Abstract
The geothermal potential in Tarutung is controlled by both the Sumatra Fault system and young arc volcanism. In this study we use the spatial distribution of seismic attenuation, calculated from local earthquake recordings, to image the 3-D seismic attenuation of the area and relate it with the temperature anomalies and the fluid distribution of the subsurface. A temporary seismic network of 42 stations was deployed around Tarutung and Sarulla (south of Tarutung) for a period of 10 months starting in 2011 May. Within this period, the network recorded 2586 local events. A high-quality subset of 229 events recorded by at least 10 stations was used for the attenuation inversion (tomography). Path-average attenuation (t(p)*) was calculated by using a spectral inversion method. The spread function, the contour lines of the model resolution matrix and the recovery test results show that our 3-D attenuation model (Q(p)) has good resolution around the Tarutung Basin and along the Sarulla graben. High attenuation (low Q(p)) related to the geothermal system is found in the northeast of the Tarutung Basin suggesting fluid pathways from below the Sumatra Fault. The upper part of the studied geothermal system in the Tarutung district seems to be mainly controlled by the fault structure rather than by magmatic activities. In the southwest of the Tarutung Basin, the high attenuation zone is associated with the Martimbang volcano. In the Sarulla region, a low-Q(p) anomaly is found along the graben within the vicinity of the Hopong caldera.
Highlights
The Tarutung region is one of the geothermal areas in Sumatra that the Indonesian government is planning to exploit
We have produced a well-resolved Qp structure of the Tarutung geothermal area correlating with geothermal prospects and volcanism
Our study confirms that attenuation tomography is a powerful tool for the exploration of a geothermal site in a seismically active region
Summary
The Tarutung region is one of the geothermal areas in Sumatra that the Indonesian government (the Center for Geological Resources) is planning to exploit. The geothermal potential in the region is manifested by several hot springs (represented by red stars in Fig. 1) along the Tarutung Basin. As Tarutung is located on the Tarutung Basin along the Sumatra Fault and surrounded by young volcanoes and calderas, the whole tectonic system of the area is considered to play a significant role for the geothermal system (Muksin et al 2013)
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