its geological architecture may have …

Up, down, or sideways: emplacement of magmatic Fe–Ni–Cu–PGE sulfide melts in large igneous provinces

CM Lesher - Canadian Journal of Earth Sciences, 2019 - cdnsciencepub.com
The preferential localization of Fe–Ni–Cu–PGE sulfides within the horizontal components of
dike–sill–lava flow complexes in large igneous provinces (LIPs) indicates that they were …

Origin of PGE-depleted Ni-Cu sulfide mineralization in the Triassic Hongqiling No. 7 orthopyroxenite intrusion, Central Asian orogenic belt, northeastern China

B Wei, CY Wang, C Li, Y Sun - Economic Geology, 2013 - pubs.geoscienceworld.org
Abstract The~ 216 Ma Hongqiling No. 7 intrusion is located in the southern margin of the
Central Asian orogenic belt, northeastern China. It was the second largest Ni producer after …