By Dennis E. Hayes
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Published through the yank Geophysical Union as a part of the Geophysical Monograph Series.
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Extra info for The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands
31, edited by D. E. , pp. S. Government Printing Office, Washington, D. , 1975. Karig, D. , and G. F. Sharman, III, Subduction and accretion in trenches, Geol. Soc. Amer. , 86, 377-389, 1975. Karig, D. , J. G. Caldwell, and E. M. Parmentier, Effects of accretion on the geometry of the descending lithosphere, J. Geophys. , 81, 6281-6291, 1976. Katili, J. , Large transcurrent faults in Southeast Asia with special reference to Indonesia, Geol. , 59, 581-600, 1970. , and W. McCann, Buoyant zones, great earthquakes, and unstable boundaries of subduction, J.
Plate convergence, transcurrent faults, and internal deformation adjacent to Southeast Asia and the western Pacific, J. Geophys. , 77, 4432-4460, 1972. Fitch, T. , and P. Molnar, Focal mechanisms along inclined earthquake zones in the Indonesian-Philippine region, J. Geophys. , 75, 1431-1444, 1970. , and C. F. , Princeton University Press, Princeton, N. , 1954. , Earthquake map of the Indonesian region, scale 1:5,000,000, Misc. Invest. S. Geol. , 1974. , Tectonic map of the Indonesian region, scale 1:5,000,000, Misc.
No focal mechanism solutions that show underthrusting were found for shallow earthquakes along the trench, although event 133 in section K of Figure 5 may represent a compressional bending stress on the bottom of the subducting plate. Only one intermediate depth earthquake has a focal mechanism solution along the North Sulawesi subduction zone. Event 134 (section K of Figure 5) could be interpreted as having a T axis that is oriented down the dip' of the seismic zone. This would help provide some support for a south-dipping seismic zone.