Diamonds and water in the deep Earth: a new scenario

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Hydration-reduced lattice thermal conductivity of olivine in Earth's upper mantle.Inclusions in super-deep diamonds: windows on the very deep Earth

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Diamonds and water in the deep Earth: a new scenario

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wetenschappelijk artikel

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наукова стаття, опублікована в червні 2015

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Diamonds and water in the deep Earth: a new scenario

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Diamonds and water in the deep Earth: a new scenario

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Diamonds and water in the deep Earth: a new scenario

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Diamonds and water in the deep Earth: a new scenario

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Diamonds and water in the deep Earth: a new scenario

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Diamonds and water in the deep Earth: a new scenario

@nl

P1476

Diamonds and water in the deep Earth: a new scenario

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P2093

Joseph R. Smyth

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Solubility of water in the α, β and γ phases of (Mg,Fe) 2 SiO 4

Vapour undersaturation in primitive mid-ocean-ridge basalt and the volatile content of Earth's upper mantle.

Whole-mantle convection and the transition-zone water filter.

Hydrous mantle transition zone indicated by ringwoodite included within diamond.

Mineralogy. Discovery of bridgmanite, the most abundant mineral in Earth, in a shocked meteorite.

Water in Earth's lower mantle.

Earth's interior. Dehydration melting at the top of the lower mantle.

Water content in the transition zone from electrical conductivity of wadsleyite and ringwoodite.

Carbon, hydrogen and nitrogen in carbonaceous chondrites: abundances and isotopic compositions in bulk samples.

Olivine water contents in the continental lithosphere and the longevity of cratons.

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263-276

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scholarly article

P356

10.1080/00206814.2015.1056758

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P433

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

P478

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Fabrizio Nestola

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2015-06-25T00:00:00Z

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Diamonds and water in the deep Earth: a new scenario

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P2860

P2860

Diamonds and water in the deep Earth: a new scenario

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P1433

P1476

P2093

P2860

P304

P31

P356

P433

P478

P50

P577

P356

P1433

P1476

P2093

P2860

P304

P31

P356

P433

P478

P50

P577