Results 211 to 220 of about 24,591 (277)

Melt-bearing nodules from Tenerife reveal magma reservoir diversity prior to caldera-forming eruptions. [PDF]

Contrib Mineral Petrol
Horn EL, Taylor RN, Gernon TM, Stock MJ, Schofield KE, Brown RJ, Smith VC, McLean D.   +7 more
europepmc   +1 more source

Building wet planets through high-pressure magma-hydrogen reactions. [PDF]

Nature
Horn HW, Vazan A, Chariton S, Prakapenka VB, Shim SH.   +4 more
europepmc   +1 more source

The role of C-O-H-F-Cl fluids in the making of Earth's continental roots. [PDF]

Nat Commun
Gibson SA, Jackson CJ, Crosby JC, Day JAF.   +3 more
europepmc   +1 more source

Discovery of a heavy silicon isotope mantle reservoir. [PDF]

Natl Sci Rev
Liu MR, Wang J, Cui ZX, Wei GJ, Yang Q, Xu YG, Kerr AC, Wyman D, Bai JH, Zhu GH, Ma L, Hao LL, Zhou JS, Fan JJ, Huang TY, Zhang MY, Wang Q.   +16 more
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Evaluation of Matrix Effects in SIMS Using Gaussian Process Regression: The Case of Olivine Mg Isotope Microanalysis. [PDF]

Rapid Commun Mass Spectrom
Itano K, Fukuda K, Kita NT, Ueki K, Kuwatani T, Akaho S.   +5 more
europepmc   +1 more source

A Low-Background, High-Flatness Mounting Method for In Situ SIMS Isotopic Analysis for Fine-Grained Samples. [PDF]

Anal Chem
Gao YB, Hao JL, Zhou Z, He HC, Tang GQ, Hu S, Yang W, Lin YT.   +7 more
europepmc   +1 more source

Connecting Meteorite Spectra to Lunar Surface Composition Using Hyperspectral Imaging and Machine Learning

Hesar FF, Raouf M, Chegeni A, Soltani P, Foing B, Chatzitheodoridis E, de Dood MJ, Verbeek FJ.   +7 more
europepmc   +1 more source

Experimental evidence supporting a long-lived magma layer at the Martian core–mantle boundary

Pierru R, Gréaux S, Dominijanni S, Man L, Kono Y, Kakizawa S, Higo Y, Badro J, Frost D, Antonangeli D.   +9 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 R. Ramsey, Geoffrey H. Howarth, Arya Udry, Juliane Gross   +3 more
openaire   +1 more source