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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Bear River basin (1)
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Europe
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Western Europe
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United Kingdom
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Great Britain
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England (1)
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Scotland
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Perthshire Scotland (1)
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North America
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Basin and Range Province (1)
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South America
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Andes (1)
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United States
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Arizona
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Pima County Arizona (1)
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Oklahoma
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Utah
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commodities
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hydrogen (1)
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C-14 (2)
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stable isotopes
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He-3 (2)
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Ne-21 (3)
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Sm-147/Nd-144 (1)
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metals
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Pu-244 (1)
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thorium (2)
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uranium (1)
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alkaline earth metals
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beryllium
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Be-10 (5)
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Be-7 (2)
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aluminum
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Al-26 (2)
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iron
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Fe-60 (1)
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platinum group
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iridium (1)
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rare earths
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neodymium
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samarium
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Sm-147/Nd-144 (1)
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noble gases
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argon
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Ar-38 (1)
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helium
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neon
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radon
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geologic age
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Mesozoic
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igneous rocks
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Primary terms
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carbon
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Tertiary
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Neogene
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Earth (1)
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Europe
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land use (1)
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metal ores
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metals
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actinides
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Pu-244 (1)
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thorium (2)
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uranium (1)
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alkaline earth metals
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beryllium
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Be-10 (5)
-
Be-7 (2)
-
-
-
aluminum
-
Al-26 (2)
-
-
iron
-
Fe-60 (1)
-
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platinum group
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iridium (1)
-
-
rare earths
-
neodymium
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Sm-147/Nd-144 (1)
-
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samarium
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Sm-147/Nd-144 (1)
-
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-
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meteorites
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stony meteorites
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achondrites
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diogenite (1)
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eucrite (1)
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HED meteorites (1)
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howardite (1)
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lunar meteorites (1)
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ureilite (1)
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chondrites
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mineral deposits, genesis (1)
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Moon (3)
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noble gases
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argon
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Ar-36 (1)
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Ar-38 (1)
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helium
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neon
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radon
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Rn-222 (1)
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North America
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Basin and Range Province (1)
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ocean floors (1)
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sediments
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underground installations (1)
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sediments
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sediments
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clastic sediments
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marine sediments (1)
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-
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soils
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soils
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forest soils (1)
-
-
cosmic rays
The Dust, Atmosphere, and Plasma at the Moon
4. NOBLE GASES IN TERRESTRIAL ROCKS
Space history of the High Possil and Strathmore meteorites from Ne and Ar isotopes
Abstract The existing controversy regarding the climatic response to given changes in the geomagnetic field intensity (e.g. climate cooling or warming in periods of geomagnetic field strengthening) raises scepticism about the existence of any relationship between both variables. The main shortcomings of the recent understanding of the geomagnetic field–climate relationship are the expectations for: (i) its universal character over the globe; and (ii) the zonal homogeneity of this relationship. This paper offers a new conceptual framework aimed at resolving the existing controversy and explaining the mechanism for the appearance of geomagnetic footprints on climatic records. We show that particles trapped in the Earth's radiation belts are subject to geomagnetic lensing in the parts of their trajectories closest to the surface, being focused or defocused at different regions over the world. The irregularly distributed ionization, created in such a way near the tropopause, activates various ion–molecular reactionships which affect the atmospheric composition there. Thus, the regional changes in the ozone and water vapour are furthermore projected onto the surface temperature and pressure. Consequently, the geomagnetic field–climate relationship is not a rigid but, rather, a flexible one because it is mediated by the near-tropopause ionization, ozone and humidity, with each of them being subject to the other's influence.
From Cosmic Explosions to Terrestrial Fires? A Discussion
From Cosmic Explosions to Terrestrial Fires? A Reply
Chapter 18 Radon gas hazard
Abstract Radon ( 222 Rn) is a natural radioactive gas that occurs in rocks and soils and can only be detected with special equipment. Radon is a major cause of lung cancer. Therefore, early detection is essential. The British Geological Survey and Public Health England have produced a series of maps showing radon affected areas based on underlying geology and indoor radon measurements, which help to identify radon-affected buildings. Many factors influence how much radon accumulates in buildings. Remedial work can be undertaken to reduce its passage into homes and workplaces and new buildings can be built with radon preventative measures.