Structural development and petrofabrics of eclogite facies shear zones, Bergen Arcs, western Norway: implications for deep crustal deformational processes-Reference-Cited by-同舟云学术

Structural development and petrofabrics of eclogite facies shear zones, Bergen Arcs, western Norway: implications for deep crustal deformational processes

Published:1992-03 Issue:2 Volume:10 Page:127-146
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J Metamorph Geol

Author:

BOUNDY T. M.,FOUNTAIN D. M.,AUSTRHEIM H.

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1525-1314.1992.tb00075.x/fullpdf

Reference58 articles.

1. Fluid inclusions in granulites and eclogites from the Bergen Arcs, Caledonides of W. Norway

2. Fluid-induced retrogression of granulites in the Bergen Arcs, Caledonides of W. Norway: Fluid inclusion evidence from amphibolite-facies shear zones

3. Uplift of deep crust during orogenic extensional collapse: A model based on field studies in the Sogn-Sunnfjord Region of western Norway

4. Eclogitization of lower crustal granulites by fluid migration through shear zones

5. H. Austrheim , 1987 . Eclogitisation and amphibolitisation of granulite facies anorthosites in relation to deep crustal shear zones, Bergen Arcs, western Norway . Excursion Guide NARW, Lindas, 6 pp.

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