DISTRIBUTION OF CARBONATE RESERVOIR USING AMPLITUDE VERSUS AZIMUTH (AVAZ) OF 3D SEISMIC DATA "SWZ" FIELD OF TUBAN FORMATION, EAST JAVA, INDONESIA

Main Author: noviyanti, shinta; brawijaya university
Format: Article application/pdf eJournal
Bahasa: eng
Terbitan: Department of Physics - Faculty of Science , 2013
Online Access: http://physics.studentjournal.ub.ac.id/index.php/psj/article/view/15
http://physics.studentjournal.ub.ac.id/index.php/psj/article/downloadSuppFile/15/44
ctrlnum article-15
fullrecord <?xml version="1.0"?> <dc schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><title lang="en-US">DISTRIBUTION OF CARBONATE RESERVOIR USING AMPLITUDE VERSUS AZIMUTH (AVAZ) OF 3D SEISMIC DATA "SWZ" FIELD OF TUBAN FORMATION, EAST JAVA, INDONESIA</title><creator>noviyanti, shinta; brawijaya university</creator><description lang="en-US">Seismic response of a medium depends on many factor one of them is porosity and saturation. There are seismic amplitude dependent offset changes within the same lithology&#xA0; when the different pore fluid types and saturations are introduced. Amplitude versus offset (AVO) method that works in reflectivity domain used to identify and analyze hydrocarbon anomaly. But, in some cases we need deeper analysis to predict the axistence of hydrocarbon of carbonate reservoir .In this study to identify the presence of hydrocarbons in the Formation Tuban in East Java Basin using the AVO application Amplitude Versus Azimuth (AVAZ). AVAZ method is a method to identify a distribution based on the AVO effect that appear in direction of reservoir fracture. To determine the fracture direction, gradient of attenuation to offset is used in every measurement direction.</description><publisher lang="en-US">Department of Physics - Faculty of Science</publisher><contributor lang="en-US"/><date>2013-04-26</date><type>Journal:Article</type><type>File:application/pdf</type><identifier>http://physics.studentjournal.ub.ac.id/index.php/psj/article/view/15</identifier><source lang="en-US">Physics Student Journal; Vol 1, No 1 (2013); pp.62-64</source><language>eng</language><relation>http://physics.studentjournal.ub.ac.id/index.php/psj/article/downloadSuppFile/15/44</relation><recordID>article-15</recordID></dc>
language eng
format Journal:Article
Journal
File:application/pdf
File
Journal:eJournal
author noviyanti, shinta; brawijaya university
title DISTRIBUTION OF CARBONATE RESERVOIR USING AMPLITUDE VERSUS AZIMUTH (AVAZ) OF 3D SEISMIC DATA "SWZ" FIELD OF TUBAN FORMATION, EAST JAVA, INDONESIA
publisher Department of Physics - Faculty of Science
publishDate 2013
url http://physics.studentjournal.ub.ac.id/index.php/psj/article/view/15
http://physics.studentjournal.ub.ac.id/index.php/psj/article/downloadSuppFile/15/44
contents Seismic response of a medium depends on many factor one of them is porosity and saturation. There are seismic amplitude dependent offset changes within the same lithology when the different pore fluid types and saturations are introduced. Amplitude versus offset (AVO) method that works in reflectivity domain used to identify and analyze hydrocarbon anomaly. But, in some cases we need deeper analysis to predict the axistence of hydrocarbon of carbonate reservoir .In this study to identify the presence of hydrocarbons in the Formation Tuban in East Java Basin using the AVO application Amplitude Versus Azimuth (AVAZ). AVAZ method is a method to identify a distribution based on the AVO effect that appear in direction of reservoir fracture. To determine the fracture direction, gradient of attenuation to offset is used in every measurement direction.
id IOS2367.article-15
institution Universitas Brawijaya
affiliation mill.onesearch.id
fkp2tn.onesearch.id
institution_id 30
institution_type library:university
library
library Perpustakaan Universitas Brawijaya
library_id 480
collection Physics Student Journal
repository_id 2367
subject_area Fisika
city MALANG
province JAWA TIMUR
repoId IOS2367
first_indexed 2016-09-22T20:46:14Z
last_indexed 2016-09-22T20:46:14Z
recordtype dc
_version_ 1713030900439056384
score 17.203505