Results 131 to 140 of about 2,701 (192)

A potential mantle origin for precursor rocks of high-Mg impact glass beads in Chang'e-5 soil. [PDF]

Sci Adv
Ding CL, Nemchin A, Johnson T, Norman MD, Guan Y, Tian LL, Xie WL, Li LS, Zhou SD, Xu KX, Wang XL.   +10 more
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Suitability of rocks, minerals, and cement waste for CO₂ removal via enhanced rock weathering. [PDF]

Commun Chem
Danczyk M, Oze C.
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Plant nickel-exclusion versus hyperaccumulation: a microbial perspective. [PDF]

Microbiome
Dijoux J, Gigante S, Lecellier G, Guentas L, Burtet-Sarramegna V.   +4 more
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Microbial growth rates captured using Raman-SIP reveal a highly active subsurface biosphere fueled by serpentinization. [PDF]

Nat Commun
Kashyap S, Caro TA, Templeton AS.
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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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Effect of soil additives on biogeochemistry of ultramafic soils-an experimental approach with Brassica napus L. [PDF]

Environ Monit Assess
Pędziwiatr A, Kierczak J, Potysz A, Pietranik A.   +3 more
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Zircon behavior in the partially melted planetary mantle

Yakimenko A, Borisova A, Fedortchouk Y, Fairhurst L.   +3 more
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Synchronous Miocene radiations and geographic-dependent diversification of pantropical Xylopia (Annonaceae)

Nge FJ, Johnson DM, Murray NA, Holzmeyer L, Floyd K, Stull G, Soule V, Sepulchre P, Tardif D, Rodrigues-Vaz C, Couvreur TLP.   +10 more
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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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Nature of Ultramafics

2007
The earth is divided into three layers: the crust, the mantle, and the core. There are two principle regions within the crust: continents and ocean basins. The rocks that make up these layers differ from one another in chemical composition and density.
Earl B. Alexander, Roger G. Coleman, Todd Keeler-Wolfe, Susan P. Harrison   +3 more
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