The form and placement of the Sumatran fault along with the active volcanic arc are hugely correlated with the shape and character of your fundamental subducting oceanic lithosphere. Nevertheless, Lively volcanic facilities with the Sumatran volcanic arc haven't affected noticeably the geometry of the Energetic Sumatran fault. On The premise of its geologic record and pattern of deformation, we divide the Sumatran plate margin into northern, central and southern domains. We guidance preceding proposals that the geometry and character of your subducting Investigator fracture zone are influencing The form and evolution of your Sumatran fault system throughout the central area. The southern domain is easily the most normal. The Sumatran fault there comprises 6 combat-stepping segments. This pattern suggests that the general development of the fault deviates four ø clockwise in the slip vector amongst The 2 blocks it separates. The regularity of this area and its Affiliation Using the percentage of the subduction zone that generated the large (Mw 9) earthquake of 1833 suggest that a geometrically uncomplicated subducting slab ends in both of those straightforward strike-slip faulting and unusually large subduction earthquakes.
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The PCFZ is interpreted like a regional fault which controlled the N-S transtensional pull-apart Paleogene basins in NWJB. The PCFZ is probably going for being Component of the dextral Malacca strike-slip fault which controlled the event with the Paleogene basins in Sumatra. This regional tectonic reconstruction could be a achievable substitute product to elucidate the distribution of numerous hydrocarbon seep during the Neogene deep water North Serayu and Banyumas basins with enigmatic origin in petroleum procedure, differed Together with the adjacent Bogor Basin for the west which reveals no hydrocarbon seeps.
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