期刊
HELIYON
卷 9, 期 5, 页码 -出版社
CELL PRESS
DOI: 10.1016/j.heliyon.2023.e15621
关键词
Lower Goru formation; Seismic data interpretation; Seismic attributes; Petrophysical analysis; Rock physics; Contour mapping; Hydrocarbon bearing zones
An integrated approach combining petrophysical analysis, seismic data interpretation, seismic attributes analysis, lithology, mineralogy identification, and Gassmann fluid substitution was used to identify potential leads by providing information about the subsurface structure, fluid type, and physical properties of rocks. Structural interpretation using seismic data revealed an extensional regime with horst and graben structures in the study area, with two negative flower structures cutting across the Cretaceous deposits. Well data interpretation identified four possible reservoir zones in the Sawan-01 well and two zones in the Judge-01 well, with the main lithology being sandstone with thin beds of shale in the Lower Goru Formation.
The information about the subsurface structure, type of fluids present in the reservoir, and physical properties of the rocks is essential for identifying potential leads. The integrated approach of petrophysical analysis, seismic data interpretation, seismic attributes analysis, lithology, mineralogy identification, and Gassmann fluid substitution were used for this purpose. The structural interpretation with the help of seismic data indicated the extensional regime with horst and graben structures in the study area. The two negative flower structures are cutting the entire Cretaceous deposits. The depth contour map also indicate favorable structures for hydrocarbon accumulation. The four possible reservoir zones in the Sawan-01 well and two zones in the Judge-01 well at B sand and C sand levels are identified based on well data interpretation. The main lithology of the Lower Goru Formation is sandstone with thin beds of shale. The clay types confirm the marine depositional environment for Lower Goru Formation. The water substitution in the reservoir at B sand and C sand levels indicated increased P-wave velocity and density. The water substitution affected the shear wave velocity varies slightly due to density changes. The cross plots of P-impedance versus Vp/Vs ratio differentiate the sandstone with low P-impedance and low Vp/Vs ratio from shaly sandstone with high values in the reservoir area. The P-impedance and S-impedance cross plot indicate increasing gas saturation with a decrease in impedance values. The low values of Lambda-Rho and Mu-Rho indicated the gas sandstone in the cross plot.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据