Jf. Genrich et al., ACCRETION OF THE SOUTHERN BANDA ARC TO THE AUSTRALIAN PLATE MARGIN DETERMINED BY GLOBAL POSITIONING SYSTEM MEASUREMENTS, Tectonics, 15(2), 1996, pp. 288-295
Global Positioning System geodetic measurements at thirteen locations
in Indonesia and four in Australia reveal that the Australian continen
t has accreted the Banda island are to its margin. Small relative velo
cities of five sites on west Java, south Kalimantan, Bah, and south Su
lawesi define a rigid Sunda shelf that moves relative to northern Aust
ralia in a manner consistent with pole locations from NUVEL-1 Australi
a-Eurasia but at a rate that is about 7% slower. Block-like northward
motion of the southern Panda are toward the Sunda shelf at nearly the
same rate as Australia suggests that the Timer trough is now inactive
as a thrust. Little of the convergence of Australia with Eurasia is ac
commodated by strain within the Banda are structure. Most of the conve
rgence appears to occur as northward translation of the rigid are with
shortening on the Flores and Wetar thrusts and possibly on faults wit
hin the back are basin.