GSTDTAP
项目编号1634422
Aluminous phase at high-pressures & temperatures: Elasticity and Energetics of hydrogen incorporation
Mainak Mookherjee
主持机构Florida State University
项目开始年2015
2015-12-23
项目结束日期2018-06-30
资助机构US-NSF
项目类别Continuing grant
项目经费209314(USD)
国家美国
语种英语
英文摘要Geophysical and geochemical observations provide insights into the physical and chemical states of the Earth's interior. However, only by comparing mineral physics data (physical properties) with geophysical (seismological) observations can we disentangle the thermal state of the deep Earth from its chemistry. Conventionally, as a first order approximation, the Earth's mantle is thought to be composed of a homogenous pyrolite. However, the distinct trace element signatures in mid ocean ridge and ocean island basalts reveal the heterogeneity in the Earth's mantle. Although the scale of the heterogeneity is unknown, it is likely that large regions of the mantle are composed of a depleted harzburgite and enriched crustal fractions. We have limited knowledge of the thermodynamics and physical properties of mineral phases in these subducted crusts at high pressures.

In this proposal, the PI intends to use first principles calculations to investigate how chemistry influences crystal structure, energetics, and elasticity of aluminous mineral phases which are likely to be stabilized in deeply subducted oceanic and continental crusts. He will also investigate the energetics of hydrogen incorporation within these aluminous phases. The results will be relevant for geophysics, mineral-physics, geodynamics, petrology, and geochemistry sub disciplines. The PI will also train undergraduate student/s in Solid Earth Geosciences/Mineral Physics.
来源学科分类Geosciences - Earth Sciences
文献类型项目
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/69026
专题环境与发展全球科技态势
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Mainak Mookherjee.Aluminous phase at high-pressures & temperatures: Elasticity and Energetics of hydrogen incorporation.2015.
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