PEMROSESAN DATA SEISMIK REFLEKSI UNTUK IDENTIFIKASI PERLAPISAN BATUBARA DI MANGUPEH KABUPATEN TEBO PROVINSI JAMBI

Survey with shallow seismic reflection method has been carried out in Tebo regency, Jambi province on around December 2012, to generate seismic layering that can identify the presence of coal at a certain depth and describe the subsurface geology. The data are a 2D land reflection seismic data with...

وصف كامل

محفوظ في:
التفاصيل البيبلوغرافية
المؤلفون الرئيسيون: , WAHYU SETYO HUTOMO, , Prof. Dr. Sismanto.
التنسيق: Theses and Dissertations NonPeerReviewed
منشور في: [Yogyakarta] : Universitas Gadjah Mada 2014
الموضوعات:
ETD
الوصول للمادة أونلاين:https://repository.ugm.ac.id/129124/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=69502
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المؤسسة: Universitas Gadjah Mada
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spelling id-ugm-repo.1291242016-03-04T08:16:55Z https://repository.ugm.ac.id/129124/ PEMROSESAN DATA SEISMIK REFLEKSI UNTUK IDENTIFIKASI PERLAPISAN BATUBARA DI MANGUPEH KABUPATEN TEBO PROVINSI JAMBI , WAHYU SETYO HUTOMO , Prof. Dr. Sismanto. ETD Survey with shallow seismic reflection method has been carried out in Tebo regency, Jambi province on around December 2012, to generate seismic layering that can identify the presence of coal at a certain depth and describe the subsurface geology. The data are a 2D land reflection seismic data with seg-y format that will be processed with using ProMAX software. Seg-y data are combined with field geometry data in processing of header load, then is carried out noise reduction (trace editing and filtering), seismic signal amplification (deconvolution and TAR) and eliminating the influence of topography. Gather data are ready for velocity analysis by choosing the right velocity, and according to the semblance. Residual static correction is done to fix the reflector continuity in stack display. The final stage of the process above will produce velocity that will be migrated. The migration process is done to shift the position of the reflector to the actual position by using Post Stack Time Migration Method in order to obtain the final result of stacking seismic section. Seismic section at the time domain is converted into the depth domain for easy identification of the coal bedding and geological structure. At seismic section resulted, it can be seen layers of coal in several depths in accordance with previous geological studies, namely shallow drilling (coring) and outcrop on the surface. In seismic section, it also shows different geological structures such as shear fault structures. [Yogyakarta] : Universitas Gadjah Mada 2014 Thesis NonPeerReviewed , WAHYU SETYO HUTOMO and , Prof. Dr. Sismanto. (2014) PEMROSESAN DATA SEISMIK REFLEKSI UNTUK IDENTIFIKASI PERLAPISAN BATUBARA DI MANGUPEH KABUPATEN TEBO PROVINSI JAMBI. UNSPECIFIED thesis, UNSPECIFIED. http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=69502
institution Universitas Gadjah Mada
building UGM Library
country Indonesia
collection Repository Civitas UGM
topic ETD
spellingShingle ETD
, WAHYU SETYO HUTOMO
, Prof. Dr. Sismanto.
PEMROSESAN DATA SEISMIK REFLEKSI UNTUK IDENTIFIKASI PERLAPISAN BATUBARA DI MANGUPEH KABUPATEN TEBO PROVINSI JAMBI
description Survey with shallow seismic reflection method has been carried out in Tebo regency, Jambi province on around December 2012, to generate seismic layering that can identify the presence of coal at a certain depth and describe the subsurface geology. The data are a 2D land reflection seismic data with seg-y format that will be processed with using ProMAX software. Seg-y data are combined with field geometry data in processing of header load, then is carried out noise reduction (trace editing and filtering), seismic signal amplification (deconvolution and TAR) and eliminating the influence of topography. Gather data are ready for velocity analysis by choosing the right velocity, and according to the semblance. Residual static correction is done to fix the reflector continuity in stack display. The final stage of the process above will produce velocity that will be migrated. The migration process is done to shift the position of the reflector to the actual position by using Post Stack Time Migration Method in order to obtain the final result of stacking seismic section. Seismic section at the time domain is converted into the depth domain for easy identification of the coal bedding and geological structure. At seismic section resulted, it can be seen layers of coal in several depths in accordance with previous geological studies, namely shallow drilling (coring) and outcrop on the surface. In seismic section, it also shows different geological structures such as shear fault structures.
format Theses and Dissertations
NonPeerReviewed
author , WAHYU SETYO HUTOMO
, Prof. Dr. Sismanto.
author_facet , WAHYU SETYO HUTOMO
, Prof. Dr. Sismanto.
author_sort , WAHYU SETYO HUTOMO
title PEMROSESAN DATA SEISMIK REFLEKSI UNTUK IDENTIFIKASI PERLAPISAN BATUBARA DI MANGUPEH KABUPATEN TEBO PROVINSI JAMBI
title_short PEMROSESAN DATA SEISMIK REFLEKSI UNTUK IDENTIFIKASI PERLAPISAN BATUBARA DI MANGUPEH KABUPATEN TEBO PROVINSI JAMBI
title_full PEMROSESAN DATA SEISMIK REFLEKSI UNTUK IDENTIFIKASI PERLAPISAN BATUBARA DI MANGUPEH KABUPATEN TEBO PROVINSI JAMBI
title_fullStr PEMROSESAN DATA SEISMIK REFLEKSI UNTUK IDENTIFIKASI PERLAPISAN BATUBARA DI MANGUPEH KABUPATEN TEBO PROVINSI JAMBI
title_full_unstemmed PEMROSESAN DATA SEISMIK REFLEKSI UNTUK IDENTIFIKASI PERLAPISAN BATUBARA DI MANGUPEH KABUPATEN TEBO PROVINSI JAMBI
title_sort pemrosesan data seismik refleksi untuk identifikasi perlapisan batubara di mangupeh kabupaten tebo provinsi jambi
publisher [Yogyakarta] : Universitas Gadjah Mada
publishDate 2014
url https://repository.ugm.ac.id/129124/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=69502
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