Flores Back Arc Thrust Fault is a major system of west–east trending thrust faults that extend eastwards from west of Lombok just south of where Sunda Shelf ends at Bali Sea, towards the islands of Sumbawa, Flores, and Alor, with a total length of at least 800 km.,[1] entering the Weber Basin and Aru Basin adjacent Sahul Shelf of the Australian plate. The thrust faults are south-dipping and lie within the back arc region of the Sunda-Banda Arc, which is related to the ongoing subduction of the Australian Plate beneath the Sunda and Banda Sea Plates. The thrust fault system developed as a result of the onset of continental collision as continental crust of the Australian Plate reached the Sunda Trench. The eastern part of the fault system is also known as the Wetar thrust. Above the main thrust fault are a series of imbricate (overlapping) thrust faults. These imbricate thrust faults are shallower in depth than the main Flores thrust.[2] Although the exact thrust faults have not been established, these faults were thought to be responsible for the 2018 Lombok earthquakes.
^Yang, X.; Singh, S.; Tripathi, A. (2020). "Did the Flores backarc thrust rupture offshore during the 2018 Lombok earthquake sequence in Indonesia?" (PDF). Geophysical Journal International. 221: 758–768. doi:10.1093/gji/ggaa018.
^"Earthquake Report: Lombok, Indonesia | Jay Patton online".
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shallow thrustfault on or near the FloresBackArcThrust, at which the Australian and Sunda plates underthrusts the Indonesian volcanic island arcs, the...
a major thrustfault, the 500 km (310 mi) long FloresThrust. The Lombok earthquake has been attributed to movement along the FloresThrust. The earthquake...
Lesser Sunda Islands. The Sunda Arc begins at Sumatra and ends at Flores, and is adjacent to the Banda Arc. The Sunda Arc is formed via the subduction of...
This list covers all faults and fault-systems that are either geologically important[clarification needed] or connected to prominent seismic activity.[clarification...
Small FaultsFloresBackArcThrustFault Great Sumatran Fault Marikina Valley Fault System New Britain subduction zone Palu-Koro Fault Philippine Fault System...
the accretionary wedge associated with the trench and the age of adakitic arc rocks on Mindanao thought to date the onset of subduction. The trench is...
Small FaultsFloresBackArcThrustFault Great Sumatran Fault Marikina Valley Fault System New Britain subduction zone Palu-Koro Fault Philippine Fault System...
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Eastwards from Bali, the Sunda Arc is also being thrust over the Bali and Floresback-arc basins on a series of south-dipping thrusts. Focal mechanisms for earthquakes...
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the seabed. 1,500-metre-high (5,000 ft) thrust ridges created by previous geologic activity along the fault had collapsed, generating landslides several...
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Ryukyu islands and mainland China Flores Sea – A marginal sea in Indonesia between Sulawesi and the Sunda Islands of Flores and Sumbawa Gulf of Carpentaria...