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Titlebook: Meteorites; Classification and P John T. Wasson Book 1974 John T. Wasson, Los Angeles 1974 Accretion.Meteorit.Meteorites.classification.min

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41#
發(fā)表于 2025-3-28 14:36:25 | 只看該作者
42#
發(fā)表于 2025-3-28 20:51:30 | 只看該作者
Mineralogy and Phase Composition,1969a), who also summarizes information about the less common minerals. . (1967d; 1972) gives brief general reviews of the mineralogy of meteorites, and . (1969a) a somewhat more detailed review of chondrite mineralogy. . (1963a, b, 1964,1973) gives detailed accounts of his optical observations of opaque minerals in stony meteorites.
43#
發(fā)表于 2025-3-28 22:59:01 | 只看該作者
44#
發(fā)表于 2025-3-29 05:49:11 | 只看該作者
45#
發(fā)表于 2025-3-29 10:49:01 | 只看該作者
Morphology and Macrostructure,tant orientation during their fall have furrows on their forward surfaces radiating away from the apex. The rear surface is either unmarked or is furrowed, with the wavelength longer and amplitude smaller than on the forward surface. An excellent example of an oriented meteorite is the Cabin Creek iron (pp.40–41 of ., 1962a).
46#
發(fā)表于 2025-3-29 12:29:09 | 只看該作者
An Example of the Interpretation of Meteorite Properties: The Origin of Ordinary Chondrites, 42, 49, and 9%, respectively. Each group includes representatives of . (1967) petrologic types 3–6; the distribution among these types is shown in Table II-4. Type 6 is the most abundant type in the L and LL groups, type 5 in the H group.
47#
發(fā)表于 2025-3-29 16:57:50 | 只看該作者
978-3-642-65865-5John T. Wasson, Los Angeles 1974
48#
發(fā)表于 2025-3-29 23:43:02 | 只看該作者
49#
發(fā)表于 2025-3-30 00:44:40 | 只看該作者
50#
發(fā)表于 2025-3-30 04:31:45 | 只看該作者
Trace Elements,ce elements as diagnostic indicators of solar-nebula (e.g., . and ., 1967) or parent-body (e.g., . and ., 1969) fractionation processes, or as a means for defining genetically related groups of meteorites (e.g., . et al., 1972).
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