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O. Bellier and M. Sebrier
Is the slip rate variation on the Great Sumatran Fault accommodated by fore-arc stretching?
Geophysical Research Letters (August 1995), 22(15):1969-1972

Index Terms/Descriptors:
accommodation zones; Asia; back-arc basins; basins; displacements; Eurasian Plate; Far East; faults; fore-arc basins; Great Sumatran Fault; Indian Ocean; Indo-Australian Plate; Indonesia; oblique-slip faults; plate convergence; plate tectonics; slip rates; strike-slip faults; subduction zones; Sumatra; Sunda Arc; transpression

Latitude & Longitude:
S60°00'00" - N25°00'00" and E20°00'00" - E120°00'00" (Search for maps and images at Alexandria Digital Library)
S6°00'00" - N5°45'00" and E95°05'00" - E106°10'00" (Search for maps and images at Alexandria Digital Library)
S11°00'00" - N6°00'00" and E95°00'00" - E128°00'00" (Search for maps and images at Alexandria Digital Library)

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