Flow banding in obsidian: A record of evolving textural heterogeneity during magma deformation

Earth and Planetary Science Letters

Volumn 236, Issue 1-2, 2005, Pages 135-147

  Gonnermann, Helge M ^a,b   Manga, Michael ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

^b HARVARD UNIVERSITY   (United States)

Author keywords

Flow banding; Fractal; Fragmentation; Mixing; Obsidian; Volcanology

Indexed keywords

BIG GLASS MOUNTAIN (BGM); SPECTRAL DENSITY; TEXTURAL ANALYSIS; VARIABLE MICROLITE CONTENT (VMC);

BRITTLE FRACTURE; CRYSTALLINE MATERIALS; DEGASSING; MATHEMATICAL MODELS; NUCLEATION; NUMERICAL ANALYSIS; VISCOUS FLOW; VOLCANIC ROCKS;

GEOMORPHOLOGY;

LAVA FLOW; OBSIDIAN; TEXTURE;

EID: 22144475795     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2005.04.031     Document Type: Article

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