Pseudo 3D seismic using biharmonic spline interpolation

E. Yulianto; F. Abdullah; N. Novrizal; A. Riyanto

doi:10.1088/1755-1315/481/1/012054

Pseudo 3D seismic using biharmonic spline interpolation

E. Yulianto, F. Abdullah, N. Novrizal, A. Riyanto

Department of Geosciences

Research output: Contribution to journal › Conference article › peer-review

1 Citation (Scopus)

Abstract

Pseudo three dimensional (3D) seismic has been carried out to real seismic dataset using biharmonic spline interpolation. The dataset contains 11 two dimensional (2D) seismic lines with two-millisecond sampling rates and 2000 millisecond record length. Biharmonic spline interpolation was performed for each time sample using the gridding interval of 25 x 25 meter. The resulted interpolation for each time sample was combined to generate three-dimension matrix that called as pseudo-3D seismic. The results of pseudo-3D seismic data clearly showed the structural geological features, compared to 2D seismic data. The result can minimize the uncertainty of the subsurface interpretation and reduce the exploration risk.

Original language	English
Article number	012054
Journal	IOP Conference Series: Earth and Environmental Science
Volume	481
Issue number	1
DOIs	https://doi.org/10.1088/1755-1315/481/1/012054
Publication status	Published - 27 Apr 2020
Event	Life and Environmental Sciences Academics Forum 2018, LEAF 2018 - Depok, West Java, Indonesia Duration: 1 Nov 2018 → …

Keywords

2D seismic
biharmonic spline interpolation
Pseudo 3D seismic

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10.1088/1755-1315/481/1/012054

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title = "Pseudo 3D seismic using biharmonic spline interpolation",

abstract = "Pseudo three dimensional (3D) seismic has been carried out to real seismic dataset using biharmonic spline interpolation. The dataset contains 11 two dimensional (2D) seismic lines with two-millisecond sampling rates and 2000 millisecond record length. Biharmonic spline interpolation was performed for each time sample using the gridding interval of 25 x 25 meter. The resulted interpolation for each time sample was combined to generate three-dimension matrix that called as pseudo-3D seismic. The results of pseudo-3D seismic data clearly showed the structural geological features, compared to 2D seismic data. The result can minimize the uncertainty of the subsurface interpretation and reduce the exploration risk.",

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T1 - Pseudo 3D seismic using biharmonic spline interpolation

AU - Yulianto, E.

AU - Abdullah, F.

AU - Novrizal, N.

AU - Riyanto, A.

PY - 2020/4/27

Y1 - 2020/4/27

N2 - Pseudo three dimensional (3D) seismic has been carried out to real seismic dataset using biharmonic spline interpolation. The dataset contains 11 two dimensional (2D) seismic lines with two-millisecond sampling rates and 2000 millisecond record length. Biharmonic spline interpolation was performed for each time sample using the gridding interval of 25 x 25 meter. The resulted interpolation for each time sample was combined to generate three-dimension matrix that called as pseudo-3D seismic. The results of pseudo-3D seismic data clearly showed the structural geological features, compared to 2D seismic data. The result can minimize the uncertainty of the subsurface interpretation and reduce the exploration risk.

AB - Pseudo three dimensional (3D) seismic has been carried out to real seismic dataset using biharmonic spline interpolation. The dataset contains 11 two dimensional (2D) seismic lines with two-millisecond sampling rates and 2000 millisecond record length. Biharmonic spline interpolation was performed for each time sample using the gridding interval of 25 x 25 meter. The resulted interpolation for each time sample was combined to generate three-dimension matrix that called as pseudo-3D seismic. The results of pseudo-3D seismic data clearly showed the structural geological features, compared to 2D seismic data. The result can minimize the uncertainty of the subsurface interpretation and reduce the exploration risk.

KW - 2D seismic

KW - biharmonic spline interpolation

KW - Pseudo 3D seismic

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DO - 10.1088/1755-1315/481/1/012054

M3 - Conference article

AN - SCOPUS:85084728240

SN - 1755-1307

VL - 481

JO - IOP Conference Series: Earth and Environmental Science

JF - IOP Conference Series: Earth and Environmental Science

IS - 1

M1 - 012054

T2 - Life and Environmental Sciences Academics Forum 2018, LEAF 2018

Y2 - 1 November 2018

ER -

Pseudo 3D seismic using biharmonic spline interpolation

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