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フィジーの下には,大量に浸透した石層が残っている証拠があります

W P Chen1, M R Brudzinski

  • 1Department of Geology, University of Illinois, Urbana, IL 61801, USA. w-chen@uiuc.edu

Science (New York, N.Y.)
|June 30, 2001
PubMed
まとめ

トンガ・バック・アークの下の深い地震は,ワダティ・ベニオフ・ゾーンと相互作用する分離したスラブによって説明される. この相互作用によって,原始的なマントルの物質が保存されることがあります.

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