高解像度石層の粘度と磁電流画像による動態
1Department of Geology, University of Illinois at Urbana-Champaign, Champaign, IL 61820, USA. ljliu@illinois.edu.
まとめ
地球の動態を理解するために不可欠な 石層の粘度を示しています この方法は地形とマントルの上流を正確にモデル化し,実験室での実験よりも優れた制約を提供します.
科学分野:
- 地理学
- 地力学
- 地球科学
背景:
- 地力学的プロセスをモデル化するには正確な石層粘度が不可欠です.
- 以前の粘度測定方法には限界がある.
研究 の 目的:
- マグネトテルリック (MT) データを用いて効果的石層粘度を推論する.
- 地力学モデリングで推測された粘度を検証する.
主な方法:
- アメリカ合衆国西部における高解像度磁電図 (MT) 調査.
- 電気抵抗性による粘度構造の近似.
- 推論された粘度を含む地力学モデリング.
主要な成果:
- 短波の地表の予測に成功しました
- リトスフィアの変形とマントルの上流の正確なモデリング.
- 粘度制限は,実験室ベースのレオロギーよりも優れています.
結論:
- MTイメージングは,石層粘度を制限するための実用的なツールです.
- このアプローチは,大陸の石層のダイナミクスの理解を高めます.
- 電気抵抗は機械的な強さの 信頼できる代用として機能する.
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