13562680-n 'a geological process in which one edge of a crustal plate is forced sideways and downward into the mantle below another plate';
Definitions
- 日语
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地殻プレートの1つの端がもう一つのプレートの側面と下部に面し、下に大きく押し込まれる地質学的プロセス
- 英语
-
a geological process in which one edge of a crustal plate is forced sideways and downward into the mantle below another plate
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Maintainer:
Francis Bond
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