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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Morocco
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Asia
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Central Asia
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Kazakhstan
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Kustanay Kazakhstan (1)
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Chukotka Russian Federation
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Chukchi Peninsula (1)
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Far East
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China
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Hunan China (1)
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Okhotsk-Chukchi volcanic belt (1)
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Russian Far East (1)
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Russian Pacific region (1)
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Sakhalin Russian Federation
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Kuril Islands
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Kunashir Island (1)
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Canada
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Eastern Canada
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Ontario
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Gowganda Ontario (1)
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Timiskaming District Ontario (1)
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Western Canada
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British Columbia (1)
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Clara Mine (1)
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Commonwealth of Independent States
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Kazakhstan
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Russian Federation
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Chukotka Russian Federation
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Chukchi Peninsula (1)
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Okhotsk-Chukchi volcanic belt (1)
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Russian Far East (1)
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Russian Pacific region (1)
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Sakhalin Russian Federation
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Kuril Islands
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Europe
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Central Europe
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Germany
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Odenwald (2)
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Mexico
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Moctezuma Mexico (1)
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Sonora Mexico (3)
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Zacatecas Mexico (1)
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North America
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Canadian Shield
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Superior Province
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Abitibi Belt (1)
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South America
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Argentina
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Pampean Mountains (1)
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San Luis Argentina (1)
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Chile
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Peru
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United States
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Idaho
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commodities
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barite deposits (1)
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fluorspar deposits (1)
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metal ores
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copper ores (2)
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gold ores (7)
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lead ores (2)
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lead-zinc deposits (1)
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polymetallic ores (1)
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silver ores (10)
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zinc ores (2)
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elements, isotopes
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antimony (1)
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arsenic (1)
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copper (2)
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germanium (2)
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indium (1)
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mercury (2)
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lanthanum (1)
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silver (6)
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selenium (1)
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tellurium (1)
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geologic age
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Cenozoic
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Tertiary
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Neogene
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Mesozoic
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igneous rocks
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igneous rocks
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volcanic rocks (1)
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skarn (1)
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minerals
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alloys
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electrum (1)
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arsenides
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gersdorffite (1)
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carbonates
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kutnohorite (1)
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rhodochrosite (1)
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halides
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melilite group
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sulfides
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galena (5)
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gersdorffite (1)
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pyrite (1)
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cylindrite (1)
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sulfantimonites
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polybasite (19)
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sulfarsenites
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pearceite (25)
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tennantite (2)
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sulfobismuthites
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berryite (1)
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galenobismutite (1)
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matildite (1)
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tellurides
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calaverite (1)
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hessite (1)
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tungstates
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ferberite (1)
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scheelite (1)
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uranium minerals (1)
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Primary terms
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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Anti-Atlas (1)
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Morocco
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Moroccan Atlas Mountains
-
Anti-Atlas (1)
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-
-
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Asia
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Central Asia
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Kazakhstan
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Kustanay Kazakhstan (1)
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Chukotka Russian Federation
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Chukchi Peninsula (1)
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Far East
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China
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Hunan China (1)
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-
-
Okhotsk-Chukchi volcanic belt (1)
-
Russian Far East (1)
-
Russian Pacific region (1)
-
Sakhalin Russian Federation
-
Kuril Islands
-
Kunashir Island (1)
-
-
-
-
barite deposits (1)
-
Canada
-
Eastern Canada
-
Ontario
-
Gowganda Ontario (1)
-
Timiskaming District Ontario (1)
-
-
-
Western Canada
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British Columbia (1)
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Cenozoic
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Tertiary
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Neogene
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Miocene (2)
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Pliocene (1)
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crystal chemistry (9)
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crystal growth (3)
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crystal structure (12)
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crystallography (1)
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data processing (1)
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economic geology (1)
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Europe
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Central Europe
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Black Forest (1)
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Germany
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Baden-Wurttemberg Germany (1)
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Odenwald (2)
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faults (1)
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fluorspar deposits (1)
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geochemistry (1)
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igneous rocks
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volcanic rocks (1)
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inclusions
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fluid inclusions (2)
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Mesozoic
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Cretaceous
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Upper Cretaceous (1)
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metal ores
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copper ores (2)
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gold ores (7)
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lead ores (2)
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lead-zinc deposits (1)
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polymetallic ores (1)
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silver ores (10)
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zinc ores (2)
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metals
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antimony (1)
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arsenic (1)
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copper (2)
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germanium (2)
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indium (1)
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mercury (2)
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precious metals (2)
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rare earths
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lanthanum (1)
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silver (6)
-
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metamorphic rocks
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metasomatic rocks
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skarn (1)
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-
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Mexico
-
Moctezuma Mexico (1)
-
Sonora Mexico (3)
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Zacatecas Mexico (1)
-
-
mineral deposits, genesis (8)
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mineral exploration (1)
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mineralogy (1)
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minerals (2)
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North America
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Canadian Shield
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Superior Province
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Abitibi Belt (1)
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paragenesis (2)
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petrology (1)
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phase equilibria (2)
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Precambrian
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Archean (1)
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selenium (1)
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South America
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Argentina
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Pampean Mountains (1)
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San Luis Argentina (1)
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Santa Cruz Argentina
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Deseado Massif (1)
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-
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Chile
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Atacama Chile
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Copiapo Chile (2)
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Peru
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Ayacucho Peru (1)
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-
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tellurium (1)
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United States
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Idaho
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Owyhee County Idaho (1)
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-
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weathering (1)
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pearceite
First occurrence of the M 2 a 2 b 2 c polytype of argentopolybasite, [Ag 6 Sb 2 S 7 ][Ag 10 S 4 ]: Structural adjustments in the Cu-free member of the pearceite–polybasite group
Ferrofettelite, [Ag 6 As 2 S 7 ][Ag 10 FeAs 2 S 8 ], a new sulfosalt from the Glasberg quarry, Odenwald, Germany
The Ag- and Au-bearing phases in the Escondida epithermal vein, Cerro Moro deposit, Santa Cruz, Argentina
Physicochemical Conditions of Formation of Gold and Silver Parageneses at the Valunistoe Deposit (Chukchi Peninsula)
Unusual Mineral Diversity in a Hydrothermal Vein-type Deposit: the Clara Mine, SW Germany, as a Type Example
Enrichment in critical metals (In-Ge) and Te-Se in epithermal deposits of the ‘La Carolina’ district, San Luis, Argentina
The three-dimensional periodic nature of crystalline structures was so strongly anchored in the minds of scientists that the numerous indications that seemed to question this model struggled to acquire the status of validity. The discovery of aperiodic crystals, a generic term including modulated, composite and quasicrystal structures, started in the 1970s with the discovery of incommensurately modulated structures and the presence of satellite reflections surrounding the main reflections in the diffraction patterns. The need to use additional integers to index such diffractograms was soon adopted and theoretical considerations showed that any crystal structure requiring more than three integers to index its diffraction pattern could be described as a periodic object in a higher dimensional space, i.e. superspace, with dimension equal to the number of required integers. The structure observed in physical space is thus a three-dimensional intersection of the structure described as periodic in superspace. Once the symmetry properties of aperiodic crystals were established, the superspace theory was soon adopted in order to describe numerous examples of incommensurate crystal structures from natural and synthetic organic and inorganic compounds even to proteins. Aperiodic crystals thus exhibit perfect atomic structures with long-range order, but without any three-dimensional translational symmetry. The discovery of modulated structures was soon followed by the discovery of composite structures consisting of structural entities with partly independent translations and finally by the discovery of quasicrystals. In recent years, the use of CCD and imaging plate systems improved considerably the sensitivity of data collection for aperiodic structures and in particular modulated structures and, therefore, there was a need for further improvement of the methods. Today, several computer programs are able to solve and refine incommensurately modulated structures using the superspace approach. In nature, it is uncommon to find minerals which have strong and sharp incommensurate satellites that could be used for a higher dimensional refinement. Here we describe several cases of aperiodic minerals (natrite, calaverite, melilite, fresnoite, pearceite–polybasite, cylindrite) including the first examples of natural and stable quasicrystalline structures (icosahedrite and decagonite) which settle beyond doubt any questions which remain about the long-term stability of quasicrystals.