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Updated: May 24, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

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Published on: August 5, 2016

大陸の衝突が遅いのは,地形ではなく粘着性マントルの石層による

Marin Kristen Clark1

  • 1Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA. marinkc@umich.edu

Nature
|March 3, 2012
PubMed
まとめ

プレート速度は,プレート境界にある力によって導かれる. 大陸のマントルの石層変形はプレート運動に影響し,インド-ユーラシアの衝突以来,チベットでは恒常的な緊張率を示しています.

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