The Jinchuan deposit, NW China, is one of the world's most important Ni-Cu-(PGE) sulfide deposits related to a magma conduit system and is hosted in an ultramafic intrusion. The intrusion is composed of lherzolite and dunite with the two largest sulfide ore bodies (named as ore body 1 and 2) in its middle portion. The sulfide ores may be disseminated, net-textured, or massive. The disseminated and net-textured sulfide ores are characterized by variable but generally low PGE concentrations: 10-3200 ppb Pt, 240-9800 ppb Pd, 17-800 ppb Ir, 25-1500 ppb Ru, and 15-400 ppb Rh in 100% sulfides. The massive sulfide ores are extremely low in Pt (<30 ppb) on a 100% sulfides and have very high Cu/Pd ratios, ranging from 10 4 to 4.5 × 10 5. The low PGE...
The Yangliuping Ni–Cu–(PGE) sulfide deposit in southwestern China is hosted by a series of mafic-ult...
Recent analytical developments now make it possible to determine chalcophile and siderophile element...
The ~ 260. Ma Jinbaoshan sill is part of the Permian Emeishan large igneous province in SW China and...
Magmatic sulfide deposits in the Emeishan large igneous province, SW China, have variable chalcophil...
The Jinchuan ultramafic body on the southwestern margin of the North China craton hosts a giant Ni-C...
Cenozoic volcanic rocks are widespread in eastern China. These rocks have variable isotope compositi...
The world-class Jinchuan magmatic Ni–Cu sulfide deposit in China is one of the world's major supplie...
The Kalatongke Cu-Ni sulfide deposit in the Paleozoic Altay orogenic belt, NW China, is hosted in a ...
The Yangliuping Ni-Cu-(PGF) sulfide deposit in southwestern China is hosted by a series of mafic-ult...
The ∼260 Ma-old Baimazhai Ni-Cu-(PGE) sulfide deposit in the Jinping region, Yunnan, SW China, is ho...
The Ni-Cu-PGE sulfide deposits in the Yangliuping area, SW China, are hosted in mafic-ultramafic sil...
International audienceField mapping and petrological-geochemical investigation of the Jinchuan intru...
The division of platinum-group elements (PGE) between those hosted in platinum-group minerals (PGM) ...
The division of platinum-group elements (PGE) between those hosted in platinum-group minerals (PGM) ...
The Jinchuan Ni–Cu sulfide deposit is hosted by an elongated, olivine-rich ultramafic body that is d...
The Yangliuping Ni–Cu–(PGE) sulfide deposit in southwestern China is hosted by a series of mafic-ult...
Recent analytical developments now make it possible to determine chalcophile and siderophile element...
The ~ 260. Ma Jinbaoshan sill is part of the Permian Emeishan large igneous province in SW China and...
Magmatic sulfide deposits in the Emeishan large igneous province, SW China, have variable chalcophil...
The Jinchuan ultramafic body on the southwestern margin of the North China craton hosts a giant Ni-C...
Cenozoic volcanic rocks are widespread in eastern China. These rocks have variable isotope compositi...
The world-class Jinchuan magmatic Ni–Cu sulfide deposit in China is one of the world's major supplie...
The Kalatongke Cu-Ni sulfide deposit in the Paleozoic Altay orogenic belt, NW China, is hosted in a ...
The Yangliuping Ni-Cu-(PGF) sulfide deposit in southwestern China is hosted by a series of mafic-ult...
The ∼260 Ma-old Baimazhai Ni-Cu-(PGE) sulfide deposit in the Jinping region, Yunnan, SW China, is ho...
The Ni-Cu-PGE sulfide deposits in the Yangliuping area, SW China, are hosted in mafic-ultramafic sil...
International audienceField mapping and petrological-geochemical investigation of the Jinchuan intru...
The division of platinum-group elements (PGE) between those hosted in platinum-group minerals (PGM) ...
The division of platinum-group elements (PGE) between those hosted in platinum-group minerals (PGM) ...
The Jinchuan Ni–Cu sulfide deposit is hosted by an elongated, olivine-rich ultramafic body that is d...
The Yangliuping Ni–Cu–(PGE) sulfide deposit in southwestern China is hosted by a series of mafic-ult...
Recent analytical developments now make it possible to determine chalcophile and siderophile element...
The ~ 260. Ma Jinbaoshan sill is part of the Permian Emeishan large igneous province in SW China and...