Email this article 
Hide
Show all
SEISMIC FACIES ANALYSIS ON 2D SEISMIC REFLECTION PROFILE IN BARUNA AND JAYA LINE AT NORTH EAST JAVA BASIN
Abstract
Two dimension (2D) seismic profile of Baruna and Jaya lines at North-East Java Basin show seismic reflector characteristics that can be used to interpret sediment thickness and continuity. Those reflector characteristics that can be applied for seismic facies analysis that represent depositional environment. This study starts from seismic data processing that using Kirchhoff Post Stack Time Migration method which is 2D seismic profile as result. Seismic reflector characterization has been done to both 2D profiles. Seismic reflector characterization was grouped as (i) individual reflection, (ii) reflection configuration, (iii) reflection termination, (iv) external form. Individual reflection characteristics show high and medium amplitude, medium and low frequency, and continuous. Configuration reflection is continuous with parallel and subparallel type. Reflection termination shows onlap, and external form shows sheet drape. Local mound appearance can be interpreted as paleo-reef. Facies seismic anlysis result for this study area is shelf.
Keywords
Full Text:
PDFReferences
Boggs, S.Jr. Principles of Sedimentology and Stratigraphy, 4th Ed. New Jersey: Pearson Prentice Hall; 2009.
R. G. Walker and N. P. James (eds). Facies Models. Response to Sea Level Change. 2nd ed. Canada: Geological Association of Canada; 1992.
Munadi, S. Pengolahan Data Seismik: Prinsip Dasar dan Metodologi. Depok: Percetakan Universitas Indonesia, Indonesia; 2002.
Yilmaz, O. Seismic Data Processing, Society of Exploration Geophysicists, Investigations in Geophysics No. 2. Tulsa, Society of Exploration Geophysics; 1987.
Schneider W.A. Integral Formulation for Migration in Two and Three Dimensions. Geophysics. 1978 Feb; 13(I),19-76.
Bancroft, J. C. A Practical Understanding of Pre- and Poststack Migrations, Volume I. Tulsa: Society of Exploration Geophysicist; 1997.
Mitchum, R.M, Vail P.R., and Thompson S. Seismic stratigraphy and global changes in sealevel, Part 2: The depositional sequence as a basic unit for stratigraphic analysis. In: Payton (Ed.), Seismic Stratigraphy: Application to Hydrocarbon Exploration. AAPG-Memoir No. 26, AAPG, Tulsa; 1977. p. 53–62.
Badley, M. E. Practical Seismic Interpretation. Englewwod Cliffs: Prentice Hall; 1985.
Soeka S. and Munadi, S. Prinsip Dasar Rekonstruksi Lingkungan Pengendapan Berdasarkan Fasies Seismik. Depok: Percetakan Universitas Indonesia, Indonesia; 2008.
Sangree, J.B and Widmier J.M. Seismic stratigraphy and global changes in sealevel Part 9: seismic interpretation of clastic depositional facies. In: Payton (Ed.), Seismic Stratigraphy: Application to Hydrocarbon Exploration, AAPG-Memoir No. 26, AAPG, Tulsa; 1977. p. 165–184.
Vail, P. R., Todd R. G., and Sangree J. B. Seismic Stratigraphy and Global Changes of Sea Level: Part 5. Chronostratigraphic Significance of Seismic Reflections: Section 2. Application of Seismic Reflection Configuration to Stratigraphic Interpretation. AAPG Memoir 26; 1977. p. 99 – 116.
Veeken P.C.H. Seismic Stratigraphy and Depositional Facies Model. Amsterdam: Academic Press; 2013.
Nicholas G. Sedimentology and Stratigraphy. UK: Wiley-Blackwell; 2009.
The Walker School Environmental Science. Geology and The Environment; 31st October 2008 [cited June 20th 2016]. Available from: http://www.slideshare.net/guest 4eac6/geology-and-the-environment-presentation. Internet.
DOI: https://doi.org/10.18860/neu.v9i1.3665
Refbacks
- There are currently no refbacks.
Copyright (c) 2016 Taufan Wiguna, Rahadian Rahadian, Sri Ardhyastuti, Safira Rahmah, Tati Zera
This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.
Editorial Office of Jurnal Neutrino:
Department of Physics, Faculty of Sains and Technology, Universitas Islam Negeri Maulana Malik Ibrahim Malang, Indonesia
B.J. Habibie 2nd Floor
Gajayana st. No.50 Malang 65144
Telp. +62 813-4090-1818
Email: neutrino@uin-malang.ac.id
This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License
