High-pressure polymorphs of olivine and silica in Kamargaon (L6) chondrite by laser micro-Raman and XRD studies
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12040-021-01803-y.pdf
Reference84 articles.
1. Agarwal V, Parthasarathy G, Sisodia M S and Bhandari N 2014 Fall, mineralogy and chemistry of Nathdwara H6 chondrite; Geosci. Front. 5 413–417.
2. Agee C B 1998 Phase transformations and seismic structure in the upper mantle and transition zone; In: Ultra-high pressure mineralogy: Physics and chemistry of the Earth’s deep interior (ed.) Hemley R J, Rev. Mineral. 37 165–203.
3. Andrault D, Fiquet G, Guyot F and Hanfland M 1998 Pressure-induced landau-type transition in stishovite; Science 282 720–724.
4. Aoudjehane H C, Jambon A, Reynard B and Blanc P 2005 Silica as a shock index in shergottites: A cathodoluminescence study; Meteor. Planet. Sci. 40 967–979.
5. Bauer J F 1979 Experimental shock metamorphism of mono- and polycrystalline olivine – A comparative study; 10th LPSC, pp. 2573–2596.
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1. Bulk and in-situ chemical analysis of meteorite Berduc, an L6 chondrite;Journal of Earth System Science;2023-01-27
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