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Format
Article Type
Journal
Publisher
Section
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
-
Altiplano (43)
-
Asia
-
Far East
-
Indonesia (1)
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Lesser Sunda Islands
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Timor (1)
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Taiwan (1)
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-
-
Atlantic Ocean
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South Atlantic
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Southwest Atlantic (1)
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-
-
Central America (2)
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Cordillera de la Costa (3)
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Europe
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Alps
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Eastern Alps (1)
-
-
Southern Europe
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Italy
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Apennines
-
Central Apennines (1)
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-
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-
-
Malay Archipelago
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Timor (1)
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Mexico
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Sierra Madre Occidental (1)
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North America
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Basin and Range Province
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Great Basin (1)
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Rocky Mountains
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Southern Rocky Mountains (1)
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Oceania
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Melanesia
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New Caledonia (1)
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Pacific Ocean
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East Pacific
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East Pacific Rise (1)
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Peru-Chile Trench (1)
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Southeast Pacific
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Nazca Ridge (1)
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-
-
North Pacific
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Northwest Pacific (1)
-
-
South Pacific
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Southeast Pacific
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Nazca Ridge (1)
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-
Southwest Pacific
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Banda Sea (1)
-
-
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West Pacific
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Indonesian Seas
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Banda Sea (1)
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Northwest Pacific (1)
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Southwest Pacific
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Banda Sea (1)
-
-
-
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Pacific region (1)
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Puna (34)
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Rio Grande Valley (1)
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South America
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Amazon Basin (1)
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Andes
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Argentine Andes (2)
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Central Andes (216)
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Cordillera Real (2)
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Eastern Cordillera (27)
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Northern Andes (2)
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Patagonian Andes (1)
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Southern Andes (5)
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Subandean Belt (5)
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Western Cordillera (15)
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Argentina
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Argentine Andes (2)
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Catamarca Argentina (1)
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Jujuy Argentina (5)
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La Pampa Argentina (1)
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Mendoza Argentina (2)
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Neuquen Argentina (4)
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Neuquen Basin (5)
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Pampean Mountains (8)
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Salta Argentina (7)
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San Juan Argentina (4)
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Bolivia
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Oruro Bolivia (2)
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Potosi Bolivia (2)
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Brazil
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Brazilian Shield (1)
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Chile
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Antofagasta Chile
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Socompa (1)
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Atacama Chile (1)
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Atacama Desert (3)
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Tarapaca Chile (2)
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Colombia
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Magdalena Valley (1)
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Ecuador (4)
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Lake Titicaca (1)
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Paraguay (1)
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Patagonia
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Patagonian Andes (1)
-
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Peru
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Arequipa Peru (1)
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Lima Peru (1)
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Puno Peru (1)
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Precordillera (7)
-
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United States
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Alaska
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Aleutian Islands (1)
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Great Basin (1)
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Nevada (1)
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New Mexico
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Datil-Mogollon volcanic field (1)
-
-
Utah (1)
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-
-
commodities
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borate deposits (1)
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brines (5)
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ceramic materials (1)
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construction materials (1)
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energy sources (1)
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evaporite deposits (2)
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geothermal energy (1)
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industrial minerals (1)
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metal ores
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antimony ores (1)
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base metals (3)
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bismuth ores (1)
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copper ores (22)
-
gold ores (9)
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IOCG deposits (2)
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iron ores (2)
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lead ores (3)
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lead-zinc deposits (2)
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manganese ores (1)
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molybdenum ores (8)
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polymetallic ores (5)
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silver ores (6)
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tin ores (10)
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tungsten ores (2)
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zinc ores (2)
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mineral deposits, genesis (25)
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mineral exploration (5)
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mineral resources (5)
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nitrate deposits (1)
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oil and gas fields (1)
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petroleum (3)
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elements, isotopes
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boron
-
B-11/B-10 (1)
-
-
carbon
-
C-13/C-12 (2)
-
C-14 (4)
-
-
chemical ratios (2)
-
halogens
-
chlorine
-
chloride ion (1)
-
-
iodine (1)
-
-
hydrogen
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D/H (3)
-
tritium (1)
-
-
isotope ratios (30)
-
isotopes
-
radioactive isotopes
-
Be-10 (2)
-
C-14 (4)
-
Cs-137 (1)
-
Pb-206/Pb-204 (12)
-
Pb-207/Pb-204 (10)
-
Pb-208/Pb-204 (10)
-
Pb-210 (1)
-
tritium (1)
-
-
stable isotopes
-
B-11/B-10 (1)
-
C-13/C-12 (2)
-
D/H (3)
-
Fe-56/Fe-54 (1)
-
He-4/He-3 (1)
-
Hf-177/Hf-176 (1)
-
Nd-144/Nd-143 (14)
-
O-17/O-16 (1)
-
O-18/O-16 (8)
-
Pb-206/Pb-204 (12)
-
Pb-207/Pb-204 (10)
-
Pb-208/Pb-204 (10)
-
S-34/S-32 (2)
-
Sr-87/Sr-86 (18)
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-
-
large-ion lithophile elements (1)
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metals
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alkali metals
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cesium
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Cs-137 (1)
-
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rubidium (1)
-
-
alkaline earth metals
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barium (1)
-
beryllium
-
Be-10 (2)
-
-
magnesium (1)
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strontium
-
Sr-87/Sr-86 (18)
-
-
-
hafnium
-
Hf-177/Hf-176 (1)
-
-
iron
-
Fe-56/Fe-54 (1)
-
-
lead
-
Pb-206/Pb-204 (12)
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Pb-207/Pb-204 (10)
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Pb-208/Pb-204 (10)
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Pb-210 (1)
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mercury (1)
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niobium (1)
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precious metals (1)
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rare earths
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dysprosium (1)
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europium (1)
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lanthanum (2)
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neodymium
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Nd-144/Nd-143 (14)
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terbium (1)
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ytterbium (1)
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yttrium (2)
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-
tantalum (1)
-
titanium (1)
-
-
noble gases
-
helium
-
He-4/He-3 (1)
-
-
-
oxygen
-
O-17/O-16 (1)
-
O-18/O-16 (8)
-
-
sulfur
-
S-34/S-32 (2)
-
-
trace metals (1)
-
-
fossils
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Notoungulata (2)
-
-
-
-
-
-
-
ichnofossils (1)
-
Invertebrata
-
Arthropoda
-
Mandibulata
-
Crustacea
-
Ostracoda (1)
-
-
-
-
Mollusca
-
Bivalvia (1)
-
Cephalopoda
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Ammonoidea (1)
-
-
Gastropoda (1)
-
-
Protista
-
Foraminifera (1)
-
-
-
microfossils (2)
-
palynomorphs
-
miospores
-
pollen (1)
-
-
-
Plantae
-
algae
-
diatoms (1)
-
-
-
-
geochronology methods
-
(U-Th)/He (6)
-
Ar/Ar (15)
-
exposure age (1)
-
fission-track dating (10)
-
K/Ar (13)
-
Nd/Nd (1)
-
paleomagnetism (4)
-
Rb/Sr (2)
-
Re/Os (1)
-
Sm/Nd (2)
-
tephrochronology (2)
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Th/U (1)
-
thermochronology (10)
-
U/Pb (24)
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U/Th/Pb (1)
-
-
geologic age
-
Cenozoic
-
lower Cenozoic (1)
-
Quaternary
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Holocene
-
lower Holocene (1)
-
upper Holocene (1)
-
-
Pleistocene
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middle Pleistocene (1)
-
upper Pleistocene (4)
-
-
upper Quaternary (1)
-
-
Tertiary
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lower Tertiary (1)
-
Neogene
-
Miocene
-
lower Miocene (4)
-
middle Miocene (3)
-
upper Miocene (9)
-
-
Pliocene
-
lower Pliocene (2)
-
-
-
Paleogene
-
Eocene
-
middle Eocene (1)
-
upper Eocene (1)
-
-
Oligocene
-
lower Oligocene (1)
-
upper Oligocene (2)
-
-
Paleocene
-
lower Paleocene (2)
-
-
-
upper Tertiary (1)
-
-
upper Cenozoic (7)
-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Agrio Formation (1)
-
-
Middle Cretaceous (2)
-
Upper Cretaceous
-
Maestrichtian (1)
-
Senonian (1)
-
Turonian (1)
-
-
-
Jurassic
-
Lower Jurassic (1)
-
Middle Jurassic (2)
-
Upper Jurassic (2)
-
-
middle Mesozoic (1)
-
Triassic
-
Lower Triassic (2)
-
Middle Triassic (1)
-
-
upper Mesozoic (1)
-
Vaca Muerta Formation (1)
-
-
Paleozoic
-
Cambrian
-
Lower Cambrian (1)
-
-
Carboniferous (2)
-
Devonian (2)
-
Ordovician
-
Lower Ordovician
-
Arenigian (1)
-
Tremadocian (1)
-
-
-
Permian
-
Middle Permian (1)
-
Upper Permian (1)
-
-
Silurian (2)
-
-
Phanerozoic (2)
-
Precambrian
-
upper Precambrian
-
Proterozoic
-
Neoproterozoic (1)
-
-
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
diorites
-
tonalite (1)
-
-
granites
-
A-type granites (1)
-
I-type granites (1)
-
monzogranite (2)
-
S-type granites (3)
-
-
granodiorites (3)
-
ultramafics
-
peridotites (1)
-
pyroxenite (1)
-
-
-
porphyry (1)
-
volcanic rocks
-
andesites (9)
-
basalts
-
flood basalts (1)
-
mid-ocean ridge basalts (2)
-
shoshonite (1)
-
-
dacites (3)
-
glasses
-
volcanic glass (5)
-
-
pyroclastics
-
ignimbrite (16)
-
pumice (5)
-
tuff (3)
-
-
rhyodacites (1)
-
rhyolites (4)
-
trachyandesites (1)
-
-
-
ophiolite (2)
-
volcanic ash (4)
-
-
metamorphic rocks
-
metamorphic rocks
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eclogite (1)
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gneisses (1)
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granulites (1)
-
metaigneous rocks
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metabasite (1)
-
-
metasedimentary rocks (5)
-
metasomatic rocks
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greisen (1)
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skarn (2)
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-
mylonites (1)
-
schists
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glaucophane schist (1)
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-
slates (1)
-
-
ophiolite (2)
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turbidite (1)
-
-
minerals
-
alloys (1)
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borates
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colemanite (1)
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hydroboracite (1)
-
-
carbonates
-
calcite (1)
-
-
halides
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chlorides
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halite (1)
-
-
-
minerals (1)
-
oxides
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hematite (1)
-
iron oxides (3)
-
magnetite (3)
-
-
phosphates
-
apatite (12)
-
-
silicates
-
chain silicates
-
amphibole group
-
clinoamphibole
-
glaucophane (1)
-
hornblende (1)
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pargasite (1)
-
-
-
-
framework silicates
-
feldspar group
-
alkali feldspar
-
K-feldspar (1)
-
sanidine (1)
-
-
plagioclase
-
albite (1)
-
-
-
silica minerals
-
quartz (2)
-
-
-
orthosilicates
-
nesosilicates
-
garnet group (2)
-
olivine group
-
olivine (1)
-
-
titanite group
-
titanite (1)
-
-
zircon group
-
zircon (17)
-
-
-
sorosilicates
-
epidote group
-
epidote (1)
-
-
-
-
ring silicates
-
tourmaline group (2)
-
-
sheet silicates
-
chlorite group
-
chlorite (3)
-
-
clay minerals
-
smectite (2)
-
-
illite (1)
-
mica group
-
biotite (4)
-
muscovite (3)
-
paragonite (1)
-
-
-
-
sulfates
-
anhydrite (1)
-
gypsum (3)
-
-
sulfides
-
chalcocite (1)
-
molybdenite (1)
-
-
-
Primary terms
-
absolute age (49)
-
Asia
-
Far East
-
Indonesia (1)
-
Lesser Sunda Islands
-
Timor (1)
-
-
Taiwan (1)
-
-
-
Atlantic Ocean
-
South Atlantic
-
Southwest Atlantic (1)
-
-
-
boron
-
B-11/B-10 (1)
-
-
brines (5)
-
carbon
-
C-13/C-12 (2)
-
C-14 (4)
-
-
Cenozoic
-
lower Cenozoic (1)
-
Quaternary
-
Holocene
-
lower Holocene (1)
-
upper Holocene (1)
-
-
Pleistocene
-
middle Pleistocene (1)
-
upper Pleistocene (4)
-
-
upper Quaternary (1)
-
-
Tertiary
-
lower Tertiary (1)
-
Neogene
-
Miocene
-
lower Miocene (4)
-
middle Miocene (3)
-
upper Miocene (9)
-
-
Pliocene
-
lower Pliocene (2)
-
-
-
Paleogene
-
Eocene
-
middle Eocene (1)
-
upper Eocene (1)
-
-
Oligocene
-
lower Oligocene (1)
-
upper Oligocene (2)
-
-
Paleocene
-
lower Paleocene (2)
-
-
-
upper Tertiary (1)
-
-
upper Cenozoic (7)
-
-
Central America (2)
-
ceramic materials (1)
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Notoungulata (2)
-
-
-
-
-
-
-
clay mineralogy (1)
-
climate change (9)
-
construction materials (1)
-
crust (48)
-
data processing (7)
-
deformation (33)
-
diagenesis (2)
-
earthquakes (4)
-
ecology (1)
-
economic geology (12)
-
energy sources (1)
-
engineering geology (1)
-
epeirogeny (1)
-
Europe
-
Alps
-
Eastern Alps (1)
-
-
Southern Europe
-
Italy
-
Apennines
-
Central Apennines (1)
-
-
-
-
-
evaporite deposits (2)
-
faults (41)
-
folds (10)
-
foliation (2)
-
foundations (1)
-
fractures (1)
-
geochemistry (30)
-
geochronology (11)
-
geodesy (1)
-
geomorphology (17)
-
geophysical methods (18)
-
geothermal energy (1)
-
ground water (4)
-
heat flow (2)
-
hydrogen
-
D/H (3)
-
tritium (1)
-
-
hydrology (2)
-
ichnofossils (1)
-
igneous rocks
-
plutonic rocks
-
diorites
-
tonalite (1)
-
-
granites
-
A-type granites (1)
-
I-type granites (1)
-
monzogranite (2)
-
S-type granites (3)
-
-
granodiorites (3)
-
ultramafics
-
peridotites (1)
-
pyroxenite (1)
-
-
-
porphyry (1)
-
volcanic rocks
-
andesites (9)
-
basalts
-
flood basalts (1)
-
mid-ocean ridge basalts (2)
-
shoshonite (1)
-
-
dacites (3)
-
glasses
-
volcanic glass (5)
-
-
pyroclastics
-
ignimbrite (16)
-
pumice (5)
-
tuff (3)
-
-
rhyodacites (1)
-
rhyolites (4)
-
trachyandesites (1)
-
-
-
inclusions
-
fluid inclusions (6)
-
-
industrial minerals (1)
-
intrusions (25)
-
Invertebrata
-
Arthropoda
-
Mandibulata
-
Crustacea
-
Ostracoda (1)
-
-
-
-
Mollusca
-
Bivalvia (1)
-
Cephalopoda
-
Ammonoidea (1)
-
-
Gastropoda (1)
-
-
Protista
-
Foraminifera (1)
-
-
-
isostasy (2)
-
isotopes
-
radioactive isotopes
-
Be-10 (2)
-
C-14 (4)
-
Cs-137 (1)
-
Pb-206/Pb-204 (12)
-
Pb-207/Pb-204 (10)
-
Pb-208/Pb-204 (10)
-
Pb-210 (1)
-
tritium (1)
-
-
stable isotopes
-
B-11/B-10 (1)
-
C-13/C-12 (2)
-
D/H (3)
-
Fe-56/Fe-54 (1)
-
He-4/He-3 (1)
-
Hf-177/Hf-176 (1)
-
Nd-144/Nd-143 (14)
-
O-17/O-16 (1)
-
O-18/O-16 (8)
-
Pb-206/Pb-204 (12)
-
Pb-207/Pb-204 (10)
-
Pb-208/Pb-204 (10)
-
S-34/S-32 (2)
-
Sr-87/Sr-86 (18)
-
-
-
land use (1)
-
lava (11)
-
lineation (1)
-
magmas (30)
-
Malay Archipelago
-
Timor (1)
-
-
mantle (13)
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Agrio Formation (1)
-
-
Middle Cretaceous (2)
-
Upper Cretaceous
-
Maestrichtian (1)
-
Senonian (1)
-
Turonian (1)
-
-
-
Jurassic
-
Lower Jurassic (1)
-
Middle Jurassic (2)
-
Upper Jurassic (2)
-
-
middle Mesozoic (1)
-
Triassic
-
Lower Triassic (2)
-
Middle Triassic (1)
-
-
upper Mesozoic (1)
-
Vaca Muerta Formation (1)
-
-
metal ores
-
antimony ores (1)
-
base metals (3)
-
bismuth ores (1)
-
copper ores (22)
-
gold ores (9)
-
IOCG deposits (2)
-
iron ores (2)
-
lead ores (3)
-
lead-zinc deposits (2)
-
manganese ores (1)
-
molybdenum ores (8)
-
polymetallic ores (5)
-
silver ores (6)
-
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Central Andes
Mesozoic to Cenozoic deformation of the western Central Andes: an update from structural and U–Pb data of the Calama Basin and surrounding areas Available to Purchase
Eocene exhumation of the High Andes at ~30°S differentiated by detrital multimethod U-Pb-He thermochronology Available to Purchase
Pleistocene deformation of the Malargüe fold–thrust belt from structural modelling and geochronology of syntectonic sedimentation Available to Purchase
Tin Mineralization in the Triassic Chacaltaya District (Cordillera Real, Bolivia) Traced by In Situ Chemical and δ 18 O-δ 11 B Compositions of Tourmaline Available to Purchase
A Model for the Lithospheric Architecture of the Central Andes and the Localization of Giant Porphyry Copper Deposit Clusters Available to Purchase
Crustal structure of the Lazufre volcanic complex and the Southern Puna from 3-D inversion of magnetotelluric data: Implications for surface uplift and evidence for melt storage and hydrothermal fluids Open Access
Rhyolitic melt production in the midst of a continental arc flare-up—The heterogeneous Caspana ignimbrite of the Altiplano-Puna volcanic complex of the Central Andes Open Access
Controls of the Lithospheric Thermal Field of an Ocean-Continent Subduction Zone: The Southern Central Andes Open Access
Kinematic evolution of the central Andean retroarc thrust belt in northwestern Argentina and implications for coupling between shortening and crustal thickening Available to Purchase
Emplacement conditions and exhumation of the Varvarco Tonalite and associated plutons from the Cordillera del Viento, Southern Central Andes Available to Purchase
What drives Fe depletion in calc-alkaline magma differentiation: Insights from Fe isotopes Available to Purchase
Tectonic and paleoclimatic controls on the composition of inland wetland deposits, Chaco foreland basin, Central Andes Available to Purchase
Detrital zircon record of Phanerozoic magmatism in the southern Central Andes Open Access
Pliocene–Pleistocene landscape evolution and watershed reorganization east of the central Andes in Argentine Patagonia Available to Purchase
ABSTRACT Uplift of the central Andes during the Miocene was followed by large-scale reorganization of Atlantic-draining rivers in Argentine Patagonia. Here, we document the abandonment of one large river in the late Pliocene and the establishment of the modern drainage in the Early Pleistocene. A chronology for these events is provided by 40 Ar/ 39 Ar ages on basalt flows. Remnants of the Pliocene paleovalley system are well preserved in the Lago Cardiel–Gobernador Gregores area, where they are eroded into flat-lying basalt flows dated from ca. 13.9 Ma to 8.6 Ma. Younger basalts that erupted onto the abandoned floor of the paleovalley are as young as 3.7 Ma. Abandonment of the Pliocene paleovalley and establishment of the modern Río Chico and Río Shehuen catchments happened near the close of the Pliocene when Andean glaciers incised the east-sloping pediment on which the late Miocene drainage was established. Lago Cardiel sits within a large endorheic basin that is inset into the late Pliocene paleovalley. The basin began to develop just before 4 Ma, after the paleovalley was abandoned. It became larger and deeper during the Pleistocene due to mass movements along its margins, deflation of the basin floor during times when Lago Cardiel was dry or nearly dry, and possibly lowering along bounding faults. The Pliocene–Pleistocene landscape and drainage changes that we have documented are not unique to the Lago Cardiel–Gobernador Gregores area; similar changes are apparent elsewhere in Patagonia east of the crest of the Andes.
Lithospheric Structure of the Central Andes Forearc from Gravity Data Modeling: Implication for Plate Coupling Open Access
Case Study: Reconstructing the 2015 Dulcepamba River Flood Disaster Available to Purchase
Geological development of the Timor Orogen Available to Purchase
Abstract The Timor Orogen comprises the island of Timor, a narrow offshore area to the north and a wider offshore fold-and-thrust belt to the south. This orogen formed by jamming and subsequent collision of the Banda Sea subduction system by the Australian Plate. The BandaSeis seismic survey has revealed excellent images of the deep-water fold-and-thrust belt. Seismic interpretation of the dataset demonstrated structural and tectonic features not previously described, including regional geological features on the Australian continental crust and two regional NE–SW sinistral strike-slip faults, and a prominent Middle Permian palaeogeographical high (Timor Plateau). Moreover, since the Middle–Late Triassic and Middle Jurassic, the two NE-trending strike-slip faults governed the formation of the West Timor and Cova-Lima sub-basins. The location along the Australian margin plays a dominant role in controlling the structural style and shaping of the Timor Orogen. Vertical loading and the southerly motion of the orogenic wedge are the main driving forces responsible for its building, illustrating a thin-skinned tectonic framework. Thrust faults nucleate in a forward-breaking sequence in the motion of thrust transport, with younger thrusts developing in front of older thrusts. Most of the collisional deformation has been classified into two styles: shallow thin-skinned and deep-seated deformation.