Please use this identifier to cite or link to this item: http://localhost:8081/jspui/handle/123456789/17476
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dc.contributor.authorShukla, Shivam-
dc.date.accessioned2025-07-01T12:43:46Z-
dc.date.available2025-07-01T12:43:46Z-
dc.date.issued2015-05-
dc.identifier.urihttp://localhost:8081/jspui/handle/123456789/17476-
dc.description.abstractFor quantitative analysis and interpretation of the reservoir quality tight sandstone reservoirs it is essential to understand the seismic properties of low-to-intermediate porosity gas-saturated sandstones (Avseth et al., 2014). Tight sandstones have generally undergone severe mechanical and geochemical compaction processes that cause a large reduction in their original porosity from the time of their deposition. The elastic properties of low-porosity rocks depend more on the specific pore structure than on the actual porosity and, in general , the bulk modulus within the crack-like porosity dominates the overall fliud reposonse. Pore fluid effects are modelled using gassmann ( 195 1) model. It is proposed to study the variation of elastic moduli and seismic wave speeds of low to intermediate porosity sandstones using the theories mentioned above. Also a comparison between theoretical and empirical results is carried outen_US
dc.description.sponsorshipINDIAN INSTITUTE OF TECHNOLOGY ROORKEEen_US
dc.language.isoenen_US
dc.publisherIIT ROORKEEen_US
dc.subjectQuantitative Analysisen_US
dc.subjectSandstone Reservoirsen_US
dc.subjectPore Fluid Effectsen_US
dc.subjectGeochemical Compaction Processesen_US
dc.titleROCK PHYSICS MODELLThG OF LOW TO INTERMEDIATE POROSITY SANDSTONESen_US
dc.typeOtheren_US
Appears in Collections:MASTERS' THESES (Earth Sci.)

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