Terrestrial Rare Gases: Proceedings of the U.S.-Japan Seminar on Rare Gas Abundance and Isotopic Constraints on the Origin and Evolution of the Earth’s Atmosphere: Advances in Earth and Planetary Sciences, cartea 3
Editat de E.C. Alexander Jr., M. Ozimaen Limba Engleză Paperback – 18 apr 2012
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Specificații
ISBN-13: 9789401098304
ISBN-10: 9401098301
Pagini: 244
Ilustrații: 242 p.
Dimensiuni: 178 x 254 x 13 mm
Greutate: 0.43 kg
Ediția:Softcover reprint of the original 1st ed. 1978
Editura: SPRINGER NETHERLANDS
Colecția Springer
Seria Advances in Earth and Planetary Sciences
Locul publicării:Dordrecht, Netherlands
ISBN-10: 9401098301
Pagini: 244
Ilustrații: 242 p.
Dimensiuni: 178 x 254 x 13 mm
Greutate: 0.43 kg
Ediția:Softcover reprint of the original 1st ed. 1978
Editura: SPRINGER NETHERLANDS
Colecția Springer
Seria Advances in Earth and Planetary Sciences
Locul publicării:Dordrecht, Netherlands
Public țintă
ResearchCuprins
Experimental Studies.- A Mantle Helium Component in Circum-Pacific Volcanic Gases: Hakone, the Marianas, and Mt. Lassen.- Nitrogen to Argon Ratio in Volcanic Gases.- Rare Gas Abundance Pattern of Fumarolic Gases in Japanese Volcanic Areas.- A Review: Some Recent Advances in Isotope Geochemistry of Light Rare Gases.- Abundances and Isotopic Compositions of Rare Gases in Granites and Thucholites.- Rare Gas Isotopic Compositions in Diamonds.- Rare Gases in Mantle-Derived Rocks and Minerals.- A Comparison of Terrestrial and Meteoritic Noble Gases.- The Composition and History of the Martian Atmosphere.- Theoretical Studies.- Nuclear Components in the Atmosphere.- Trapped Xenon and Cosmic-Ray Effects in Meteorites, in Lunar Sample, and in the Earth’s Materials.- Classification and Generation of Terrestrial Rare Gases.- Earth-Atmosphere Evolution Model Based on Ar Isotopic Data.- Terrestrial Potassium and Argon Abundances as Limits to Models of Atmospheric Evolution.- On the Ambient Mantle 4He/40Ar Ratio and the Coherent Model of Degassing of the Earth.- Earth Degassing Models, and the Heterogeneous vs. Homogeneous Mantle.- Lead Isotope Constraints on the Early History of the Earth.- Matter Accretion into the Solar System.