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NARROW
Format
Article Type
Journal
Publisher
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Southern Africa
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Karoo Basin (1)
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Namibia (1)
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South Africa
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Western Cape Province South Africa (1)
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Antarctica (1)
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Asia
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Far East
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China
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Altyn Tagh Fault (1)
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Xizang China (1)
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Himalayas (1)
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Karakoram (1)
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Tibetan Plateau (1)
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Australasia
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Australia
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South Australia (1)
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Cordillera de la Costa (1)
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Europe
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Alps (1)
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Central Europe
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Austria (1)
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Switzerland (2)
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Western Europe
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France
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Bouches-du-Rhone France (1)
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Provence (1)
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United Kingdom
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Great Britain
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Scotland
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Perthshire Scotland (1)
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Front Range (1)
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North America
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Appalachian Basin (1)
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Great Plains
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Northern Great Plains (1)
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Rocky Mountains
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U. S. Rocky Mountains
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Medicine Bow Mountains (1)
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Platte River basin (1)
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Puna (1)
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South America
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Andes
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Southern Andes (1)
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Argentina (2)
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Chile
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Atacama Desert (1)
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Patagonia (1)
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United States
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Anadarko Basin (1)
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Hugoton Embayment (1)
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Idaho
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Snake River plain (1)
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Kansas
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Hugoton Field (1)
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Nebraska (1)
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New York (1)
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Oklahoma (1)
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Palo Duro Basin (1)
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Texas
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Amarillo Uplift (1)
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Dalhart Basin (1)
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U. S. Rocky Mountains
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commodities
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brines (1)
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oil and gas fields (1)
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petroleum
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natural gas (2)
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elements, isotopes
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carbon
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C-13/C-12 (2)
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C-14 (4)
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halogens
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chlorine
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Cl-36 (5)
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isotope ratios (3)
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isotopes
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radioactive isotopes
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Al-26 (6)
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Ar-38 (1)
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Be-10 (10)
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Be-7 (1)
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C-14 (4)
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Cl-36 (5)
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stable isotopes
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Ar-36 (2)
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Ar-40 (1)
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C-13/C-12 (2)
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He-3 (10)
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He-4 (3)
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Kr-84 (1)
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N-15/N-14 (1)
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Ne-20 (1)
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Ne-21 (22)
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Ne-22/Ne-20 (1)
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metals
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alkaline earth metals
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beryllium
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Be-10 (10)
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Be-7 (1)
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aluminum
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Al-26 (6)
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nitrogen
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N-15/N-14 (1)
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noble gases
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argon
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Ar-36 (2)
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Ar-38 (1)
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Ar-40 (1)
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helium
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He-3 (10)
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He-4 (3)
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krypton
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Kr-84 (1)
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neon
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Ne-20 (1)
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Ne-21 (22)
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Ne-22/Ne-20 (1)
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geochronology methods
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exposure age (12)
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optically stimulated luminescence (1)
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paleomagnetism (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene (2)
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Pleistocene
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upper Pleistocene
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Weichselian
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upper Weichselian
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Younger Dryas (1)
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Tertiary
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Neogene
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Miocene
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Ash Hollow Formation (1)
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middle Miocene (1)
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upper Miocene
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Tortonian (1)
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Pliocene
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upper Pliocene (1)
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Paleogene
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Oligocene (1)
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Mesozoic
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Cretaceous (1)
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Paleozoic
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Carboniferous (1)
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Devonian
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Middle Devonian
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Marcellus Shale (1)
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Upper Devonian
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Canadaway Group (1)
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Ordovician
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Middle Ordovician
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Black River Group (1)
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Trenton Group (1)
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Permian
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Chase Group (1)
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Lower Permian
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Wolfcampian (1)
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Silurian (1)
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Precambrian
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Archean (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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diabase (1)
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metamorphic rocks
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metamorphic rocks
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quartzites (2)
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meteorites
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meteorites
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stony meteorites
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chondrites
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ordinary chondrites
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L chondrites (1)
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LL chondrites (1)
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minerals
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silicates
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framework silicates
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silica minerals
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quartz (1)
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orthosilicates
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nesosilicates
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olivine group
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olivine (1)
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Primary terms
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absolute age (3)
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Africa
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Southern Africa
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Karoo Basin (1)
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Namibia (1)
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South Africa
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Western Cape Province South Africa (1)
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-
-
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Antarctica (1)
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Asia
-
Far East
-
China
-
Altyn Tagh Fault (1)
-
Kunlun Mountains (1)
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Xizang China (1)
-
-
-
Himalayas (1)
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Karakoram (1)
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Tibetan Plateau (1)
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asteroids (1)
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Australasia
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Australia
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South Australia (1)
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-
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brines (1)
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carbon
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C-13/C-12 (2)
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C-14 (4)
-
-
Cenozoic
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Quaternary
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Holocene (2)
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Pleistocene
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upper Pleistocene
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Weichselian
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upper Weichselian
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Younger Dryas (1)
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-
-
-
-
-
Tertiary
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Neogene
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Miocene
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Ash Hollow Formation (1)
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middle Miocene (1)
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upper Miocene
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Tortonian (1)
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-
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Pliocene
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upper Pliocene (1)
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-
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Paleogene
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Oligocene (1)
-
-
-
-
chemical analysis (1)
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climate change (2)
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deformation (1)
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Europe
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Alps (1)
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Central Europe
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Austria (1)
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Switzerland (2)
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Jura Mountains (1)
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Western Europe
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France
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Bouches-du-Rhone France (1)
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Provence (1)
-
-
United Kingdom
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Great Britain
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Scotland
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Perthshire Scotland (1)
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-
-
-
-
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faults (4)
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folds (1)
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geochemistry (1)
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geochronology (8)
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geomorphology (2)
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igneous rocks
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plutonic rocks
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diabase (1)
-
-
-
isotopes
-
radioactive isotopes
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Al-26 (6)
-
Ar-38 (1)
-
Be-10 (10)
-
Be-7 (1)
-
C-14 (4)
-
Cl-36 (5)
-
-
stable isotopes
-
Ar-36 (2)
-
Ar-40 (1)
-
C-13/C-12 (2)
-
He-3 (10)
-
He-4 (3)
-
Kr-84 (1)
-
N-15/N-14 (1)
-
Ne-20 (1)
-
Ne-21 (22)
-
Ne-22/Ne-20 (1)
-
-
-
Mesozoic
-
Cretaceous (1)
-
-
metals
-
alkaline earth metals
-
beryllium
-
Be-10 (10)
-
Be-7 (1)
-
-
-
aluminum
-
Al-26 (6)
-
-
-
metamorphic rocks
-
quartzites (2)
-
-
meteorites
-
stony meteorites
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chondrites
-
ordinary chondrites
-
L chondrites (1)
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LL chondrites (1)
-
-
-
-
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nitrogen
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N-15/N-14 (1)
-
-
noble gases
-
argon
-
Ar-36 (2)
-
Ar-38 (1)
-
Ar-40 (1)
-
-
helium
-
He-3 (10)
-
He-4 (3)
-
-
krypton
-
Kr-84 (1)
-
-
neon
-
Ne-20 (1)
-
Ne-21 (22)
-
Ne-22/Ne-20 (1)
-
-
-
North America
-
Appalachian Basin (1)
-
Great Plains
-
Northern Great Plains (1)
-
-
Rocky Mountains
-
U. S. Rocky Mountains
-
Medicine Bow Mountains (1)
-
-
-
-
oil and gas fields (1)
-
paleoclimatology (3)
-
paleomagnetism (1)
-
Paleozoic
-
Carboniferous (1)
-
Devonian
-
Middle Devonian
-
Marcellus Shale (1)
-
-
Upper Devonian
-
Canadaway Group (1)
-
-
-
Ordovician
-
Middle Ordovician
-
Black River Group (1)
-
-
Trenton Group (1)
-
-
Permian
-
Chase Group (1)
-
Lower Permian
-
Wolfcampian (1)
-
-
-
Silurian (1)
-
-
petroleum
-
natural gas (2)
-
-
plate tectonics (1)
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Precambrian
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Archean (1)
-
-
remote sensing (1)
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sea-level changes (1)
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sedimentary rocks
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chemically precipitated rocks
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evaporites
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salt (1)
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silcrete (1)
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clastic rocks
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conglomerate (2)
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mudstone (1)
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gas shale (1)
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sedimentation (1)
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sediments
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clastic sediments
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alluvium (1)
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boulders (3)
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gravel (1)
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pebbles (1)
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marine sediments (1)
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slope stability (1)
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South America
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Andes
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Southern Andes (1)
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Argentina (2)
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Chile
-
Atacama Desert (1)
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-
Patagonia (1)
-
-
spectroscopy (1)
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tectonics
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neotectonics (4)
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United States
-
Anadarko Basin (1)
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Hugoton Embayment (1)
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Idaho
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Snake River plain (1)
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Kansas
-
Hugoton Field (1)
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Nebraska (1)
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New York (1)
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Oklahoma (1)
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Palo Duro Basin (1)
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Texas
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Amarillo Uplift (1)
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Dalhart Basin (1)
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U. S. Rocky Mountains
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Medicine Bow Mountains (1)
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weathering (1)
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rock formations
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Medina Formation (1)
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sedimentary rocks
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sedimentary rocks
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chemically precipitated rocks
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evaporites
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salt (1)
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silcrete (1)
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clastic rocks
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conglomerate (2)
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mudstone (1)
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gas shale (1)
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sediments
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sediments
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clastic sediments
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alluvium (1)
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boulders (3)
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gravel (1)
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pebbles (1)
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marine sediments (1)
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GeoRef Categories
Era and Period
Epoch and Age
Date
Availability
Ne-21
Dating the late Miocene marine sediments around the southern middle Durance valley (Provence, SE France): new evidences for a Tortonian age
Space history of the High Possil and Strathmore meteorites from Ne and Ar isotopes
Exposure-age data from across Antarctica reveal mid-Miocene establishment of polar desert climate
Origin of helium and nitrogen in the Panhandle–Hugoton field of Texas, Oklahoma, and Kansas, United States
Detrital cosmogenic 21 Ne records decoupling of source-to-sink signals by sediment storage and recycling in Miocene to present rivers of the Great Plains, Nebraska, USA
COSMOGENIC 21 Ne AND 10 Be REVEAL A MORE THAN 2 Ma ALLUVIAL FAN FLANKING THE CAPE MOUNTAINS, SOUTH AFRICA
The Elements Toolkit
CosmoELEMENTS
Cosmogenic Nuclides: Dates and Rates of Earth-Surface Change
Dating Disappearing Ice with Cosmogenic Nuclides
Determining the source and genetic fingerprint of natural gases using noble gas geochemistry: A northern Appalachian Basin case study
SOIL EROSION RATES IN SOUTH AFRICA COMPARED WITH COSMOGENIC 3 HE-BASED RATES OF SOIL PRODUCTION
Multiple slope failures associated with neotectonic activity in the Southern Central Andes (37°–37°30′S), Patagonia, Argentina
Late Pleistocene landscape evolution in south-central Chile constrained by luminescence and stable cosmogenic nuclide dating
Single-grain cosmogenic 21 Ne concentrations in fluvial sediments reveal spatially variable erosion rates
Present denudation rates at selected sections of the South African escarpment and the elevated continental interior based on cosmogenic 3 He and 21 Ne
Exposure dating of boulder and bedrock surfaces with 10 Be, 21 Ne, 26 Al, and 36 Cl allows us to constrain periods of glacier expansion in the European Alps. The age of 155 ka from a boulder of Alpine lithology located in the Jura Mountains (Switzerland) provides a minimum age for pre-LGM (Last Glacial Maximum), more extensive Alpine glaciations. During the LGM, glaciers expanded onto the foreland after 30 ka. By 21.1 ± 0.9 ka deglaciation had begun, and the Rhône Glacier abandoned the outer moraines. The age of 15.4 ± 1.4 ka provides a minimum age for formation of Gschnitz stadial moraines (Austria). They mark the first clear post-LGM readvance of mountain glaciers, when glacier termini were already situated well inside the mountains. Glacier advance at the onset of the Younger Dryas led to formation of Egesen I moraines, dated to 12.2 ± 1.0 ka at the Schönferwall site (Austria) and to 12.3 ± 1.5 ka at the outer moraine at Julier Pass (Switzerland). The age of 11.3 ± 0.9 ka for the inner moraine / rock glacier complex at Julier Pass corroborates the field evidence, which points to a marked increase in rock glacier activity and delayed moraine stabilization during the late Younger Dryas. An early Preboreal glacier advance, larger than the Little Ice Age advance(s) at 10.8 ± 1.0 ka, was recorded at Kartell cirque (Austria). A moraine doublet located a few hundred meters outside the A.D. 1850 moraines in Kromer Valley (Austria) was dated at 8.4 ± 0.7 ka. At least during termination 1, glacier volumes in the Alps varied in tune with climate oscillations, Heinrich event 1, the Younger Dryas cold phase, the Preboreal oscillation, and the 8.2 ka event.
The Himalayas and the Tibetan Plateau were formed as a result of the collision of India and Asia, and provide an excellent opportunity to study the mechanical response of the continental lithosphere to tectonic stress. Geophysicists are divided in their views on the nature of this response, advocating either (1) homogeneously distributed deformation with the lithosphere deforming as a fluid continuum or (2) highly localized deformation with the lithosphere deforming as a system of blocks. The resolution of this issue has broad implications for understanding the tectonic response of continental lithosphere in general. Homogeneous deformation is supported by relatively low decadal, geodetic slip-rate estimates for the Altyn Tagh and Karakorum faults. Localized deformation is supported by high millennial, geomorphic slip rates constrained by both cosmogenic and radiocarbon dating on these faults. Based upon the agreement of rates determined by radiocarbon and cosmogenic dating, the overall linearity of offset versus age correlations, and the plateau-wide correlation of landscape evolution and climate history, the disparity between geomorphic and geodetic slip-rate determinations is unlikely to be due to the effects of surface erosion on the cosmogenic age determinations. Similarly, based upon the consistency of slip rates over various observation intervals, secular variations in slip rate appear to persist no longer than 2000 yr and are unlikely to provide reconciliation. Conversely, geodetic and geomorphic slip-rate estimates on the Kunlun fault, which does not have significant splays or associated thrust faults, are in good agreement, indicating that there is no fundamental reason why these complementary geodetic and geomorphic methods should disagree. Similarly, the geodetic and geomorphic estimates of shortening rates across the northeastern edge of the plateau are in reasonable agreement, and the geomorphic rates on individual thrust faults demonstrate a significant eastward decrease in the shortening rate. This rate decrease is consistent with the transfer of slip from the Altyn Tagh fault to genetically related thrust mountain building at its terminus. Rates on the Altyn Tagh fault suggest a similar decrease in rate, but the current data set is too small to be definitive. Overall, the high, late Pleistocene–Holocene geomorphic slip velocities on the major strike-slip faults of Tibet suggest that these faults absorb as much of India's convergence relative to Siberia as the Himalayan Main Frontal Thrust on the southern edge of the plateau.