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U-series dating of travertines provides an opportunity to unravel paleohydrologic and neotectonic histories near the southeastern edge of the Colorado Plateau. This interdisciplinary study combines water and gas chemistry data, travertine morphology and geochronology, analysis of geologic structures, basalt geochronology, and river incision studies to formulate an integrative model for both travertine formation and for landscape evolution of this region. This area is at the intersection of the southeastern edge of the Colorado Plateau with the Jemez lineament, a northeast-trending zone of volcanic activity over the last 4. Johns Dome, a faulted asymmetric anticline trapping a large natural CO2 reservoir.
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Plates vs Plumes: A Geological Controversy 1, Gillian R. Foulger - alterna180.com

Why does 4He act like a boson but 3He doesn't? What accounts for their different behavior at low temperatures? Why does 4He act as a Bose Condensate, but 3He doesn't? I read somewhere that because 4He has an even number of fermions 2 protons, 2 neutrons, 2 electrons , it behaves as a boson. What is the physical origins of this statement? Can someone please help?
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We examine their superconductive transition properties and other detector functions. A second function we fulfill is the testing of our cold hardware in the cryostat. The study of cryogenics is more than a century old, dating back to the end of the 19th century. The application, however, of cryogenic technology to other fields of science and commerce only dates back to the 's.
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An alternative explanation for the Hf-Nd mantle array. Crust-mantle interaction inferred from the petrology and Sr-Nd-Pb isotope geochemistry of Eocene arc lavas from the Kahrizak Mountains, north-central Iran. These volcanic rocks, similar to those from eastern Pontides and northern Anatolia, Turkey, were mainly produced during the Eocene magmatic flare-up associated with the Arabia-Eurasia convergence. Their normalized trace element concentration patterns are moderately enriched in light rare earth element and depleted in high field-strength elements HFSE; e.
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