作为核心-地幔边界的超低速度区域的来源,起的带状铁层构成
David P Dobson1, John P Brodholt
1Department of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, UK. d.dobson@ucl.ac.uk
Nature
|March 18, 2005
概括
在地球上超低速度区域 (ULVZs).
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 地球科学 地球科学 地球科学
背景情况:
- 超低速区 (ULVZs) 是核心-地幔边界的独特区域,其特点是地震波速度降低和密度增加.
- 关于ULVZ起源的现有假设包括酸融化池,核心-地幔反应和核心沉积.
- 这些区域厚度约为1-10公里,压缩波速度降低10-20%,剪切波速度降低10-30%.
研究的目的:
- 为超低速区 (ULVZ) 提出一个新的来源.
- 为了研究潜水带铁构成的潜水带铁构成作为ULVZ的来源的潜力.
- 解释ULVZ观察到的地震和密度特征.
主要方法:
- 地质学假设的制定.
- 对带状铁层构成的组成和沉积环境的分析.
- 模拟核-地幔边界的降温过程和材料行为.
主要成果:
- 由氧化铁和二氧化组成的带状铁构成,沉积在古代海洋中.
- 这些构造,当潜入时,可以到达核心-地幔边界.
- 沉积带状铁层的特性与观察到的ULVZ特征一致.
结论:
- 压缩带状铁形构造代表了超低速区 (ULVZ) 的合理起源.
- 这种假设可能解释了ULVZ中观察到的地震和密度异常.
- 拟议的机制将古代地球过程与当今的深层地幔结构联系起来.
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
09:45Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
Published on: July 24, 2016
相关概念视频
Isothermal Processes
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...
Magnetostatic Boundary Conditions
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...
Magnetic Susceptibility and Permeability
In linear magnetic materials, like paramagnets and diamagnets, magnetization is proportional to the magnetic field intensity. The constant of proportionality, a dimensionless number, is called magnetic susceptibility. The value of the susceptibility depends on the type of material.
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...
Sulfur Assimilation
Sulfur is an essential element in biological systems, contributing to synthesizing key biomolecules, including amino acids such as cysteine and methionine, and cofactors such as coenzyme A and biotin. Microorganisms primarily assimilate sulfur as sulfate (SO₄²⁻) from the environment, which must undergo a series of biochemical transformations before it can be incorporated into cellular components. As sulfate is highly oxidized, it must undergo assimilatory sulfate reduction to become...
Microbial Mats
Microbial communities forming biofilms and mats represent complex, spatially structured ecosystems where metabolic processes are stratified according to light, oxygen, and nutrient gradients. Biofilms are initial colonization stages, only a few millimeters thick, while mature microbial mats can reach centimeter-scale thickness and display intricate vertical organization. Their structural and functional heterogeneity allows microorganisms to occupy distinct ecological niches within a few...
Microbes and Other Elemental Cycles
Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
