Results 141 to 150 of about 1,651 (201)

From early Earth to Enceladus-mineral electrochemistry could drive organic synthesis. [PDF]

Nat Commun
Velling SJ.
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Membrane-free electrochemical production of acid and base solutions capable of processing ultramafic rocks. [PDF]

Nat Commun
Charnay BP, Chen Y, Misleh JW, Wright JG, Agarwal RG, Sauvé ER, Toh WL, Surendranath Y, Kanan MW.   +8 more
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Alteration history of aluminum-rich rocks at Jezero crater, Mars. [PDF]

Commun Earth Environ
Broz AP, Horgan BHN, Bedford C, Royer C, Manelski H, Connell S, Wiens RC, Cardarelli EC, Madariaga JM, Mandon L, Klidaras A, Bramble M, Kathir B, Forni O, Carter J, Dehouck E, Quantin-Nataf C, Johnson JR, Nuñez JI, Hausrath E, Wolf U, Cloutis EA, Beck P, Bell JF, Simon JI, Cousin A.   +25 more
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Three-dimensional thermomechanical modelling beneath Guerrero, Mexico, and its relation to the occurrence of interplate seismic phenomena. [PDF]

Sci Rep
Suenaga N, Yoshioka S, Manea VC, Manea M, Moreno EJ, Ji Y.   +5 more
europepmc   +1 more source

Zircon behavior in the partially melted planetary mantle

Yakimenko A, Borisova A, Fedortchouk Y, Fairhurst L.   +3 more
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Phlogopite from the Horoman Ultramafic Rocks

Phlogopite from the Horoman Ultramafic Rocks
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Potassium in ultramafic rocks

Geochimica et Cosmochimica Acta, 1953
Abstract Quantitative spectrochemical determinations of potassium in 50 specimens of ultramafic rock confirm the preliminary observation ( Ahrens , Pinson and Kearns , 1952) that the abundance of potassium in this rock type is much lower than has usually been assumed.
W Holyk, L.H Ahrens
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Lichens and ultramafic rocks: a review

The Lichenologist, 2004
Floristic, vegetational and ecological features of lichens in ultramafic environments are reviewed using a wide range of literature dating from the beginning of the 20th century. Co-presence of acidophytic (silicicolous) and basiphytic (calcicolous) species and the occurrence of species characterized by particular (disjunct) distribution patterns are ...
Sergio E. FAVERO-LONGO, Deborah ISOCRONO, Rosanna PIERVITTORI   +2 more
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Ultramafic and Related Rocks

1972
The ultramafic rocks are composed mainly of dark-colored mafic or ferro-magnesian minerals such as olivine, pyroxene, amphibole, serpentine, garnet, biotite, and opaque oxides. They are usually, but not always, ultra-basic (having less than 45 percent SiO2).
Gunter Faure, James L. Powell
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Metamorphism of Ultramafic Rocks

1994
Ultramafic rocks are magnesium silicate rocks that normally contain no felsic minerals or very little (
Kurt Bucher, Martin Frey
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