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Published via the yankee Geophysical Union as a part of the Geodynamics Series.
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Extra resources for Recent Plate Movements and Deformation
M. Didyk, TRENCH Copyright American Geophysical Union DEPTH AND RELATIVE MOTION 25 Geodynamics Series Recent Plate Movements and Deformation J. K. Leggett, N. Lundberg, K. J. McMillen, N. Niitsuma, L. E. Shepard, F. J. Stephan, and H. Stradner, Progressive accretion in the Middle America trench, southern Mexico, Nature, 281, 638-642, 1979. , and T. Asanuma, Studies on seismic profiler measurements off Boso-Jyoban district, northeast Japan, Bull. Nat. Sci. Mus. Tokyo, 13, 337-355, 1970. , V. Renard, J.
Energy and Mineral map of the Circum Region, northwest quadrant, AAPG, 1981a. Circum-Pacific Council for Energy and Mineral Resources, Plate tectonic map of the Circum Pacific Region, northeast quadrant, AAPG, 1981b. Fisher, R. , Middle America trench: Topography and structure, Geol. Soc. Amer. , 72, 703-720, 1961. Geological Survey of Japan, Geological map of the northern Ogasawara arc, Marine Geology Map Series, 17, 1982. , and J. , 82, 45-56, 1982. Hilde, T. W. , N. Isezaki, and J. M. Wageman, Mesozoic Sea-floor spreading in the North Pacific, 205-226, Hilde, T.
The accelerated and widened aseismic slip event may be an indication of the plastic weakening of the deep material below the reactivated fault-tip and may be regarded as a for earthquake development with ground deformation, Symposiumof the recent plate movements and deformation, Tokyo, Japan, 1982. Y. A. Gao, Numerical modeling of short-term precursor. D. P. Wang, Cenozoic Graben systems in North China, Z. Geomorph. F•, Suppl. , 42, 99-110, 1982. stress increase on the locked and unfailed portion in the front of the fault tip, bringing it to rupture level and generating a great earthquake.