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The PCFZ is interpreted to be a regional fault which managed the N-S transtensional pull-apart Paleogene basins in NWJB. The PCFZ is probably going for being A part of the dextral Malacca strike-slip fault which managed the development with the Paleogene basins in Sumatra. This regional tectonic reconstruction can be quite a achievable different model to clarify the distribution of numerous hydrocarbon seep from the Neogene deep water North Serayu and Banyumas basins with enigmatic origin in petroleum process, differed With all the adjacent Bogor Basin to the west which displays no hydrocarbon seeps.
Tectonic evolution and crustal composition of your central Indonesian location from geology, gravity and also other geophysical knowledge
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Current coastlines of northern and southern Central Java indent significantly when compared to Those people of West Java and East Java. This really is regarded as an anomaly and wishes a geological rationalization. Observation on published and unpublished literatures, gravity, landsat imageries, floor geology, and seismic data, examined by structural Investigation and regional tectonics interpretation, lead to the summary which the Central Java indentation can be a structural segmentation forming re-entrants.
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