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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Congo (1)
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East Africa
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Zambia (1)
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Southern Africa
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Namibia (2)
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Altiplano (1)
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Asia
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Arabian Peninsula
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Yemen (3)
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Australasia
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Australia
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Western Australia (1)
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Canada
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Western Canada
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British Columbia (1)
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Canadian Cordillera (1)
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Copperbelt (1)
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Europe
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Central Europe
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Poland
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Upper Silesia (1)
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Southern Europe
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Iberian Peninsula
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Spain
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Andalusia Spain
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Donana National Park (1)
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Huelva Spain (1)
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Italy
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Lombardy Italy
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Bergamo Italy (1)
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Sardinia Italy (1)
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-
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Mexico
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Chihuahua Mexico (1)
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Guanajuato Mexico (1)
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Michoacan Mexico (1)
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San Luis Potosi Mexico (1)
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Trans-Mexican volcanic belt (1)
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North America
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Chihuahua tectonic belt (1)
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Gulf Coastal Plain (1)
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North American Cordillera
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Canadian Cordillera (1)
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South America
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Peru (3)
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United States
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Alaska
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Nixon Fork Terrane (1)
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Trans-Pecos (1)
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commodities
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metal ores
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base metals (1)
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cobalt ores (1)
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copper ores (2)
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lead ores (8)
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lead-zinc deposits (8)
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polymetallic ores (1)
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silver ores (1)
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zinc ores (10)
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mineral deposits, genesis (9)
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mineral exploration (3)
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petroleum
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natural gas (1)
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elements, isotopes
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carbon
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C-13/C-12 (2)
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isotope ratios (4)
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isotopes
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radioactive isotopes
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Pb-206/Pb-204 (2)
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Pb-207/Pb-204 (2)
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Pb-208/Pb-204 (2)
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stable isotopes
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C-13/C-12 (2)
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O-18/O-16 (2)
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Pb-206/Pb-204 (2)
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Pb-207/Pb-204 (2)
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Pb-208/Pb-204 (2)
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Sr-87/Sr-86 (3)
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (3)
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cobalt (1)
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lead
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Pb-206/Pb-204 (2)
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Pb-207/Pb-204 (2)
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Pb-208/Pb-204 (2)
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zinc (2)
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oxygen
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O-18/O-16 (2)
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fossils
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Chordata
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Vertebrata
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Tetrapoda
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Mammalia
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Theria
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Eutheria
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Artiodactyla
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Suiformes
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Suidae (1)
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ichnofossils (1)
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Invertebrata
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Mollusca
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Cephalopoda
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Ammonoidea (1)
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tracks (1)
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geochronology methods
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Ar/Ar (1)
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K/Ar (1)
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Rb/Sr (2)
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U/Pb (1)
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geologic age
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Cenozoic
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Quaternary
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Pleistocene
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upper Pleistocene (1)
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Tertiary
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Neogene
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Miocene (1)
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Pliocene (1)
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Paleogene
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Eocene (1)
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Oligocene (2)
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Mesozoic
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Cretaceous
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Kuskokwim Group (1)
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Lower Cretaceous (1)
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Middle Cretaceous (2)
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Upper Cretaceous (1)
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Jurassic
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Triassic
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MIS 5 (1)
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Paleozoic
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Devonian
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Precambrian
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upper Precambrian
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Proterozoic
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Neoproterozoic (1)
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igneous rocks
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igneous rocks
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volcanic rocks
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andesites (1)
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basalts (1)
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metamorphic rocks
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metamorphic rocks
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metasedimentary rocks (1)
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skarn (1)
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metavolcanic rocks (1)
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minerals
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arsenates (1)
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carbonates
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calcite (3)
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dolomite (3)
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hydrotalcite (1)
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magnesite (1)
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smithsonite (3)
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oxides
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hydroxides
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phosphates (1)
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sulfates (1)
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sulfides
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galena (2)
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pyrite (1)
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sphalerite (3)
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Primary terms
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absolute age (5)
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Africa
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Central Africa
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Congo (1)
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East Africa
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Zambia (1)
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Southern Africa
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Namibia (2)
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Asia
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Arabian Peninsula
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Yemen (3)
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Australasia
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Australia
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Western Australia (1)
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-
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Canada
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Western Canada
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British Columbia (1)
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Canadian Cordillera (1)
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carbon
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C-13/C-12 (2)
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Cenozoic
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Quaternary
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Pleistocene
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upper Pleistocene (1)
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Tertiary
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Neogene
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Miocene (1)
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Pliocene (1)
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Paleogene
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Eocene (1)
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Oligocene (2)
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Chordata
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Vertebrata
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Tetrapoda
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Mammalia
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Theria
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Eutheria
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Artiodactyla
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Suiformes
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Suidae (1)
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crust (1)
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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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diagenesis (1)
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economic geology (1)
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Europe
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Central Europe
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Poland
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Upper Silesia (1)
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-
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Southern Europe
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Iberian Peninsula
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Spain
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Andalusia Spain
-
Donana National Park (1)
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Huelva Spain (1)
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-
-
-
Italy
-
Lombardy Italy
-
Bergamo Italy (1)
-
-
Sardinia Italy (1)
-
-
-
-
geochemistry (3)
-
ichnofossils (1)
-
igneous rocks
-
volcanic rocks
-
andesites (1)
-
basalts (1)
-
-
-
Invertebrata
-
Mollusca
-
Cephalopoda
-
Ammonoidea (1)
-
-
-
-
isotopes
-
radioactive isotopes
-
Pb-206/Pb-204 (2)
-
Pb-207/Pb-204 (2)
-
Pb-208/Pb-204 (2)
-
-
stable isotopes
-
C-13/C-12 (2)
-
O-18/O-16 (2)
-
Pb-206/Pb-204 (2)
-
Pb-207/Pb-204 (2)
-
Pb-208/Pb-204 (2)
-
Sr-87/Sr-86 (3)
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-
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lava (1)
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magmas (1)
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Mesozoic
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Cretaceous
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Kuskokwim Group (1)
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Lower Cretaceous (1)
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Middle Cretaceous (2)
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Upper Cretaceous (1)
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Jurassic
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Upper Jurassic
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Tithonian (1)
-
-
-
Triassic
-
Upper Triassic
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Carnian (1)
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-
-
-
metal ores
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base metals (1)
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cobalt ores (1)
-
copper ores (2)
-
lead ores (8)
-
lead-zinc deposits (8)
-
polymetallic ores (1)
-
silver ores (1)
-
zinc ores (10)
-
-
metals
-
alkaline earth metals
-
strontium
-
Sr-87/Sr-86 (3)
-
-
-
cobalt (1)
-
lead
-
Pb-206/Pb-204 (2)
-
Pb-207/Pb-204 (2)
-
Pb-208/Pb-204 (2)
-
-
zinc (2)
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metamorphic rocks
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metasedimentary rocks (1)
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metasomatic rocks
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skarn (1)
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metavolcanic rocks (1)
-
-
metasomatism (2)
-
Mexico
-
Chihuahua Mexico (1)
-
Guanajuato Mexico (1)
-
Michoacan Mexico (1)
-
San Luis Potosi Mexico (1)
-
Trans-Mexican volcanic belt (1)
-
-
mineral deposits, genesis (9)
-
mineral exploration (3)
-
North America
-
Chihuahua tectonic belt (1)
-
Gulf Coastal Plain (1)
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North American Cordillera
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Canadian Cordillera (1)
-
-
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oxygen
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O-18/O-16 (2)
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paleoclimatology (1)
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paleoecology (1)
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paleontology (1)
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Paleozoic
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Devonian
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Lower Devonian (1)
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paragenesis (2)
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petroleum
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natural gas (1)
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Precambrian
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upper Precambrian
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Proterozoic
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Neoproterozoic (1)
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sedimentary rocks
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carbonate rocks
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dolostone (1)
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South America
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Peru (3)
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tectonics (2)
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United States
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Alaska
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Nixon Fork Terrane (1)
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Trans-Pecos (1)
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weathering (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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dolostone (1)
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sedimentary structures
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tracks (1)
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Jabali Deposit
Formation of Mississippi Valley–type deposits linked to hydrocarbon generation in extensional tectonic settings: Evidence from the Jabali Zn-Pb-(Ag) deposit (Yemen)
AUTOMATED SCANNING ELECTRON MICROSCOPY (QEMSCAN®)-BASED MINERAL IDENTIFICATION AND QUANTIFICATION OF THE JABALI Zn-Pb-Ag NONSULFIDE DEPOSIT (YEMEN)
Geologic map of western Yemen, with the location of the Jabali deposit (mod...
Plot of δ 13C VPDB vs. δ 18OVSMOW for various carbonates and nonsulfides...
A: 87 Sr/ 86 Sr versus 87 Rb/ 86 Sr correlation diagram showing sphalerit...
Zincian dolomite: A peculiar dedolomitization case?
A: Simplified geological map of western Yemen showing the location of the J...
New Petroleum Development by Petróleos Mexicanos in Northeastern Mexico
Sulfide-associated hydrothermal dolomite and calcite reveal a shallow burial depth for Alpine-type Zn-(Pb) deposits
F ig . 2. Location of nonsulfide zinc deposits. Note that many of the super...
Carbonate-Hosted Nonsulfide Pb-Zn Deposits of the Quesnel Lake District, British Columbia, Canada,
A cold supergene zinc deposit in Alaska: The Reef Ridge case
PALEOECOLOGICAL IMPLICATIONS OF LARGE-SIZED WILD BOAR TRACKS RECORDED DURING THE LAST INTERGLACIAL (MIS 5) AT HUELVA (SW SPAIN)
Classification, Genesis, and Exploration Guides for Nonsulfide Zinc Deposits
The Nonsulfide Zinc Deposit at Accha (Southern Peru): Geological and Mineralogical Characterization
THE MINERALOGY, GEOCHEMISTRY, AND METALLURGY OF COBALT IN THE RHOMBOHEDRAL CARBONATES
Spectral reflectance: preliminary data on a new technique with potential for non-sulphide base metal exploration
Atomistic simulation on mixing thermodynamics of calcite-smithsonite solid solutions
Genesis of the Carbonate-Hosted Tres Marias Zn-Pb-(Ge) Deposit, Mexico: Constraints from Rb-Sr Sphalerite Geochronology and Pb Isotopes
Abstract The Tethyan belt extends throughout the circum-Mediterranean and eastward through Turkey, Iran, and Pakistan to China and Southeast Asia. The belt is characterized by rift zones with bimodal volcanic rocks and thick clastic sedimentary rock fill, passive-margin basins with platform carbonates, and calc-alkaline island-arc volcanic rock sequences. It is known primarily for its copper and gold endowment, but it includes several large and globally significant zinc-lead provinces. These include the Basque-Cantabrian basin (Réocin) in northern Spain, the Atlas zinc-lead district in Morocco, Algeria, and Tunisia, the zinc-lead-silver deposits in the Balkans—including the Trepča district extending south to Macedonia and Greece—the zinc districts in central Anatolia, Turkey, and Iran—such as Angouran and Mehdiabad—and deposits such as Padaeng, in Thailand, and Jinding, in southwestern China. Late Carboniferous to Triassic rifting in northern Gondwana and opening of the Neotethys Ocean marks the commencement of the most significant zinc-lead metallogenic cycle and initiated the break-up of Pangea. Rifting migrated eastward and broad Permian to Cenozoic carbonate shelf and passive-margin basin sequences were deposited. The thick carbonate sequences provided ideal trap settings for MVT deposits, with zinc- and lead-rich mineralizing fluid flow initiated by Cretaceous to Cenozoic inversion, collision, and uplift on the Tethyan margins. High-temperature carbonate-replacement and vein-type mineralization is also associated with magmatically induced hydrothermal activity during the Cenozoic compressional events. Unusual hybrid deposits involved both basinal and magmatic fluid inputs. Subsequent uplift and oxidation has resulted in the development of economically significant nonsulfide zinc deposits throughout the belt.