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Origin of high heat flow in the back-arc basins of sumatra:An opportunity for geothermal energy development

Energy Geoscience 2024年第3期5卷 135-150页

作者： Luhut Pardamean Siringoringo Benyamin Sapiie Alfend Rudyawan I Gusti Bagus Eddy Sucipta Department of Geological Engineering Faculty of Earth Science and TechnologyInstitut Teknologi BandungJl.Ganesha No.10Bandung40132Jawa BaratIndonesia Department of Geological Engineering Faculty of Industrial TechnologyInstitut Teknologi SumateraJl.Terusan RyacuduSouth Lampung35365LampungIndonesia

Volcanic arcs such as the Barisan Mountains have been identified as attractive areas for the utilization of geothermal energy,as exemplified by Ulubelu in Lampung and Sarulla in North ***,environmental factors in the Barisan Mountains remain a primary obstacle to the exploration and exploitation of geothermal *** back-arc basins of sumatra exhibit the highest heat flow worldwide;however,the heat source in this area remains a controversial *** study aims to investigate the origin of the high heat flow in the back-arc basins of sumatra(North,Central,and South sumatra basins)based on geothermal data from 384 oil wells and the current literature for geological *** findings of this study indicate that the back-arc basins of sumatra experienced severe extensional deformation during the Tertiary Period through a large pull-apart and slab rollback *** deformation resulted in the thinning of the continental crust in this region(27-32 km)and the formation of multiple normal ***,the presence of magma resulting from mantle upwelling implies a high heat flow in the back-arc basins of *** condition ranks the back-arc basins of sumatra among the highest heat flow regions of the world,with heat flows>100 mW/m^(2).These findings indicate that the back-arc basins of sumatra have significant opportunities to exploit their geothermal energy *** study provides novel insights into the potential of geothermal energy,particularly in the back-arc basins of sumatra.

关键词： back-arc basin of sumatra Slab rollback Extensional deformation Heat flow Geothermal energy

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