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Updated: May 12, 2026

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

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

Published on: August 5, 2016

死海の下の境界層マントルの流れは,地震性アニソトロピーから推論された変形断層である

Georg Rümpker1, Trond Ryberg, Günter Bock

  • 1GeoForschungsZentrum Potsdam, Telegrafenberg, 14473 Potsdam, Germany. rumpker@gfz-potsdam.de

Nature
|October 3, 2003
PubMed
まとめ

研究者らは,死海変形の底深く,狭い20km幅の鉱物並びのゾーンを発見しました. この地殻下変形は,アフリカプレートとアラビアプレートの間のプレート運動に対応する.

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