Ravasz Csaba and Emszt Mihály and Pantó György: The Minnichhof meteorite. In: Acta mineralogica-petrographica, (23) 1. pp. 139-158. (1977)
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Abstract
The dominant minerals of the Minnichhof meteorite are olivine (Fa25.3) and hypersthene (Fa2i.6) with nickel-iron (kamacite, taenite, plessite), plagioclase (An12), diopside of minor quantity and accessory chromite, merrillite, ilmenite, daubréelite and limonite. Specific gravity: 3.53. On the basis of the given electron-probe microanalysis as well as the complete chemical analysis, X-ray diffractometric diagrams, spectrographical and mineral-petrographical examinations the stone is an olivine-hypersthene chondrite [MASON, 1962 and 1965], equilibrated, ordinary chondrite [DODD—VAN SCHMUS—WOOD, 1967] which belongs to the L-group [UREY—CRAIG, 1953] and can be classed into the L5—L6 types [VAN SCHMUS—WOOD, 1967].
| Item Type: | Article |
|---|---|
| Journal or Publication Title: | Acta mineralogica-petrographica |
| Date: | 1977 |
| Volume: | 23 |
| Number: | 1 |
| ISSN: | 0365-8066 |
| Page Range: | pp. 139-158 |
| Language: | English |
| Publisher: | University of Szeged, Department of Mineralogy, Geochemistry and Petrology |
| Place of Publication: | Szeged |
| Related URLs: | http://acta.bibl.u-szeged.hu/39396/ |
| Uncontrolled Keywords: | Kőzettan, Ásványtan, Földtan |
| Additional Information: | Bibliogr.: p. 157-158. ; ill. ; összefoglalás angol nyelven |
| Subjects: | 01. Natural sciences 01. Natural sciences > 01.05. Earth and related environmental sciences |
| Date Deposited: | 2016. Oct. 17. 09:25 |
| Last Modified: | 2022. Jul. 25. 10:14 |
| URI: | http://acta.bibl.u-szeged.hu/id/eprint/24624 |
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