Mineralbestand und Strukturen der Graphit- und Sulfideinschlüsse in Eisenmeteoriten-Reference-Cited by-同舟云学术

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Mineralbestand und Strukturen der Graphit- und Sulfideinschlüsse in Eisenmeteoriten

Published:1965-10 Issue:10 Volume:29 Page:1131-1151
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Goresy Ahmed El

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference28 articles.

1. Origin, age, and composition of meteorites;Anders;space Sci. Rev.,1964

2. Anders E. (1964) Persönliche Mitteilungen.

3. Origin of diamonds in Canyon Diablo and Novo Urei meteorites;Carter;J. Geophys. Res.,1964

4. Formation of diamond by explosive shock;De Carli;Science,1961

5. Zur Kenntnis der Troilit-Knollen der Meteoriten. ein Beitrag zur Geochemie von Chrom. Nickel und Zinn;Goldschmidt;Nachr. Gesell. Wiss. Göttingen. Math.-Phys. Klasse,1933

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1. Canyon Diablo lonsdaleite is a nanocomposite containing c/h stacking disordered diamond and diaphite;Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences;2023-09-11

2. Natural Graphite Cuboids;Minerals;2019-02-14

3. Shock effects in the Willamette ungrouped iron meteorite;Meteoritics & Planetary Science;2015-11-13

4. Low-Ir IAB irons from Morasko and other locations in central Europe: One fall, possibly distinct from IAB-MG;Meteoritics & Planetary Science;2013-12

5. New evidence of meteoritic origin of the Tunguska cosmic body;Planetary and Space Science;2013-08

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