Results 281 to 290 of about 66,103 (324)

Decoupling of high-pressure H2 production from serpentinization and magnetite in subduction zones

Siron G, Blanchard M, Aufort J, Williams S, Vitale-Brovarone A.   +4 more
europepmc   +1 more source

Lithological discrimination based on Landsat-9 OLI sensor and field observation data: The bana an-orogenic volcano-plutonic ring complex, West Cameroon line. [PDF]

Heliyon
Mohamed R, Tamen J, Ousmanou S, Yangouo FK, Nkouathio D.   +4 more
europepmc   +1 more source

Laboratory spectra of amorphous and crystalline olivine: An application to comet Halley IR spectrum

, 1990
A Blanco, V Orofino, E Bussoletti, S Fonti, L. Colangelí, John Stephens   +5 more
openalex  

Does the direct effect of friction increase continuously with absolute temperature? [PDF]

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

Slab melting boosts the mantle wedge contribution to Li-rich magmas. [PDF]

Sci Rep
Schettino E, González-Pérez I, Marchesi C, González-Jiménez JM, Grégoire M, Tilhac R, Gervilla F, Blanco-Quintero IF, Corgne A, Schilling ME.   +9 more
europepmc   +1 more source

Olivine alteration and the loss of Mars' early atmospheric carbon. [PDF]

Sci Adv
Murray J, Jagoutz O.
europepmc   +1 more source

A closer look into the structure and magnetism of the recently fallen meteorite Ribbeck. [PDF]

Sci Rep
Kołodziej M, Michalska D, Załęski K, Iatsunskyi I, Muszyński A, Coy E.   +5 more
europepmc   +1 more source

Fundamental constraints and questions from the study of martian meteorites and the need for returned samples. [PDF]

Proc Natl Acad Sci U S A
Udry A, Ostwald AM, Day JMD, Hallis LJ.
europepmc   +1 more source

Dense hydrated Mg-silicates in diamond: Implications for transport of H₂O into the mantle. [PDF]

Sci Adv
Carvalho LDV, Stachel T, Luth RW, Locock AJ, Pearson DG, Steele-MacInnis M, Stern RA, Nestola F, Scholz R, Jalowitzki T, Fuck RA.   +10 more
europepmc   +1 more source

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Nickel–manganese variability in olivine and Al‐in‐olivine thermometry for olivine‐phyric shergottites

Meteoritics & Planetary Science, 2021
AbstractOlivine‐phyric shergottites represent primitive Martian magmas, but they commonly contain excess olivine and rarely represent primary mantle melts. Olivine chemistry, however, tracks magma evolution and preserves information on the original parent magma composition.
Sierra Ramsey, Arya Udry, Geoffrey H. Howarth, Geoffrey H. Howarth, Juliane Gross, Juliane Gross, Juliane Gross, Kevin Righter   +7 more
openaire   +2 more sources