The relationship of phyllosilicate orientation, X-ray diffraction intensity ratios, and c/b fissility ratios in metasedimentary rocks of the Helvetic zone of the Swiss Alps and the Caledonides of Jämtland, central western Sweden

Author:

Jacob Gerd,Kisch Hanan J.,van der Pluijm Ben A.

Publisher

Elsevier BV

Subject

Geology

Reference33 articles.

1. The effects of tectonic strain on crystallinity, apparent mean crystallite size and lattice strain of phyllosilicates in low-temperature metamorphic rocks. A case study from the Glarus overthrust, Switzerland;Arkai;Schweizerische Mineralogische und Petrographische Mitteilungen,1997

2. Asklund, B., Thorslund, P., 1935. Stratigrafiska och tektoniska studier inom Föllingeområdet i Jämtland. Sveriges Geologiska Undersökning, Serie C, No. 388.

3. Determination of March strain from phyllosilicate preferred orientation: a semi-numerical method;Chen;Tectonophysics,1991

4. Clay orientation in some Upper Carboniferous mudrocks, its relationship to quartz content and some inferences about fissility, porosity and compaction history;Curtis;Sedimentology,1980

5. A field classification and intensity scale for first generation cleavages;Durney;AGSO Journal of Australian Geology and Geophysics,1994

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