相关实验视频
Updated: Jul 12, 2026

08:14
Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
概括
地质物理数据表明,氧化物在地球上层地幔深处转化为石榴石. 超深的岩提供了这种转变的证据,支持在400公里地震断裂处的岩转化为生态岩的转变.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 地震学 地震学
背景情况:
- 地质物理模型和实验数据预测火的结构变化越来越深.
- 这些变化包括转化为石榴石和溶解为石榴石.
研究的目的:
- 为了间接验证上层地幔中氧烯-石榴石结构变化的预测.
- 确定石的起源深度及其对地震不连续性的影响.
主要方法:
- 在带有石榴石的氧化石中对欧姆法酸溶液的分析.
- 地质化学分析以确定八面体位点中的条件.
主要成果:
- 在石中合氧化溶解间接支持氧化-石榴石转化预测.
- 石榴石中的条件表明,在300-400公里深处的石起源.
- 这些深度与400公里的地震不连续性保持一致.
结论:
- 超深的异岩提供了证据,证明在地幔过渡区的深度下,烯溶解成石榴石.
- 这些发现支持了400公里地震不连续性的理论,即它代表了石到生态石的相位过渡.
更多相关视频
11:50Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
Published on: June 13, 2015
06:37Analyzing Melts and Fluids from Ab Initio Molecular Dynamics Simulations with the UMD Package
Published on: September 17, 2021
相关概念视频
Deep Sea Microbial Ecology
The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...
Diversity of Archaea IV
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 thermal...
Diversity of Archaea III
Crenarchaeota, a prominent phylum of Archaea, is remarkable for its ability to thrive in extreme environments characterized by high temperatures and acidity. These microorganisms inhabit sulfuric hot springs, volcanic systems, and submarine hydrothermal vents, where temperatures often exceed 100°C. The unique adaptations of Crenarchaeota not only allow survival under such extreme conditions but also provide insights into the mechanisms of life in primordial Earth-like environments.Morphological...