Newtonian Dislocation Creep in Quartzites: Implications for the Rheology of the Lower Crust-Reference-Cited by-同舟云学术

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Newtonian Dislocation Creep in Quartzites: Implications for the Rheology of the Lower Crust

Published:1994-08-26 Issue:5176 Volume:265 Page:1204-1206
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Wang J. N.¹,Hobbs B. E.²,Ord A.²,Shimamoto T.¹,Toriumi M.³

Affiliation:

1. Earthquake Research Institute, University of Tokyo, Bunkyo-ku, Tokyo, 113, Japan

2. Commonwealth Scientific and Industrial Research Organization, Division of Exploration and Mining, Post Office Box Wembley, WA 6014, Australia

3. Geological Institute, University of Tokyo, Bunkyo-ku, Tokyo, 113, Japan

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference26 articles.

1. BEEMAN, M. L., JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 98: 6443 (1993).

2. COBLE, R.L., A MODEL FOR BOUNDARY DIFFUSION CONTROLLED CREEP IN POLYCRYSTALLINE MATERIALS, JOURNAL OF APPLIED PHYSICS 34: 1679 (1963).

3. COOPER, R. F., JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS 91: 9315 (1986).

4. COOPER, R. F., JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS 95: 6979 (1990).

5. DELLANGELO, L.N., EXPERIMENTAL DEFORMATION OF PARTIALLY MELTED GRANITIC AGGREGATES, JOURNAL OF METAMORPHIC GEOLOGY 6: 495 (1988).

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