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Volumn 414, Issue 6865, 2001, Pages 738-742
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Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation
a a a a |
Author keywords
[No Author keywords available]
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Indexed keywords
CHANNEL FLOW;
DUCTILITY;
METAMORPHIC ROCKS;
VISCOSITY;
DENUDATION;
TECTONICS;
CHANNEL FLOW;
EXTRUSION;
METAMORPHISM;
TECTONIC EVOLUTION;
VISCOSITY;
ARTICLE;
ASTRONOMY;
CHINA;
FLOW KINETICS;
GEOLOGY;
MODEL;
MOTION;
PRIORITY JOURNAL;
VELOCITY;
ASIA;
CHINA;
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EID: 0035856951
PISSN: 00280836
EISSN: None
Source Type: Journal
DOI: 10.1038/414738a Document Type: Article |
Times cited : (1478)
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References (30)
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