Results 161 to 170 of about 3,356 (219)
Petrologic evidence for core sulfur degassing in partially differentiated planetesimals. [PDF]
Wang SZ +5 more
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Percolative sulfide core formation in oxidized planetary bodies. [PDF]
Crossley SD +9 more
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Raman Spectroscopy and X-Ray Diffraction Investigations of Phase Composition of Tiglit Meteorite. [PDF]
Karczemska A +4 more
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A tale of two planets: Disparate evolutionary models for Mars inferred from radiogenic isotope compositions of Martian meteorites. [PDF]
Borg LE, Kruijer TS.
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Microstructural modeling of the fragmentation of ordinary chondrites. [PDF]
Mohamed MMA +5 more
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The value of returning a sample of the Martian atmosphere. [PDF]
Swindle TD +3 more
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Time of proto-Earth reservoir formation and volatile element depletion from <sup>53</sup>Mn-<sup>53</sup>Cr chronometry. [PDF]
Kruttasch PM, Mezger K.
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Science, 1964
Zircon (ZrSiO 5 ) has been identified as an accessory mineral in the Vaca Muerta mesosiderite and in the troilite nodules of the Toluca iron meteorite. The occurrence in Vaca Muerta is a new discovery confirmed by electron-probe microanalysis of a grain in a polished section of the meteorite.
U B, Marvin, C, Klein
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Zircon (ZrSiO 5 ) has been identified as an accessory mineral in the Vaca Muerta mesosiderite and in the troilite nodules of the Toluca iron meteorite. The occurrence in Vaca Muerta is a new discovery confirmed by electron-probe microanalysis of a grain in a polished section of the meteorite.
U B, Marvin, C, Klein
openaire +2 more sources
Meteorites explained: what is a meteorite?
Geology Today, 2021Meteorites are natural lumps of rock and/or metal that fall to Earth from Space. Most meteorites are from the Asteroid Belt, with a few from the Moon or from Mars, but their ultimate origins extend more widely through the Solar System. More than 150 parent bodies are represented among more than 65 000 meteorites known.
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Nature, 1939
Prof. E. A. Owen and R. W. Williams1 have recently advanced a theory in which they account for the Widmanstatten figures in meteorites on the basis of their X-ray studies of iron-nickel alloys, natural and artificial. Their conclusions have been criticized by Prof. S. W. J. Smith and J.
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Prof. E. A. Owen and R. W. Williams1 have recently advanced a theory in which they account for the Widmanstatten figures in meteorites on the basis of their X-ray studies of iron-nickel alloys, natural and artificial. Their conclusions have been criticized by Prof. S. W. J. Smith and J.
openaire +1 more source

