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相关概念视频

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.
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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...
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Tidal Forces01:06

Tidal Forces

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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...
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相关实验视频

Updated: Dec 4, 2025

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

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在构造板下部分融化的地震证据

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
概括

部分融化存在于上层地幔的地震低速区 (LVZ),为天气层提供食物. 这种融化率低于0.30%,促进了构造板块的运动和晶体的对齐.

科学领域:

  • 地质学
  • 地幔动力学
  • 地震学

背景情况:

  • 上层地幔的地震低速区 (LVZ) 对板块构造学至关重要,但其起源仍有争议.
  • 现有理论提出部分融化,固态机制或挥发性含量是低地震速度的原因.

研究的目的:

  • 使用剪切减弱和速度模型调查低速度地震区 (LVZ) 的起源.
  • 为了确定LVZ内部分融化的存在和分布.

主要方法:

  • 全球三维剪切衰减模型的解释.
  • 全球三维地震速度模型的解释.

主要成果:

  • 在海洋LVZ内部分融化的证据,在中海山脊,热点和后方弧线区域下方150-200公里.
  • 只有不到0.30%的融化物被困在海洋的LVZ中;在大陆下大部分没有融化物.
  • 融化的度随着板块的速度而增加,特别是在每年3-5厘米之间.

结论:

  • 部分融化是海洋上层地幔的重要组成部分.
  • 融化降低了层粘度,促进了板块的运动和大规模的地幔晶体对齐.

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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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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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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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  • 发现支持融化的作用在板块与地幔脱.