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dc.contributor.authorAmbusso, W.
dc.contributor.authorOdek, A.B.
dc.contributor.authorOdek, A.
dc.contributor.authorGithiri, J.G.
dc.date.accessioned2014-08-08T08:59:52Z
dc.date.available2014-08-08T08:59:52Z
dc.date.issued2014-02-25
dc.identifier.citationJournal of Agriculture, Science and Technologyen_US
dc.identifier.urihttp://ir-library.ku.ac.ke/handle/123456789/10851
dc.description.abstractIn order to fully assess the potential of Homa Hills Geothermal prospect, the heat source which is one of the main features of a geothermal system had to be located based on its perturbation on the gravity field. Ground gravity survey was conducted in an area covering about 76 km2 and the data processed to remove all other effects which are not of geological interest. Qualitative interpretation was attempted and cross sections drawn across the anomalous areas on the complete Bouguer anomaly map. Quantitative interpretation attempted involved both Euler Deconvolution and 2‐D Forward modelling. The parameters obtained from Euler Deconvolution were used as the start up parameters for 2‐D Forward modeling. Well clustered Euler solutions were obtained at a shallow depth of approximately 200‐750 m which is consistent with the modeled shallow dike like intrusive probably of carbonatite origin.en_US
dc.language.isoenen_US
dc.subjectgravity,en_US
dc.subjectAnomalies,en_US
dc.subjectHoma Hills,en_US
dc.subjectheat source,en_US
dc.subjectEuler‐Deconvolutionen_US
dc.title2D-Euler Deconvolution and Forward Modeling of Gravity Data of Homa-Hills Geothermal Prospect, Kenyaen_US
dc.typeArticleen_US


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