地球地幔的固化不可避免地导致了基底岩海洋
Charles-Édouard Boukaré1,2, James Badro3, Henri Samuel3
1Université Paris Cité, Institut de Physique du Globe de Paris, CNRS, Paris, France. boukare@yorku.ca.
Nature
|March 27, 2025
概括
地球地幔的早期演化是由富含铁的融体从较轻的固体中分离出来的,形成了基底性岩海洋. 这种从上到下发生的过程解释了古代岩石的地化学特征.
科学领域:
- 地质学
- 星球科学
- 地质化学
背景情况:
- 地球地幔的深层地质结构通常被解释为早期岩海洋的固化.
- 一个关键的争论是,这种固化是从下而上还是从上而下发生的.
研究的目的:
- 研究地幔演变的驱动机制和基本岩海洋的形成.
- 模拟原始地化学储库的组成特征和空间分布.
主要方法:
- 使用多相流体动力学方法对地幔固化的数值建模.
- 融化阶段关系和地化学模型的整合.
主要成果:
- 密集,富含铁的融物从较轻的固体中分离,驱动了地幔的演变,不论曲线和地热交叉点如何.
- 铁氧化物丰富的融体聚集在核心上方, 形成基底岩海洋.
- 显著的固体形成发生在行星表面,而不是在深处.
结论:
- 这项研究支持地球早期地幔的自上而下的固化模型.
- 浅层的酸盐分离将地化学特征注入深层地幔.
- 这一框架有助于重新研究早期的行星演化,地幔动力学,石化学和地化学.
相关概念视频
Classifying Matter by State
72.8K
Chemistry is the study of matter and the changes it undergoes. Matter is anything that has mass and occupies space. Matter is all around us; the air, water, soil, mountains, even our bodies are all examples of matter. Matter is divided into three states — solid, liquid, and gas — that are commonly found on earth. The fourth state of matter, plasma, occurs naturally in the interiors of stars.
72.8K
Phase Transitions: Melting and Freezing
12.2K
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...
12.2K
States of Water
50.4K
Water exists in any one of the three classical states: solid (ice), liquid (water), and gas (steam or water vapor). The state of water depends on i) the intermolecular forces that draw molecules together and ii) the kinetic energy that leads to movements that pull them apart.
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
50.4K
Magnetostatic Boundary Conditions
847
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...
847
Phase Transitions: Sublimation and Deposition
16.6K
Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
16.6K
Bonding in Metals
45.8K
Metallic bonds are formed between two metal atoms. A simplified model to describe metallic bonding has been developed by Paul Drüde called the “Electron Sea Model”.
45.8K


