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Statements

Subject Item
dbr:Flores_Back_Arc_Thrust_Fault
rdfs:label
Flores Back Arc Thrust Fault
rdfs:comment
Flores Back Arc Thrust Fault is a major system of west-east trending thrust faults that extend eastwards from west of Lombok towards the islands of Sumbawa, Flores, and Alor, with a total length of at least 800 km. 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
dcterms:subject
dbc:Geology_of_Indonesia dbc:Seismic_faults_of_Indonesia dbc:Thrust_faults dbc:Seismic_faults_of_Southeast_Asia
dbo:wikiPageID
58606165
dbo:wikiPageRevisionID
1095304496
dbo:wikiPageWikiLink
dbr:Banda_Sea_Plate dbr:Sunda_Arc dbr:Sunda_Trench dbc:Geology_of_Indonesia dbr:2018_Lombok_earthquake dbr:Back_arc dbr:Subduction dbr:Australian_Plate dbc:Seismic_faults_of_Indonesia dbr:Sumbawa dbr:Continental_collision dbr:Banda_Arc dbr:Continental_crust dbr:Alor_Island dbc:Thrust_faults dbr:Lombok dbr:Sunda_Plate dbr:Strike_and_dip dbc:Seismic_faults_of_Southeast_Asia dbr:Thrust_fault dbr:Flores
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dbt:Earthquakes_in_Indonesia dbt:Tectonics-stub dbt:Reflist dbt:Short_description dbt:SE_Asia_plates
dbo:abstract
Flores Back Arc Thrust Fault is a major system of west-east trending thrust faults that extend eastwards from west of Lombok towards the islands of Sumbawa, Flores, and Alor, with a total length of at least 800 km. 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. Although the exact thrust faults have not been established, these faults were thought to be responsible for the 2018 Lombok earthquakes.
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wikipedia-en:Flores_Back_Arc_Thrust_Fault?oldid=1095304496&ns=0
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2187
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wikipedia-en:Flores_Back_Arc_Thrust_Fault