Deformation patterns in a high-viscosity lava flow inferred from the crystal preferred orientation and imbrication structures: an example from Salina (Aeolian Islands, southern Tyrrhenian Sea, Italy)
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/content/pdf/10.1007/BF00304439.pdf
Reference28 articles.
1. Barca D, Ventura G (1991) Volcano-tectonic evolution of Salina island (Aeolian Archipelago, South Tyrrhenian Sea). Mem Soc Geol It 47:401–415
2. Blanchard J Ph, Boyer P, Gagny C (1979) Un noveau critere de sense de mise en place dans une caisse filoniene: le “pincement” des mineraux aux epontes (orientation des mineraux dans un magma en ecoulement). Tectonophysics 53:1–25
3. Blumenfeld P (1983) Le “tuillage des megacristaux”, un critere d'ecullement rotationnel pour les fluidalites des roches magmatiques Application au Granite de Barbey-Seroux (Vosges, France). Bull Soc Geol Fr 7 (25):309–318
4. Blumenfeld P, Bouchez JL (1988) Shear criteria in Granite and migmatite deformed in the magmatic and solid states. J Struct Geol 10 (4):361–372
5. Colletta E (1993) Studio petrografico e geochimico della sequenza eruttiva del I Ciclo di attivita' del Mte dei Porri (Isola di Salina — Arcipelago delle Eolie). Thesis, University of Calabria, Italy
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