TY - GEN
T1 - Identification fluid content using AVO analysis and elastic impedance (EI) inversion on "v" field Cekungan Kutai, Kalimantan Timur
AU - Hutasoit, V.
AU - Rosid, M. S.
N1 - Publisher Copyright:
© 2018 Author(s).
PY - 2018/10/22
Y1 - 2018/10/22
N2 - A study case of identification fluid content using AVO (Amplitude Variation with Offset) analysis and Elastic Impedance (EI) inversion on "V" field located at Kutai Basin was done. Seismic partial angle stack was processed by using analysis of AVO and Elastic Impedance inversion produced output section such as Intercept (A), Gradient (B), Product (A.B), Scaled Poisson's Ratio Changed, Near Angle Inverted, and Far Angle Inverted for further interpretation. AVO attribute analysis performed on the data field was included in class III AVO anomalies (low impedance contrast sand), and the Elastic Impedance inversion process was further performed by the three well (VB2, VA1ST, VA3) data processing and create log near EI and far EI as the inversion process controller. Well cross-plot between wells and inverted EI was also performed to determine the cross-section distribution on fluid in the reservoir. Result obtained in cross section inverted near angle zone that the gas is at the value of 9000 (ft/s)∗(g/cc) up to 14200 (ft/s)∗(g/cc), and the cross-section inverted far angle that the gas is at the value of 1100 (ft/s)∗(g/cc) up to 1600 (ft/s)∗(g/cc) at top reservoir in the period 2900-3300 ms. By slicing top reservoir map of AVO attribute and Inverted EI, reservoir distribution of reservoir sandstone have orientation direction from West to East until South-East.
AB - A study case of identification fluid content using AVO (Amplitude Variation with Offset) analysis and Elastic Impedance (EI) inversion on "V" field located at Kutai Basin was done. Seismic partial angle stack was processed by using analysis of AVO and Elastic Impedance inversion produced output section such as Intercept (A), Gradient (B), Product (A.B), Scaled Poisson's Ratio Changed, Near Angle Inverted, and Far Angle Inverted for further interpretation. AVO attribute analysis performed on the data field was included in class III AVO anomalies (low impedance contrast sand), and the Elastic Impedance inversion process was further performed by the three well (VB2, VA1ST, VA3) data processing and create log near EI and far EI as the inversion process controller. Well cross-plot between wells and inverted EI was also performed to determine the cross-section distribution on fluid in the reservoir. Result obtained in cross section inverted near angle zone that the gas is at the value of 9000 (ft/s)∗(g/cc) up to 14200 (ft/s)∗(g/cc), and the cross-section inverted far angle that the gas is at the value of 1100 (ft/s)∗(g/cc) up to 1600 (ft/s)∗(g/cc) at top reservoir in the period 2900-3300 ms. By slicing top reservoir map of AVO attribute and Inverted EI, reservoir distribution of reservoir sandstone have orientation direction from West to East until South-East.
KW - AVO
KW - Elastic Impedance (EI)
KW - inversion
UR - http://www.scopus.com/inward/record.url?scp=85056078982&partnerID=8YFLogxK
U2 - 10.1063/1.5064240
DO - 10.1063/1.5064240
M3 - Conference contribution
AN - SCOPUS:85056078982
T3 - AIP Conference Proceedings
BT - Proceedings of the 3rd International Symposium on Current Progress in Mathematics and Sciences 2017, ISCPMS 2017
A2 - Yuniati, Ratna
A2 - Mart, Terry
A2 - Anggraningrum, Ivandini T.
A2 - Triyono, Djoko
A2 - Sugeng, Kiki A.
PB - American Institute of Physics Inc.
T2 - 3rd International Symposium on Current Progress in Mathematics and Sciences 2017, ISCPMS 2017
Y2 - 26 July 2017 through 27 July 2017
ER -