Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

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Viscosity jump in the lower mantle inferred from melting curves of ferropericlase.Perovskite in Earth's deep interior.Valence and spin states of iron are invisible in Earth's lower mantle.

P2860

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P2860

Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

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http://www.wikidata.org/entity/Q48325598

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2017 nî lūn-bûn

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2017年の論文

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2017年学术文章

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2017年学术文章

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2017年学术文章

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name

Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

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Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

@nl

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Item

label

Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

@en

Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

@nl

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Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

@en

Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

@nl

P1476

Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

@en

P2093

Brent Grocholski

http://www.w3.org/2001/XMLSchema#string

Dane Morgan

http://www.w3.org/2001/XMLSchema#string

E Ercan Alp

http://www.w3.org/2001/XMLSchema#string

Shenzhen Xu

http://www.w3.org/2001/XMLSchema#string

Vitali B Prakapenka

http://www.w3.org/2001/XMLSchema#string

Yu Ye

http://www.w3.org/2001/XMLSchema#string

Yue Meng

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P2860

Subducted slabs stagnant above, penetrating through, and trapped below the 660 km discontinuity

Anomalous compressibility of ferropericlase throughout the iron spin cross-over

Spin transition zone in Earth's lower mantle.

A perovskitic lower mantle inferred from high-pressure, high-temperature sound velocity data.

Double-sided laser heating system at HPCAT for in situ x-ray diffraction at high pressures and high temperatures.

Spin and valence dependence of iron partitioning in Earth's deep mantle.

Evidence for a Fe3+-rich pyrolitic lower mantle from (Al,Fe)-bearing bridgmanite elasticity data.

Broad plumes rooted at the base of the Earth's mantle beneath major hotspots.

Viscosity jump in Earth's mid-mantle.

Preliminary reference Earth model

P304

6468-6473

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scholarly article

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10.1073/PNAS.1614036114

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P407

English

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P478

114

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P50

Sang-heon Shim

P577

2017-06-05T00:00:00Z

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28584106

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P932

5488914

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Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

about

P2860

P2860

Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.

description

name

type

label

prefLabel

P1433

P1476

P2093

P2860

P304

P31

P356

P407

P433

P478

P50

P577

P698

P932

P356

P1433

P1476

P2093

P2860

P304

P31

P356

P407

P433

P478

P50

P577

P698

P932