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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Asia
-
Altai Mountains
-
Kalba Range (1)
-
-
Altai-Sayan region (1)
-
Central Asia
-
Kazakhstan
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Eastern Kazakhstan (1)
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Far East
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Borneo
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East Malaysia
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Sarawak Malaysia (1)
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China
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Qinling Mountains (1)
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Indonesia
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Japan
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Kyushu (1)
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Malaysia
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Kyrgyzstan (1)
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Iran
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helium
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neon
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oxygen
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Invertebrata
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Primary terms
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Asia
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Altai Mountains
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carbon
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Cenozoic
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Quaternary
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Tertiary
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middle Tertiary (1)
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Paleogene
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igneous rocks
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-
diabase (1)
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diorites
-
plagiogranite (1)
-
-
granites
-
aplite (1)
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monzogranite (1)
-
-
lamprophyres (2)
-
pegmatite (1)
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quartz monzonite (1)
-
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porphyry (1)
-
volcanic rocks
-
basalts (2)
-
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-
ash-flow tuff (2)
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rhyolites (3)
-
-
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inclusions
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fluid inclusions (17)
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intrusions (23)
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Invertebrata
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Pb-207/Pb-204 (3)
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Pb-208/Pb-204 (2)
-
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stable isotopes
-
Ar-38/Ar-36 (1)
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Ar-40/Ar-36 (1)
-
C-13/C-12 (11)
-
D/H (10)
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deuterium (1)
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He-4/He-3 (1)
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Ne-22/Ne-20 (1)
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Ne-22/Ne-21 (1)
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O-18/O-16 (24)
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Pb-206/Pb-204 (3)
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Pb-207/Pb-204 (3)
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Pb-208/Pb-204 (2)
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S-34/S-32 (17)
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Sr-87/Sr-86 (1)
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magmas (9)
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Kalimantan Indonesia (1)
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mantle (2)
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Mesozoic
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Cretaceous
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Lower Cretaceous (1)
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Upper Cretaceous
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Horseshoe Canyon Formation (1)
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Jurassic
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lower Mesozoic (1)
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Triassic
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metal ores
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Sr-87/Sr-86 (1)
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antimony (5)
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lead
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metamorphic rocks
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carlin-type deposits
Gold metallogeny in Iran; implications for gold exploration and conceptual modelling
Gravity inversion with a binary structure constraint imposed by magnetotelluric data and its application to a Carlin-type gold deposit
Large-scale basement mobilization endows the giant Carlin-type gold mineralization in the Youjiang Basin, South China: Insights from mercury isotopes
Timing of Rhyolite Intrusion and Carlin-Type Gold Mineralization at the Cortez Hills Carlin-Type Deposit, Nevada, USA
New insights into the source of gold in the Youjiang basin, SW China
Seismic Reflection Profiles Reveal the Ore-Controlling Structures of Carlin-Style Gold Deposits in Lannigou Gold Fields, Southwestern Guizhou, China
“Roll-Front” Mass Transfer of Carbonate Cations in Carlin-Type Gold Deposits: Insights from UV-Fluorescent Calcite Veins
Yukon’s Carlin-Type Gold Deposits (Rackla Belt, Canada): Main Characteristics and New Insights on Alteration Styles and Geochemistry
U-Pb VEIN CALCITE DATING REVEALS THE AGE OF CARLIN-TYPE GOLD DEPOSITS OF CENTRAL YUKON AND A CONTEMPORANEITY WITH A REGIONAL INTRUSION-RELATED METALLOGENIC EVENT
Nanoscale isotopic evidence resolves origins of giant Carlin-type ore deposits
Tracing fluid evolution in sedimentary basins with calcite geochemical, isotopic and U-Pb geochronological data: Implications for petroleum and mineral resource accumulation in the Nanpanjiang Basin, South China
GEOTHERMAL SYSTEMS IN THE NORTHERN APENNINES, ITALY: MODERN ANALOGUES OF CARLIN-STYLE GOLD DEPOSITS
CALCITE U-Pb DATING UNRAVELS THE AGE AND HYDROTHERMAL HISTORY OF THE GIANT SHUIYINDONG CARLIN-TYPE GOLD DEPOSIT IN THE GOLDEN TRIANGLE, SOUTH CHINA
U-Pb Dating on Hydrothermal Rutile and Monazite from the Badu Gold Deposit Supports an Early Cretaceous Age for Carlin-Type Gold Mineralization in the Youjiang Basin, Southwestern China
Quantitative Mineral Mapping of Drill Core Surfaces II: Long-Wave Infrared Mineral Characterization Using μ XRF and Machine Learning
EVOLUTION OF INVISIBLE Au IN ARSENIAN PYRITE IN CARLIN-TYPE Au DEPOSITS
EOCENE MAGMA PLUMBING SYSTEM BENEATH CORTEZ HILLS CARLIN-TYPE GOLD DEPOSIT, NEVADA: IS THERE A DEEP-SEATED PLUTON?
The geophysical response of the Goldrush-Fourmile orebody and implications for camp-scale Carlin-type deposit exploration, Cortez District, Nevada
NOBLE GASES FINGERPRINT THE SOURCE AND EVOLUTION OF ORE-FORMING FLUIDS OF CARLIN-TYPE GOLD DEPOSITS IN THE GOLDEN TRIANGLE, SOUTH CHINA
Abstract Gold is either the only economically important metal or a major by-product in 11 well-characterized deposit types—paleoplacer, orogenic, porphyry, epithermal, Carlin, placer, reduced intrusion related, volcanogenic massive sulfide (VMS), skarn, carbonate replacement, and iron oxide-copper-gold (IOCG), arguably more than for those of any other metal; it also dominates a number of deposits of uncertain or unknown origin. Major gold concentrations formed worldwide from the Mesoarchean to the Pleistocene, from Earth’s surface to midcrustal paleodepths, alone or in association with silver, base metals, and/or uranium, and from hydrothermal fluids of predominantly metamorphic, magmatic, meteoric, seawater, or, uncommonly, basinal origins, as well as from mafic magma or ambient surface water. Most of the Neoproterozoic and Phanerozoic deposits unequivocally formed in accretionary orogens. As an introduction to this compilation of the world’s major gold deposits and provinces, this paper provides a thumbnail sketch of each gold deposit type, including geologic and economic characteristics and widely accepted genetic models, as well as briefly discusses aspects of their spatial and temporal associations and distributions.