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Updated: May 1, 2026

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
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地質物理および地化学の証拠は,深層の温度変動が,中海の山脊の下にあることを示しています

Colleen A Dalton1, Charles H Langmuir, Allison Gale

  • 1Department of Earth and Environment, Boston University, 685 Commonwealth Avenue, Boston, MA 02215, USA.

Science (New York, N.Y.)
|April 5, 2014
PubMed
まとめ

地球のマントルの温度変動は250°Cを超え,深さは400kmを超え,マントルのコンベクションと海洋流域の深さに影響を与えます. この研究は,地震データ,山脊の深さ,玄武岩の組成を統合して,地球温暖化パターンを明らかにしています.

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