Results 211 to 220 of about 73,435 (259)
Stress evolution and associated microstructure during transient creep of olivine at 1000–1200 °C
, 2018 Manuel Thieme +4 more
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Mélange et ségrégation en lit fluidisé dense de particules de media fluidisé (olivine) et de granules de biomasse [PDF]
, 2012 Marc Detournay +3 more
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MCMC-MELTS Inversion Code and Data for Olivine-Rich Units in Jezero Crater, Mars
S. Dutta, Paul Asimow, Kenneth Farley
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Olivines and olivine coronas in mesosiderites
Geochimica et Cosmochimica Acta, 1980The paper presents a study of olivines and their surrounding coronas in mesosiderites texturally and compositionally using optical and microprobe methods. Olivine composition ranges from Fo(58-92) and shows no consistent pattern of distribution within and between mesosiderites; olivine occurs as large single crystals or as partially recrystallized ...
C.E. Nehru +3 more
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Sintering of olivine and olivine-basalt aggregates
Physics and Chemistry of Minerals, 1984The sintering behavior of olivine and olivine-basalt aggregates has been examined at temperatures near 1,300° C. Experimental factors contributing to rapid sintering kinetics and high-density, fine-grained specimens include: (i) the uniform dispersion of basalt throughout the specimen, (ii) a very fine, uniform particle size for the olivine powder ...
R. F. Cooper, D. L. Kohlstedt
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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 +3 more
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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 +3 more
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Olivine nodules in olivine nephelinite from Tokatoka, Northland
New Zealand Journal of Geology and Geophysics, 1965Abstract Petrographic descriptions and a chemical analysis are presented of an olivine nephelinite occurring as a dike in argillaceous limestones and in regional association with a Miocene basalt-andesite-dacite igneous suite.The mineralogy and possible origin of olivine nodules carried by the nephelinite are discussed.
Philippa M. Black, R.N. Brothers
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