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- W3035253404 abstract "Summary Faults that formed the basin boundary fault were created during extensional evens in the Oligocene. During the late Miocene the NSB experienced compression where fold structures were formed. In addition some extensional faults were also reactivated at this time which caused the formation of inversion structures. By contrast, interpretation of offshore 2D seismic lines shows that the major faults (the basin bounding fault system) are oriented north-south. These faults are also Oligocene in age and are controlled by extensional events. Fold structures formed during the late Miocene and younger. However, there is also fold structure that formed during the Oligocene in the western part of the offshore. During late Miocene-early Neogene the offshore North Sumatra Basin also experienced minor faulting that is expressed by small normal faults." @default.
- W3035253404 created "2020-06-19" @default.
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- W3035253404 date "2019-01-01" @default.
- W3035253404 modified "2023-09-28" @default.
- W3035253404 title "OLIGOCENE TO RECENT STRUCTURAL EVOLUTION OF NORTH SUMATRA BASIN" @default.
- W3035253404 doi "https://doi.org/10.3997/2214-4609.201903422" @default.
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