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![Location of <span class="search-highlight">Kalatongke</span> <span class="search-highlight">deposit</span> in the Xinjiang Uygur Autonomous Region, Chi...]()
![Underground images of the typical ores from the <span class="search-highlight">Kalatongke</span> <span class="search-highlight">deposit</span>. (a, b) ...]()
![Location of the <span class="search-highlight">Kalatongke</span> Ni-Cu <span class="search-highlight">deposit</span> in the Xinjiang Uygur Autonomous R...]()
![Al-Fe-Cr ternary diagram for the Cr-spinel, Cr-magnetite, and magnetite of ...]()
![Location of the Ni-Cu <span class="search-highlight">deposits</span> in the Central Asian orogenic belt. The Kala...]()
![Correlation between Ni, Co, Zn content and ferrous Fe in the X site of the ...]()
![A simplified geologic map of the Xinjiang Uygur autonomous region in northw...]()
![Simplified geological map ( a ) and sections ( b–d ) of the <span class="search-highlight">Kalatongke</span> depo...]()
![(a) Simplified geologic map of the Central Asian orogenic belt, showing the...]()
![Sulfide particle size distribution (PSD) of individual samples from the Kal...]()
![Major contents ( a–e ) and Cr# variation ( f ) in Cr-spinel, Cr-magnetite, ...]()
![A cartoon shows the emplacement and enrichment processes of the <span class="search-highlight">Kalatongke</span> ...]()
![The discrimination diagrams of the origin of the massive sulfide in terms o...]()
![Pearce trace element ratio-ratio plots for intrusion-dominated orogens and ...]()
![Trace element variations of Cr-spinel, Cr-magnetite, and magnetite from the...]()
![Photos and combined false-color X-ray fluorescence (XRF) images of the type...]()
RESULTS FOR
Kalatongke Deposit
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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South Africa
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Central Asia
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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Re-187/Os-188 (2)
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stable isotopes
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C-13/C-12 (1)
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C-14/C-12 (1)
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He-4/He-3 (1)
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Hf-177/Hf-176 (7)
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Nd-144/Nd-143 (14)
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O-18/O-16 (5)
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Os-188/Os-187 (5)
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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Re-187/Os-188 (2)
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S-34/S-32 (10)
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Sr-87/Sr-86 (11)
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large-ion lithophile elements (1)
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Lu/Hf (2)
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magnesium (1)
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Sr-87/Sr-86 (11)
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antimony (1)
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chromium (1)
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upper Precambrian
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ophiolite (1)
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olivine group
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forsterite (2)
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olivine (6)
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zircon group
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zircon (17)
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sheet silicates
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sulfides
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chalcopyrite (5)
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cobaltite (1)
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copper sulfides (2)
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gersdorffite (1)
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nickel sulfides (3)
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pentlandite (4)
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pyrite (3)
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pyrrhotite (1)
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tellurides (1)
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wehrlite (1)
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Primary terms
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absolute age (23)
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Africa
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East Africa
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Tanzania (2)
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Mozambique Belt (1)
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Southern Africa
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South Africa
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Bushveld Complex (2)
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Merensky Reef (1)
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Asia
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Altai Mountains
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Gorny Altai (1)
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Mongolian Altai (2)
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Altai Russian Federation
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Gorny Altai (1)
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Baikal region (1)
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Central Asia
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Kazakhstan (2)
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Dzhugdzhur region (1)
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Far East
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China
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Da Hinggan Ling (1)
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Gansu China (2)
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Heilongjiang China (1)
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Inner Mongolia China (4)
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Jilin China (1)
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Kunlun Fault (1)
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Kunlun Mountains (3)
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Qinghai China (5)
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Sichuan China (1)
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Tarim Platform (2)
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Xinjiang China
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Junggar (7)
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Junggar Basin (1)
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Tarim Basin (3)
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Turpan Basin (1)
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Yangtze Platform (1)
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Yunnan China
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Ailao Shan (1)
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Mongolia
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Hangay Mountains (1)
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Mongolian Altai (2)
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Gobi Desert (1)
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Krasnoyarsk Russian Federation
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Taymyr Dolgan-Nenets Russian Federation
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Norilsk region (1)
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Sayan
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Eastern Sayan (1)
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Siberia (5)
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Siberian fold belt (1)
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Siberian Platform (2)
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Stanovoy Range (1)
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Tibetan Plateau (5)
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Tien Shan (8)
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Yakutia Russian Federation (1)
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Australasia
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Australia
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Western Australia
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Fraser Range (1)
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Halls Creek Orogen (1)
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Canada
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Eastern Canada
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Ontario
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Sudbury Structure (1)
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carbon
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C-13/C-12 (1)
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C-14/C-12 (1)
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organic carbon (1)
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Cenozoic
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Tertiary
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Paleogene
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Eocene (2)
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Paleocene (1)
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chemical analysis (1)
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core (2)
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crust (7)
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crystal chemistry (2)
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crystal growth (1)
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data processing (1)
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deformation (2)
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Eurasia (1)
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Europe
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Western Europe
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Scandinavia
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Finland (1)
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faults (9)
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geochemistry (6)
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geochronology (2)
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geophysical methods (5)
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heat flow (3)
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igneous rocks
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carbonatites (1)
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picrite (2)
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plutonic rocks
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diabase
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tholeiitic dolerite (1)
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diorites
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quartz diorites (1)
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tonalite (1)
-
-
gabbros
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alkali gabbros
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teschenite (1)
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-
norite (5)
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olivine gabbro (1)
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troctolite (4)
-
-
granites
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A-type granites (1)
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granodiorites (1)
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lamprophyres (1)
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ultramafics
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chromitite (1)
-
peridotites
-
dunite (4)
-
harzburgite (1)
-
lherzolite (2)
-
-
pyroxenite
-
orthopyroxenite (2)
-
websterite (2)
-
-
-
-
volcanic rocks
-
andesites
-
boninite (1)
-
-
basalts
-
alkali basalts (1)
-
mid-ocean ridge basalts (9)
-
ocean-island basalts (1)
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tholeiite (1)
-
tholeiitic basalt (1)
-
-
komatiite (1)
-
-
-
inclusions (2)
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intrusions (35)
-
isotopes
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radioactive isotopes
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C-14/C-12 (1)
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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Re-187/Os-188 (2)
-
-
stable isotopes
-
C-13/C-12 (1)
-
C-14/C-12 (1)
-
He-4/He-3 (1)
-
Hf-177/Hf-176 (7)
-
Nd-144/Nd-143 (14)
-
O-18/O-16 (5)
-
Os-188/Os-187 (5)
-
Pb-206/Pb-204 (1)
-
Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (1)
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Re-187/Os-188 (2)
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S-34/S-32 (10)
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Sr-87/Sr-86 (11)
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magmas (36)
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mantle (17)
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Mesozoic
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Cretaceous
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Lower Cretaceous (1)
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Jurassic
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Lower Jurassic (1)
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Middle Jurassic (1)
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lower Mesozoic (1)
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Triassic
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Lower Triassic
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Permian-Triassic boundary (2)
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Middle Triassic (1)
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Upper Triassic (3)
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-
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metal ores
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chromite ores (2)
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cobalt ores (8)
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copper ores (45)
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gold ores (2)
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iron ores (1)
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lead ores (1)
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lead-zinc deposits (1)
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molybdenum ores (2)
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nickel ores (45)
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platinum ores (12)
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polymetallic ores (2)
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zinc ores (2)
-
-
metals
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alkaline earth metals
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magnesium (1)
-
strontium
-
Sr-87/Sr-86 (11)
-
-
-
antimony (1)
-
arsenic (1)
-
bismuth (1)
-
chromium (1)
-
copper (4)
-
gold (1)
-
hafnium
-
Hf-177/Hf-176 (7)
-
-
iron
-
ferric iron (2)
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ferrous iron (2)
-
-
lead
-
Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
-
Pb-208/Pb-204 (1)
-
-
mercury (1)
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nickel (4)
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platinum group
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osmium
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Os-188/Os-187 (5)
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Re-187/Os-188 (2)
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palladium (3)
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platinum (1)
-
platinum ores (12)
-
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rare earths
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neodymium
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Nd-144/Nd-143 (14)
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rhenium
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Re-187/Os-188 (2)
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silver (1)
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titanium (1)
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metamorphic rocks
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amphibolites (3)
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eclogite (2)
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gneisses
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granite gneiss (1)
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orthogneiss (1)
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marbles (1)
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metaigneous rocks
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metapyroxenite (1)
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metatuff (1)
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serpentinite (1)
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metasedimentary rocks
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metasandstone (1)
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metasomatic rocks
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serpentinite (1)
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migmatites (1)
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schists
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blueschist (1)
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-
-
metamorphism (3)
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metasomatism (5)
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mineral deposits, genesis (28)
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1-20 OF 132 RESULTS FOR
Kalatongke Deposit
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Journal Article
Origin of PGE-Poor and Cu-Rich Magmatic Sulfides from the Kalatongke Deposit, Xinjiang, Northwest China
Journal: Economic Geology
Publisher: Society of Economic Geologists
Published: 01 May 2012
Economic Geology (2012) 107 (3): 481–506.
...Jian-Feng Gao; Mei-Fu Zhou; Peter C. Lightfoot; Christina Yan Wang; Liang Qi Abstract The Kalatongke Cu-Ni sulfide deposit in the Paleozoic Altay orogenic belt, NW China, is hosted in a Permian mafic intrusion consisting of norite, troctolite, gabbro, and diorite. Disseminated Ni-Cu, massive Ni-Cu...
Journal Article
Sulfide Ore Formation of the Kalatongke Ni-Cu Deposit as Illustrated by Sulfide Textures
Ya-Jing Mao, Stephen J. Barnes, Belinda Godel, Louise Schoneveld, Ke-Zhang Qin, Dongmei Tang, Morgan Williams, Zhen Kang
Journal: Economic Geology
Publisher: Society of Economic Geologists
Published: 01 December 2022
Economic Geology (2022) 117 (8): 1761–1778.
...Ya-Jing Mao; Stephen J. Barnes; Belinda Godel; Louise Schoneveld; Ke-Zhang Qin; Dongmei Tang; Morgan Williams; Zhen Kang Abstract The Kalatongke magmatic Ni-Cu deposit features high Ni-Cu grades compared with other Ni-Cu deposits in the Central Asian orogenic belt. The sulfides, mainly hosted...
Includes: Supplemental Content
Image
Location of Kalatongke deposit in the Xinjiang Uygur Autonomous Region, Chi...
in Is short-offset frequency-domain controlled-source electromagnetic survey using an equatorial configuration a good choice on land?
> Geophysics
Published: 03 December 2024
Figure 14. Location of Kalatongke deposit in the Xinjiang Uygur Autonomous Region, China (modified after Mao et al., 2018 ). The Kalatongke deposit is highlighted in red in the figure.
Image
Underground images of the typical ores from the Kalatongke deposit. (a, b) ...
in Sulfide Ore Formation of the Kalatongke Ni-Cu Deposit as Illustrated by Sulfide Textures
> Economic Geology
Published: 01 December 2022
Fig. 2. Underground images of the typical ores from the Kalatongke deposit. (a, b) Globular ore with variable grain size observed in olivine norite and gabbronorite at line 51 of the Y2 intrusion; part of the globule was connected with others forming a sulfide network, and the rim of the sulfide
Journal Article
Electromagnetic Characteristics of the Magmatic Ni-Cu Sulfide Deposits in the Orogenic Belt: A Case Study from Kalatongke Deposits in the Central Asian Orogenic Belt
Journal: Economic Geology
Publisher: Society of Economic Geologists
Published: 01 December 2022
Economic Geology (2022) 117 (8): 1779–1789.
... to explore the Ni-Cu ores in the Central Asian orogenic belt. The Kalatongke deposit is the largest Ni-Cu deposit in the Central Asian orogenic belt and has become the second largest Ni-Cu sulfide deposit, after the Jinchuan Ni-Cu sulfide deposit, in China ( Duan et al., 2017 ). We selected...
Image
Location of the Kalatongke Ni-Cu deposit in the Xinjiang Uygur Autonomous R...
in Imaging of a shallow magma conduit system based on a high-power frequency-domain controlled-source electromagnetic survey
> Geophysics
Published: 02 February 2023
Figure 1. Location of the Kalatongke Ni-Cu deposit in the Xinjiang Uygur Autonomous Region, China (modified after Mao et al., 2018 ). The Kalatongke deposit is marked in red.
Journal Article
Crystallization of spinel from coexisting silicate and sulfide immiscible liquids: An equilibrium case with postcumulus reactions
Ya-Jing Mao, Stephen J. Barnes, Louise Schoneveld, Belinda Godel, Morgan Williams, Dongmei Tang, Zhen Kang, Ke-Zhang Qin
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 May 2023
American Mineralogist (2023) 108 (5): 832–846.
...Ya-Jing Mao; Stephen J. Barnes; Louise Schoneveld; Belinda Godel; Morgan Williams; Dongmei Tang; Zhen Kang; Ke-Zhang Qin Abstract Spinel minerals occur as inclusions in both silicates and sulfides in the Kalatongke magmatic Ni-Cu deposit in NW. China, showing textural and compositional variations...
Image
Al-Fe-Cr ternary diagram for the Cr-spinel, Cr-magnetite, and magnetite of ...
in Crystallization of spinel from coexisting silicate and sulfide immiscible liquids: An equilibrium case with postcumulus reactions
> American Mineralogist
Published: 01 May 2023
Figure 6. Al-Fe-Cr ternary diagram for the Cr-spinel, Cr-magnetite, and magnetite of the Kalatongke deposit, in comparison with that from other regional deposits and the Noril’sk camp. The Kalatongke data are from this study. The Norilsk spinel data are from Schoneveld et al. (2020
Image
Location of the Ni-Cu deposits in the Central Asian orogenic belt. The Kala...
in Electromagnetic Characteristics of the Magmatic Ni-Cu Sulfide Deposits in the Orogenic Belt: A Case Study from Kalatongke Deposits in the Central Asian Orogenic Belt
> Economic Geology
Published: 01 December 2022
Fig. 1. Location of the Ni-Cu deposits in the Central Asian orogenic belt. The Kalatongke deposit is marked in red (modified from Wei et al., 2019 ).
Image
Correlation between Ni, Co, Zn content and ferrous Fe in the X site of the ...
in Crystallization of spinel from coexisting silicate and sulfide immiscible liquids: An equilibrium case with postcumulus reactions
> American Mineralogist
Published: 01 May 2023
Figure 8. Correlation between Ni, Co, Zn content and ferrous Fe in the X site of the Cr-spinel, Cr-magnetite, and magnetite from the Kalatongke deposit. The ratio is calculated by ferrous Fe to other elements. (Color online.)
Image
A simplified geologic map of the Xinjiang Uygur autonomous region in northw...
in Induced polarization effect on grounded-wire transient electromagnetic data from transverse electric and magnetic fields
> Geophysics
Published: 13 June 2020
Figure 11. A simplified geologic map of the Xinjiang Uygur autonomous region in northwest China, showing the location of the observed area, Kalatongke deposit, displayed by the yellow solid circle in the upper part of the map (modified from Mao et al., 2018 ).
Image
Simplified geological map ( a ) and sections ( b–d ) of the Kalatongke depo...
in Crystallization of spinel from coexisting silicate and sulfide immiscible liquids: An equilibrium case with postcumulus reactions
> American Mineralogist
Published: 01 May 2023
Figure 2. Simplified geological map ( a ) and sections ( b–d ) of the Kalatongke deposit, showing the distribution of the mafic intrusions and the variable types of sulfide mineralization within them. The geological map is from Wang and Zhao (1991) , whereas the sections are from Xinxin Mining
Image
(a) Simplified geologic map of the Central Asian orogenic belt, showing the...
in Sulfide Ore Formation of the Kalatongke Ni-Cu Deposit as Illustrated by Sulfide Textures
> Economic Geology
Published: 01 December 2022
Fig. 1. (a) Simplified geologic map of the Central Asian orogenic belt, showing the distribution of Irtysh fault ( Briggs et al., 2007 ). (b-e) Geologic map and sections of the Kalatongke deposit, showing the distribution of the mafic intrusions and different kinds of mineralization, modified
Image
Sulfide particle size distribution (PSD) of individual samples from the Kal...
in Sulfide Ore Formation of the Kalatongke Ni-Cu Deposit as Illustrated by Sulfide Textures
> Economic Geology
Published: 01 December 2022
Fig. 8. Sulfide particle size distribution (PSD) of individual samples from the Kalatongke deposit, showing kinked PSD with two log-linear segments. The dashed gray lines represent linear regression curves for different segments. The solid gray line shows the cumulative frequency of sulfide
Image
Major contents ( a–e ) and Cr# variation ( f ) in Cr-spinel, Cr-magnetite, ...
in Crystallization of spinel from coexisting silicate and sulfide immiscible liquids: An equilibrium case with postcumulus reactions
> American Mineralogist
Published: 01 May 2023
Figure 5. Major contents ( a–e ) and Cr# variation ( f ) in Cr-spinel, Cr-magnetite, and magnetite of the Kalatongke deposit. Mg# equals 100 × Mg/(Mg+Fe), Cr# equals 100 × Cr/(Cr+Al). The Al 2 O 3 and Cr 2 O 3 contents in magnetite are close to the detection limit and not plotted in the Cr
Image
A cartoon shows the emplacement and enrichment processes of the Kalatongke ...
in Sulfide Ore Formation of the Kalatongke Ni-Cu Deposit as Illustrated by Sulfide Textures
> Economic Geology
Published: 01 December 2022
Fig. 10. A cartoon shows the emplacement and enrichment processes of the Kalatongke deposit. (a) A bladed dike intruded along the intersections of faults. (b) Sulfide accumulated at the funnel-shaped pathway. (c) Sulfide segregation in the tubeshaped pathway and accumulation at the base
Image
The discrimination diagrams of the origin of the massive sulfide in terms o...
in Crystallization of spinel from coexisting silicate and sulfide immiscible liquids: An equilibrium case with postcumulus reactions
> American Mineralogist
Published: 01 May 2023
Figure 10. The discrimination diagrams of the origin of the massive sulfide in terms of the association of Cr vs. Ti ( a ), V ( b ), and Ni ( c ) contents in magnetite. The magnetite included in the massive sulfide of the Kalatongke deposit plot on the region of the magnetite crystallized from
Image
Pearce trace element ratio-ratio plots for intrusion-dominated orogens and ...
in Lithogeochemistry in exploration for intrusion-hosted magmatic Ni–Cu–Co deposits
> Geochemistry: Exploration, Environment, Analysis
Published: 02 February 2023
North host intrusions compared with background in the Halls Creek Orogen. ( c ) Jinchuan deposit, Gansu, China. ( d ) Xiarihamu deposit in the Kunlun Orogenic Belt, Tibet. ( e ) Kalatongke deposit, Central Asian Orogenic Belt (CAOB), Xinjiang, China and other deposits in the CAOB. PM-UCC mix
Image
Trace element variations of Cr-spinel, Cr-magnetite, and magnetite from the...
in Crystallization of spinel from coexisting silicate and sulfide immiscible liquids: An equilibrium case with postcumulus reactions
> American Mineralogist
Published: 01 May 2023
Figure 7. Trace element variations of Cr-spinel, Cr-magnetite, and magnetite from the Kalatongke deposit. The Cr-magnetite grains enclosed in disseminated sulfides have similar V, Sc, Ga, Mo, Zr, and Nb concentrations ( a–f ) but depleted Ni, Co, and Zn ( g–i ) contents relative to those enclosed
Image
Photos and combined false-color X-ray fluorescence (XRF) images of the type...
in Sulfide Ore Formation of the Kalatongke Ni-Cu Deposit as Illustrated by Sulfide Textures
> Economic Geology
Published: 01 December 2022
Fig. 3. Photos and combined false-color X-ray fluorescence (XRF) images of the type-1 globular sulfides in fine-grained gabbro (a) and moderate- to coarse-grained gabbronorite (b), emulsion textured ore (c, d), and massive ore (e) of the Kalatongke deposits at a hand sample scale, showing
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