New insights on the origin of flow bands in obsidian

Special Paper of the Geological Society of America

Volumn 396, Issue , 2005, Pages 55-65

  Castro, Jonathan M ^a   Dingwell, Donald B ^b   Nichols, Alexander R L ^b   Gardner, James E ^c  

^a SMITHSONIAN INSTITUTION   (United States)

^b UNIVERSITY OF MUNICH   (Germany)

^c UNIVERSITY OF TEXAS AT AUSTIN   (United States)

Author keywords

Deformation; Flow banding; Obsidian; Welding

Indexed keywords

DEFORMATION; DEGASSING; GLASS; GLASS TRANSITION; GRAIN BOUNDARIES; SHEAR STRESS; SILICATES; TEXTURES; WELDING;

CALORIMETRIC MEASUREMENTS; FLOW BANDING; HYDROTHERMAL ANNEALING; MICROLITE NUMBER DENSITY; OBSIDIAN; STATISTICAL DIFFERENCES; TEXTURAL HETEROGENEITIES; VISCOUS DEFORMATION;

COOLING;

ANNEALING; CONCENTRATION (COMPOSITION); DEGASSING; ESTIMATION METHOD; FLOW PATTERN; HYDROTHERMAL ACTIVITY; MAGMATISM; MELTING; MINERAL; OBSIDIAN; TEXTURE; TIMESCALE;

EID: 84874993887     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/0-8137-2396-5.55     Document Type: Article

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