eprintid: 3060 rev_number: 13 eprint_status: archive userid: 10 dir: disk0/00/00/30/60 datestamp: 2021-11-18 03:27:49 lastmod: 2021-11-23 04:20:41 status_changed: 2021-11-18 03:27:49 type: article metadata_visibility: show creators_name: Bernadeta Subandini Astuti, . creators_id: bernadeta.palguno@gmail.com title: Sedimentation Process of Rambatan Formation in Larangan Brebes, North Serayu Range, Central Java ispublished: pub subjects: QE keywords: Rambatan Formation, deep marine channel,deep marine tidal, turbidito abstract: Abstract - Rambatan Formation in the western part of North Serayu Basin, Brebes, Central Java, comprises generally flysch facies of turbidite sediments deposited in a deep marine environment. This formation is equivalent to Merawu Formation found in the eastern part of the basin and deposited in the environment of tidal flat to subtidal. The turbidite sediments were highly controlled by a rapid downward movement taking place continuously during Early to Late Miocene. The variation of the depositional environment has been the object of this research which aims to understand the sedimentation process of Rambatan Formation in this type locality with a modern turbidite approach. Rambatan Formation was deposited in N13-N19, as a deep marine sediment channel, turbidite, and deep marine tidal zone. The sedimentation was affected by gravity flow and bottom current. The sediments on N13-N14 were marked by turbidite sediments until Middle N17. The sediment supply increased on Middle N17, as a sediment filler on a channel marked by contourite mud layer (muddy slump) and debris flow, with sources from the north. The increase of sediment supply was followed by an environmental transformation from a deep marine channel into deep marine tidal area. In N19 date: 2019-08-12 date_type: published publisher: Badan Geologi official_url: https://www.library.co.id contact_email: library@itny.ac.id full_text_status: public pres_type: other publication: Indonesian Journal on Geoscience volume: 6 number: 2 pagerange: 141-151 event_title: INDONESIAN JOURNAL ON GEOSCIENCE Geological Agency Ministry of Energy and Mineral Resource event_location: Institut Teknologi Nasional Yogyakarta event_dates: 2 Agustus 2019 event_type: conference refereed: TRUE issn: 2355-9314 referencetext: Abdurrokhim and Ito, M., 2013. The Role of slump scars in slope channel initiation: A case study from the Miocene Jatiluhur Formation in the Bogor Trough, West Java. Journal of Asia Earth Sciences, p.68-86. DOI: 10.1016/j. jseaes.2013.04.005 Astuti, B. S., 2015. Identifikasi provenance selama Miosen Tengah hingga Pliosen di Cekungan Serayu Utara bagian barat di daerah Kuningan, Jawa Barat. Technocientia, IST Akprind. Astuti, B. S., 2016. 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