New Insights into the Active Tectonics of Eastern Indonesia from GPS Measurements

Friday, 19 December 2014: 9:45 AM
Susilo Susilo1, Achraf Koulali Idrissi2, Simon McClusky2, Irwan Meilano3, Phil R Cummins4, Paul Tregoning4 and Arief Syafii1, (1)Badan Informasi Geospasial, Cibinong, Indonesia, (2)ANU, Canberra, Australia, (3)Bandung Institute of Technology, Bandung, Indonesia, (4)Australian National University, Canberra, Australia
The Indonesian archipelago encompasses a wide range of tectonic environments, including island arc volcanism, subduction zones, and arc-continent collision. Many of the details of this tectonic activity are still poorly understood, especially where the Australian continent collides with Indonesia, separating the Sunda Arc in west from that at the Banda Arc in the east. While it seems clear that the Australian plate is subducted under both the Sunda and Banda Arcs, it is not clear what happens along the 1000 km -long stretch in between. The question of just where the plate motion is accommodated is of major importance to assessments of earthquake and tsunami hazard in the region.

To help resolve these questions the Geospatial Information Agency of Indonesia has collaborated with the Australian National University and the Bandung Institute of Technology in a GPS campaign spanning much of eastern Indonesia, from Lombok in the west to Alor in the east. We have combined these data with those from previous campaigns, resulting in over 27 campaign and 18 continuous GPS sites being used in the analysis. The improvement in site density allowed us to develop of a more complete description of tectonic activity in this region than has been obtained in previous studies. Our preliminary results suggests that there is a relatively simple transition from subduction at the Java Trench off east Java, to a partitioned convergence along both the Timor Trough and the Flores Thrust in the Nusa Tenggara region.