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Solubility and partitioning of noble gases in anorthite, diopside, forsterite, spinel, and synthetic basaltic melts: Implications for the origin and evolution of terrestrial planet atmospheres.

机译：稀有气体在钙长石，透辉石，镁橄榄石，尖晶石和合成玄武质熔体中的溶解度和分配：对地球行星大气的起源和演化的启示。

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Broadhurst Catherine Leigh.;
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年度 1989
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1. Solubilities of nitrogen and noble gases in silicate melts under various oxygen fugacities: Implications for the origin and degassing history of nitrogen and noble gases in the earth [J] . Miyazaki A., Hiyagon H., Sugiura N., Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society . 2004,第2期

机译：氮气和稀有气体在各种氧气逸度下在硅酸盐熔体中的溶解度：对地球上氮气和稀有气体的起源和除气历史的影响
2. IMPACT REGIMES AND POST-FORMATION SEQUESTRATION PROCESSES: IMPLICATIONS FOR THE ORIGIN OF HEAVY NOBLE GASES IN TERRESTRIAL PLANETS [J] . Olivier Mousis, Jonathan I. Lunine, Jean-Marc Petit, The Astrophysical journal . 2010,第2期

机译：冲击方案和形成后的分离过程：对陆平原重质贵气起源的影响
3. Solubility of CH4 in a synthetic basaltic melt, with applications to atmosphere-magma ocean-core partitioning of volatiles and to the evolution of the Martian atmosphere [J] . Ardia P., Hirschmann M.M., Withers A.C., Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society . 2013,第Null期

机译：CH4在合成玄武岩熔体中的溶解度，应用于大气-岩浆海芯挥发物分配和火星大气演化
4. Solubility and partitioning of noble gases in anorthite, diopside, forsterite, spinel, and synthetic basaltic melts: Implications for the origin and evolution of terrestrial planet atmospheres [D] . Broadhurst, Catherine Leigh. 1989

机译：稀有气体在钙长石，透辉石，镁橄榄石，尖晶石和合成玄武质熔体中的溶解度和分配：对地球行星大气的起源和演化的启示
5. IMPACT REGIMES AND POST-FORMATION SEQUESTRATION PROCESSES: IMPLICATIONS FOR THE ORIGIN OF HEAVY NOBLE GASES IN TERRESTRIAL PLANETS [O] . Olivier Mousis, Jonathan I. Lunine, Jean-marc Petit, 2016

机译：影响制度和后期制作过程：对地球行星中重要气体产生的影响
6. Implications of isotopic signatures of noble gases for the origin and evolution of terrestrial atmospheres [R] . Rao, A. S. P. 1987

机译：贵重气体同位素特征对陆地大气起源和演化的影响

Solubility and partitioning of noble gases in anorthite, diopside, forsterite, spinel, and synthetic basaltic melts: Implications for the origin and evolution of terrestrial planet atmospheres.

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