eprintid: 3078
rev_number: 7
eprint_status: archive
userid: 10
dir: disk0/00/00/30/78
datestamp: 2021-11-22 04:38:00
lastmod: 2022-09-28 04:48:31
status_changed: 2021-11-22 04:38:00
type: article
metadata_visibility: show
creators_name: Astuti, Bernadeta Subandini
creators_id: bernadeta.palguno@gmail.com
title: Tectonic Influence on Change in Neogen
Sediment Supply Western Part of North
Serayu basin_NASIONAL
ispublished: pub
subjects: QE
divisions: sch_civ
keywords: Tectonic Influence; North Serayu Basin; Petroleum System; Sea Level
abstract: Western part of North Serayu Basin composed of Neogene sequence; Halang, Pemali and Rambatan
Formation. The oil seeps discovery in this area is an indication of the presence an active petroleum
system. Active tectonic condition occur coincidence with the time of deposition. The tectonic
influence on change in sediment supply will be the subject of this research.
The combinations of subsidence, eustatic and sediment supply are corresponding to the
accommodation space, moreover to the type of sediment which is deposited. The quantity and rate
of sediment supply to the basin are closely related to the tectonic activity. In the context of Petroleum
Potential, study of sediment supply will provide information about the potential source rock,
reservoir and caprock that developed in the research area. During the Neogene at least there have
been three times of sea level change in the research area which is related to thickening sedimentary
sequence during middle of N18 and thinning in N13 to N17 in some place
date: 2016-05-01
date_type: published
publisher: PPs-UNHAS
official_url: https://itny.ac.id
contact_email: library@itny.ac.id
full_text_status: public
publication: International Journal of Engineering and Science Applications
volume: 3
pagerange: 61-68
refereed: TRUE
issn: 2406-9833
referencetext: Astuti, 2012, Stratigrafi dan Sedimentasi
Batuan Neogen di Cekungan Serayu Utara,
Daerah Kuningan, Jawa Barat – Larangan,
Brebes, Jawa Tengah, Thesis, tidak
dipublikasikan.
[2] Astuti, 2015, Perubahan Muka Air Laut Di
Cekungan Serayu Utara Bagian Barat
Selama Miosen Tengah Hingga Pliosen Di
Daerah Kuningan Jawa Barat, Retti
[3] Satyana, A. H., 2007, Central Java,
Indonesia – “A Terra Incognita” in
Petroleum Exploration : New
Considerations on The Tectonic Evolution
and Petroleum Implications, Proceedings
of Indonesian Petroleum Association
Annual Convention, IPA07-G-085, p. 22.
[4] Pulunggono, A. & Martodjojo, S., 1994,
Geologi Daerah Pegunungan Selatan:
Suatu Kontribusi, pada : Sriyono.,
Hendrayana, H., Rahardjo, W. dan
Wiyono, S. (Eds.), Perubahan Tektonik
Paleogene-Neogene merupakan peristiwa
Terpenting di Jawa. dalam Geologi dan
Geotektonik Pulau Jawa, sejak akhir
Mesozoik hingga Kuarter; Nafiri,
Yogyakarta, Jurusan Teknik Geologi
IJEScA vol. 3, 1, May 2016
Fakultas Teknik , Universitas Gadjah
Mada, hal 37-50.
[5] Van Bemmelen, 1949, The Geology of
Indonesia; vol. I A, General Geology;
Government Printing Office, The Hague,
P. 732. Cox, K. G., Bell, J. D., and
Pankhurst, R. J., (1979). The Interpretation
of Igneous Rocks: London, England,
George Allen & Unwin, Ltd., 450 p.
[6] Satyana, A.H., dan Armandita, C., 2004,
Deepwater plays of Java, Indonesia :
Regional evaluation on opportunities and
risks, IPA Annual Convention
Proceedings, DFE04-OR-002, p 27.
[7] Vail, P. R., Audemard, F., Bowman, S. A.,
Eiser, P. N, Perezcrus, G., 1990, The
Stratigraphic Signatures of Tectonic,
Eustasy and Sedimentation, AAPG
International Lecture, Manuscrip vertion,
p. 99.
[8] Rahardjo, W., 1995, Foraminifera Besar
Tersies Indonesia (merupakan kumpulan
artikel yang diterbitkan Wetenshappelijke
Mededeelingen Dienst van Den
Minjnbouw in Nederlandch-Indie), Teknik
Geologi, Fakultas Teknik UGM.
[9] Tucker, M.E., 1991, Sedimentary
petrology : an introduction to the origin of
sedimentary rocks, Blackwell scientific
publications. P. 260.
[10] Boggs, S. Jr., 2006, Principles of
Sedimentology and Stratigraphy, fourth
edition, Upper Saddle River, New Jersey,
p. 662.
[11]Selley, R.C., 1977, Ancient Sedimentary
Environment, Cornell University Press,
New York, p. 317.
[12]Kastowo, 1975, Peta Geologi Lembar
Majenang, Jawa, P3G, Bandung.
[13]Satyana, A. H., 2010, Gravity Tectonics in
Indonesia-A Companion to Plate Tectonics
: Cases of Isostatic Exhumation and
Gravitational Gliding, Proceedings PIT
IAGI Lombok, p. 12.
[14]Koesoemadinata, R. P. danMartodjojo, S.,
1974, Penelitian Turbidit di Pulau Jawa,
Laporan research no. 1295174, Badan
66
International Journal of Engineering and Science Applications
ISSN: 2406-9833 @2016 PPs-UNHAS
research Institut Teknologi Bandung, 237
hal.
[15] Cateuneanu, 2006, Principles of Sequence
Stratigraphy, Elsevier.
[16]Astuti, B. S., 2016, Identifikasi
Provenance Selama Miosen Tengah
Hingga Pliosen Di Cekungan Serayu Utara
Bagian Barat Di Daerah Kuningan Jawa
Barat, Jurnal Technoscientia, Akprind,
Yogyakarta.
IJEScA vol. 3, 1, May 2016
IJEScA
67
citation:   Astuti, Bernadeta Subandini  (2016) Tectonic Influence on Change in Neogen Sediment Supply Western Part of North Serayu basin_NASIONAL.  International Journal of Engineering and Science Applications, 3.  pp. 61-68.  ISSN 2406-9833     
document_url: https://repository.itny.ac.id/id/eprint/3078/1/11.%20S.%20Tectonic_Influence_on_Change_in_Neogen_Sediment_Su.pdf