Skripsi
STUDI PROVENANCE BATUPASIR FORMASI PENETA, DAERAH TAMBANG TINGGI DAN SEKITARNYA, KABUPATEN SAROLANGUN, JAMBI.
The South Sumatra Basin is a basin located in the back area formed from the interaction between the Sunda Shelf (part of the Asian continental plate) and the Indian Ocean plate. This interaction causes sedimentation of various types of sedimentary rocks, one of which is the Peneta Formation, the Peneta Formation was deposited due to the subduction process between Ngalau Plate and West Sumatra which took place intensively during the limestone age, one of which formed clastic sedimentary rocks to sandstone metasediment. The sandstones found in the study area have a fairly wide distribution with varying characteristics either megascopically or petrographically so that they can determine the origin of the rock (provenance) of the sandstone. petrographically, the sandstones found are lithic arenite, lithic arkose, and argillaceous sandstone by looking at the content of monoquartz, polyquartz, feldspar, and lithic. Thus, based on petrographic analysis, it shows that the original rock has undergone several uplifting processes due to tectonic activity, in this case, the subduction between Ngalau Plate and the West Sumatra Block, precisely at Subduction Complex Sources which are characterized by an increase in maturity or stability of Continental Block Provenances, In addition, the sandstones of the Peneta Formation contain detritus of quartz and feldspar originating from volcanic and plutonic rocks as a result of the rest of the altitude. granite or other volcanism material that has weathered, then transported, and deposited to a lower place in the study area.
Inventory Code | Barcode | Call Number | Location | Status |
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2207002302 | T74105 | T741052022 | Central Library (Referens) | Available |
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