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Detail Karya Ilmiah Dosen

Teti Syahrulyatia,

Judul : The Environmental Construction of the Bojongmanik Formation in the Rangkasbitung Basin
Abstrak :

The Bojongmanik Formation is the typical formation in the Rangkasbitung Basin. This study aims to know the evolution of the depositional environment in the Rangkasbitung sub-basin, along the Middle Miocene. It continues previous research on the Bojongmanik Formation. The method is field observation and mapping an area of 7 x 8km in the Gajrug area. The development of the Rangkasbitung Basin environment begins at the age of Middle Miocene N9 - N11, at a depth of 10m to 180m, deposited in the form of claystone and sandstone intercalation. The elevation process which causes the basin to be elevated to a depth of 20m – 80m, is the coastline moving further north at the age of N13 - N14. This movement deposited sandstone unit rocks of claystone and limestone intercalation. The process of sedimentation that occurs is Regression.

Tahun : 2020 Media Publikasi : jurnal internasional
Kategori : Jurnal No/Vol/Tahun : Issue 9 / Volume 12, Issue 9 / 2020
ISSN/ISBN : 2201-1323
PTN/S : Universitas Pakuan, Universitas Padjadjaran Program Studi : TEKNIK GEOLOGI
Bibliography :

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