The influence of Al on the stability region of DHMS and water transports into the Earth's interior
The influence of Al on the stability region of DHMS and water transports into the Earth's interior
批准号:
18J12511
负责人:
徐 超文
金额:
$1.22万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for JSPS Fellows
财政年份:
2018
资助国家:
日本
项目状态:
已结题
起止时间:
2018-04-25 至 2020-03-31
中文摘要
(1)在14 ~ 25 GPa的MgO-Al2O3-SiO2-H2O体系中,研究了富al致密水合硅酸镁D相(PhD)在900℃~ 1500℃下的稳定性。富al的PhD在地幔过渡带压力下分解为Egg相,在上、下地幔压力下随着温度升高分解为δ-AlOOH相。广阔的含铝PhD稳定区是地幔过渡带中水的重要储藏点。(2)在900℃-1500℃条件下,研究了MgO-Al2O3-FeO-SiO2-H2O (MAFSH)体系中水欠饱和(2 wt%)模拟物在15 ~ 21 GPa范围内的相关系。结果表明,在15 ~ 16.5 GPa和1050℃以下,与瓦德利石或环伍德石共存的E相至少稳定;当压力高于16.5 GPa、温度低于1100℃时,D相与环伍德石共存。(3)在本研究中,我们确定了aloh - feooh二元体系在15-25 GPa和700℃-1200℃下的相关系。x射线衍射测量表明,δ-AlOOH和ε-FeOOH在较宽的压力和温度范围内部分形成固溶体。结果表明,在1200℃和20gpa下,在不脱水和不熔化的情况下,形成了二元共晶图。我们的研究结果表明,俯冲到深部地幔的cacl2型氢氧化物在很大的组成范围内形成了固溶体。到目前为止,我已经发表了三篇论文。我们将在几个月后再处罚三篇论文。
英文摘要
(1) We investigated the stability of the Al-rich dense hydrous magnesium silicate Phase D (PhD) in a MgO-Al2O3-SiO2-H2O system between 14 and 25 GPa at 900℃-1,500 ℃. Al-rich PhD decomposes to Phase Egg at pressure of the mantle transition zone, whereas it decomposes to δ-AlOOH phase with a temperature increase at pressure of the uppermost lower mantle.The wide stability region of Al-bearing PhD would contribute an important storage site for water in the mantle transition zone.(2)We investigated the phase relation of a water-undersaturated (2 wt%) analog of Martian mantle in simplified MgO-Al2O3-FeO-SiO2-H2O (MAFSH) system between 15 and 21 GPa at 900℃-1500 °C . Results showed that phase E coexisting with wadsleyite or ringwoodite was at least stable at 15-16.5 GPa and below 1050 °C. Phase D coexisted with ringwoodite at pressures higher than 16.5 GPa and temperatures below 1100 °C.(3) In this study, we ascertain the phase relations in the AlOOH-FeOOH binary system at 15-25 GPa and 700℃-1200 °C. X-ray diffraction measurements of quenched samples show that δ-AlOOH and ε-FeOOH partly form solid solutions over wide pressure and temperature ranges. Our results demonstrate that a binary eutectic diagram is formed without dehydration or melting below 1200 °C at 20 GPa. Our results suggest that the CaCl2-type hydroxides subducted into the deep mantle form a solid solution over a wide composition range.Until now, I have published three papers. We will punlish three more papers a few months later.
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Melting phase relation of Fe-bearing PhD up to the uppermost lower mantle and transportation of H2O to the deep Earth
含铁PhD到最上层下地幔的熔化相关系以及H2O向地球深处的输送
DOI:
--
发表时间:
2018
期刊:
影响因子:
--
作者:
[Chaowen Xu, Toru Inoue]
通讯作者:
Toru Inoue
DOI:
10.3390/min9090559
发表时间:
2019-09
期刊:
Minerals
影响因子:
2.5
作者:
[Chaowen Xu;T. Inoue]
通讯作者:
Chaowen Xu;T. Inoue
Effect of Al on stability of DHMS up to the uppermost lower mantle
Al 对 DHMS 直至最上层下地幔稳定性的影响
DOI:
--
发表时间:
2017
期刊:
影响因子:
--
作者:
[Xu, C., Inoue, T.]
通讯作者:
T.
DOI:
10.1029/2019gc008476
发表时间:
2019-09
期刊:
Geochemistry
影响因子:
3.7
作者:
[Chaowen Xu;T. Inoue]
通讯作者:
Chaowen Xu;T. Inoue
Solubility behavior of δAlOOH-εFeOOH at high pressures: Implication for water transports into the deep lower mantle and early Mars’interior
δAlOOH-εFeOOH在高压下的溶解度行为:对水输送到下地幔深处和早期火星内部的意义
DOI:
--
发表时间:
2019
期刊:
影响因子:
--
作者:
[Xu Chaowen, Inoue Toru, Chaowen Xu and Toru Inoue]
通讯作者:
Chaowen Xu and Toru Inoue
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