中部和下部地的近同热条件是由融化迁移引起的
Gabriela V Depine1, Christopher L Andronicos, Jason Phipps-Morgan
1Department of Earth and Atmospheric Sciences, Snee Hall, Cornell University, Ithaca, New York 14853, USA. gvd2@cornell.edu
Nature
|March 7, 2008
概括
长期存在的冥土主义产生了准稳定状态的地热,导致高温变形和地削弱. 这种热结构解释了观测到的orogens的变形条件,并影响了随后的地质过程,如挖掘.
科学领域:
- 地质物理学 地质物理学
- 变态石器学 变态石器学
- 构造学 构造学 构造学 构造学
背景情况:
- 地的热结构对于地质过程如变态和浮动主义至关重要.
- 标准的地热梯度模型与来自高温变态地形的观测相冲突.
研究的目的:
- 开发结合融化迁移的热模型,以解释观察到的地热结构.
- 调查浮动主义对地热和变态条件的影响.
主要方法:
- 开发简单的单维热模型.
- 将化迁移和脱水化反应纳入模型.
主要成果:
- 模型预测准稳态地热与快速上层地加热和中下层地同热条件.
- 由于融化导致的上升热引力驱动了颗粒岩和安达卢石-西利曼石的变形.
- 高温和中下层地的无氧化导致地削弱和引力崩.
结论:
- 融化迁移和浮动主义显著改变地的热结构,为特定的变形面形成条件.
- 模拟的准稳定状态地热与从挖掘出来的orogenic带的观察结合了理论预测.
- 通过脱水融反应进行的热缓冲在塑造地热和促进地变形方面发挥着关键作用.
相关概念视频
Bonding in Metals
57.0K
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”.
57.0K
Phase Transitions: Melting and Freezing
15.7K
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...
15.7K
Isothermal Processes
5.4K
A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
5.4K
Temperature Dependent Deformation
670
In a nonhomogeneous rod made up of steel and brass, restrained at both ends and subjected to a temperature change, several steps are involved in calculating the stress and compressive load. Due to the problem's static indeterminacy, one end support is disconnected, allowing the rod to experience the temperature change freely. Next, an unknown force is applied at the free end, triggering deformations in the rod's steel and brass portions. These deformations are then calculated and added...
670
Solid–Solid Solutions
108
The temperature-composition phase diagram of two solids, A and B, which are immiscible in the solid phase but form miscible liquids, shows that when the temperature is low, these two exist as separate, pure solids (A and B). As the temperature increases, they transition into a single-phase liquid solution where A and B coexist. Moving from point a1 to a2 in the phase diagram, the composition changes such that solid B begins to separate from the solution, enriching the remaining liquid with A.
108
Diversity of Archaea IV
611
Hyperthermophilic archaea are a group of extremophiles thriving at temperatures above 80°C, often in hydrothermal vents and volcanic soils where conditions surpass the boiling point of water. At such temperatures, proteins, membranes, and DNA in most organisms degrade, but hyperthermophiles have evolved remarkable adaptations to maintain stability and function.Unique Cellular FeaturesHyperthermophilic membranes are composed of a monolayer of biphytanyl tetraether lipids, which resist...
611


