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Updated: Apr 13, 2026

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

Published on: June 13, 2015

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上層マントルの謎めいた条紋は,インド南東部のの玄武岩のハフニウムイソトープによって明らかになった

D W Graham1, J Blichert-Toft, C J Russo

  • 1College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97331, USA. dgraham@coas.oregonstate.edu

Nature
|March 10, 2006
PubMed
まとめ

古代の組成線が地球の上層マントルに存在し,インド南東部のの玄武岩でバイモダルのハフニウム同位体分布によって明らかにされています. このマントルの線条は,厚さ約40キロメートルである.

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