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関連する概念動画

The Evidence for Evolution02:55

The Evidence for Evolution

46.9K
Genetic variations accumulating within populations over generations give rise to biological evolution. Evolutionary changes can result in the formation of novel varieties and entire new species. These changes are responsible for the diverse forms of life inhabiting the planet. The evidence for evolution suggests that all living organisms descended from common ancestors.
46.9K
Global Climate Change01:50

Global Climate Change

28.2K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
28.2K
Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

14.2K
Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
14.2K
Tidal Forces01:06

Tidal Forces

3.0K
The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to...
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The Fossil Record02:56

The Fossil Record

26.7K
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
26.7K
Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

1.5K
An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
1.5K

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関連する実験動画

Updated: Dec 4, 2025

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

Published on: August 5, 2016

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プレート下部の部分的な融解の地震的証拠

Eric Debayle1, Thomas Bodin2, Stéphanie Durand2

  • 1Univ Lyon, Univ Lyon 1, ENSL, CNRS, LGL-TPE, Villeurbanne, France. Eric.Debayle@ens-lyon.fr.

Nature
|October 22, 2020
PubMed
まとめ

部分的な融解は上層マントルの地震低速度地帯 (LVZ) に存在し,アステノスフィアに供給されます. 0.30%未満の融解は プレート移動と結晶の並び方を 促進します

科学分野:

  • 地理学
  • マントルダイナミクス
  • 地震学

背景:

  • 頂上マントルの地震低速帯 (LVZ) はプレート構造に不可欠ですが,その起源は議論されています.
  • 現存する理論では,部分的な溶解,固体機構,または低地震速度の原因として揮発性成分が提案されています.

研究 の 目的:

  • シーア・アテンチュエーションと速度モデルを用いて,低速度ゾーン (LVZ) の起源を調査する.
  • LVZ内の部分溶融の存在と分布を決定する.

主な方法:

  • グローバル3次元シーア減弱モデルの解釈
  • グローバル3次元地震速度モデルの解釈

主要な成果:

  • 海洋 LVZ の内部の部分的な溶解の証拠は,中海の山脊,ホットスポット,バック・アーチ地域の下の 150 - 200 km までです.
  • 溶融の0.30%未満が海洋のLVZに閉じ込められ,溶融は大陸の下ではほとんど存在しない.
  • 溶融の濃度はプレート速度で増加し,特に3〜5cm/年です.

結論:

  • 部分的な融解は,海洋上のマントルLVZの重要な構成要素です.

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Atom Probe Tomography Analysis of Exsolved Mineral Phases
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Atom Probe Tomography Analysis of Exsolved Mineral Phases

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関連する実験動画

Last Updated: Dec 4, 2025

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
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Atom Probe Tomography Analysis of Exsolved Mineral Phases
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Atom Probe Tomography Analysis of Exsolved Mineral Phases

Published on: October 25, 2019

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  • 溶けるとアステノスフィアの粘度が低下し,板の動きや大規模なマントルの結晶の整列が容易になる.
  • 発見は,マントルからの構造板の分離における 融解の役割を裏付ける.