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Updated: Jul 14, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

コンドライトバリウム,ネオジミウム,サマリウムイソトープの異質性と初期の地球分化

Richard W Carlson1, Maud Boyet, Mary Horan

  • 1Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road, NW, Washington, DC 20015, USA. carlson@dtm.ciw.edu

Science (New York, N.Y.)
|May 26, 2007
PubMed
まとめ

隕石内のバリウム,ネオジミウム,サマリウムの同位体変動は,初期の太陽系への多様な恒星の貢献を明らかにします. この研究は,初期の惑星の分化プロセスが隕石のネオジミウム-142 (142Nd) レベルに影響を与えたことを確認しています.

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Determination of Thermodynamic Properties of Alkaline Earth-liquid Metal Alloys Using the Electromotive Force Technique12:02

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Conditions on Early Earth02:06

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Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
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