Chemical and crystallographic study of cronstedtite in the matrix of the Cochabamba (CM2) carbonaceous chondrite-Reference-Cited by-同舟云学术

Chemical and crystallographic study of cronstedtite in the matrix of the Cochabamba (CM2) carbonaceous chondrite

Published:1979-12 Issue:4 Volume:26 Page:293-304
ISSN:0041-3763
Container-title:TMPM Tschermaks Mineralogische und Petrographische Mitteilungen
language:en
Short-container-title:TMPM Tschermaks Petr. Mitt.

Author:

M�ller W. F.,Kurat G.,Kracher A.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF01089843.pdf

Reference20 articles.

1. Bunch, T. E., Chang, S., 1978: Carbonaceous chondrite (CM) phyllosilicates: Condensation or alteration origin? Lunar Planet. Sci.9, 134?136 (1978).

2. Gossner, B., 1936: Über Cronstedtit von Kisbanay. Zbl. Min.A36, 195?201.

3. Hendricks, S. B., 1938: The crystal structure of nacrite Al2O3·2SiO2·2H2O and the polymorphism of the kaolin minerals. Z. Kristallogr.100, 509?518.

4. Kallemeyn, G. W., Wasson, J. T., 1979: Unusual chondritic meteorites and clasts: elemental fractionations and relationships to the carbonaceous chondrite groups. Lunar Planet. Sci.10, 644?646.

5. Kerridge, J. F., 1976: Major element composition of phyllosilicates in the Orgueil carbonaecous meteorite. Earth Planet. Sci. Letts.29, 194?200.

Cited by 50 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Characterization of Iron-Rich Phyllosilicates Formed at Different Fe/Si Ratios;Clays and Clay Minerals;2022-08

2. Cronstedtite from Litošice, Czech Republic;Journal of Geosciences;2021-12-29

3. An evolutionary system of mineralogy, Part V: Aqueous and thermal alteration of planetesimals (~4565 to 4550 Ma);American Mineralogist;2021-09-01

4. Microstructures of enstatite in fine-grained CAIs from CV3 chondrites: Implications for mechanisms and conditions of formation;Geochimica et Cosmochimica Acta;2021-03

5. An evolutionary system of mineralogy. Part III: Primary chondrule mineralogy (4566 to 4561 Ma);American Mineralogist;2021-03-01