Occurrence of low-Ca clinopyroxene and the role of deformation in the formation of pyroxene-Fe−Ti oxide symplectites-Reference-Cited by-同舟云学术

Occurrence of low-Ca clinopyroxene and the role of deformation in the formation of pyroxene-Fe−Ti oxide symplectites

Published:1991-07 Issue:1-2 Volume:108 Page:181-195
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Barton Michael,Sheets Julia Meyer,Lee William E.,van Gaans Chris

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00307337.pdf

Reference75 articles.

1. Ashwal LD (1982) Mineralogy of mafic and Fe−Ti oxide-rich differentiates of the Marcy anorthosite massif, Adirondacks, New York. Am Mineral 67: 14–27

2. Bard JP (1986) Microtextures of igneous and metamorphic rocks. D. Reidel Publishing company, Dordrecht

3. Barton M, van Bergen MJ (1984) Secondary ilvaite in a dolerite dyke from Rogaland, SW Norway. Mineral Mag 48: 449–456

4. Barton M, van Gaans C (1988) Formation of orthopyroxene-Fe−Ti oxide symplectites in Precambrian intrusives, Rogaland, south-western Norway. Am Mineral 73: 1046–1059

5. Binns RA, Long JVP, Reed SJB (1963) Some naturally occurring members of the clinoenstatite-clinoferrosilite mineral series. Nature 198: 777–778

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