Results 101 to 110 of about 3,352 (155)

Subcritical cracking and sealing along cleavage planes and subgrain boundaries in plagioclase from the Mado Megamullion oceanic core complex. [PDF]

Sci Rep
Nimura K, Okudaira T, Michibayashi K.
europepmc   +1 more source

Breakup of strong cratonic lithosphere causes extensive magmatism at continental margins. [PDF]

Sci Rep
Wang S, Leng W.
europepmc   +1 more source

The moving mantle beneath Hawaii: A new look at an old bend. [PDF]

Proc Natl Acad Sci U S A
Müller RD.
europepmc   +1 more source

Dissecting the puzzle of tectonic lid regimes in terrestrial planets. [PDF]

Nat Commun
Lyu T, Ballmer MD, Li ZH, Lee MH, Yan J, Wu B, Zhao G.   +6 more
europepmc   +1 more source

Heavy melts, light residues: new research identifies the potential importance of Si isotope fractionation in subducting slabs. [PDF]

Natl Sci Rev
Savage PS.
europepmc   +1 more source

Spin transition in magnesiowüstite and ultralow thermal conduction in ultralow velocity zones. [PDF]

Nat Commun
Hsieh WP, Deschamps F, Tsao YC, Pease A, Dorfman SM, Bausch HJ, Wang F.   +6 more
europepmc   +1 more source

Shock compression of FeOOH and implications for iron-water interactions in super-earth magma oceans. [PDF]

Nat Commun
Zhang Y, Bali K, Dorn C, Ravasio A, Yang H, Pandolfi S, Chen AJ, Wei X, Libon L, Che Q, Zheng D, Boulard E, Benuzzi-Mounaix A, Lee HJ, Galtier E, Czapla NA, Sokaras D, Alonso-Mori R, Gleason AE, Shim SH, Morard G, Mao WL.   +21 more
europepmc   +1 more source

Some of the next articles are maybe not open access.

Related searches:

Melting of MORB at core–mantle boundary

Earth and Planetary Science Letters, 2015
Abstract We investigated the melting properties of natural mid-ocean ridge basalt (MORB) up to core–mantle boundary (CMB) pressures using laser-heated diamond anvil cell. Textural and chemical characterizations of quenched samples were performed by analytical transmission electron microscopy.
Guillaume Fiquet, Julien Siebert, Gopal K Pradhan   +2 more
exaly   +3 more sources

The Core-Mantle Boundary

Scientific American Sp, 1993
The largest compositional discontinuity within the Earth is the core-mantle boundary (CMB), at a depth of 2889 km. This boundary and the adjacent transition zones in the lowermost mantle and outermost core play a critical role in the Earth's thermal and chemical evolution.
Raymond Jeanloz, Thorne Lay
openaire   +1 more source