Geology Mineralogy Geochemistry and Genesis of Abiyata Diatomite in Central Main Ethiopian Rift

dc.contributor.advisorGetaneh, Worash
dc.contributor.authorHunegnaw, Yirgalem
dc.date.accessioned2022-03-04T07:55:23Z
dc.date.accessioned2023-11-09T14:13:17Z
dc.date.available2022-03-04T07:55:23Z
dc.date.available2023-11-09T14:13:17Z
dc.date.issued2021-09-09
dc.description.abstractAbiyata diatomite is situated in Central Main Ethiopian Rift (CMER) on the narrow strip of land dividing the two lakes Abiyata and Shala in the lakes district of the Ethiopian Rift Valley which is about 210 km from Addis Ababa. Geology of the deposit area is composed of Miocene to Quaternary age acidic igneous rocks consisting of pyroclastic tuff, ignimbrite and pumice and lacustrine sediments in which diatomite is hosted. Diatomite's geological, geochemical, and mineralogical features, as well as its formation, are discussed in this research. To characterize diatomite from Abiyata, chemical, mineralogical, technological, and micro paleontological examinations were conducted on samples collected from outcrops and stream sections. The XRD characteristic peaks of diatomite demonstrate that it is primarily made up of Opal-A silica, however certain crystalline phases were discovered in adequate amounts. Quartz and feldspar were the predominant crystalline phases, with lesser amounts of calcite, cristobalite, illite, mordinite, wairakite, halloysite, clinoaptilolite, adularia, and tridymite. From SEM photomicrographs diatomites are primarily formed of benthic freshwater diatom species such as Staurosirella pinnata, Staurosira construens, Pseudostaurosira brevistriata, Epithemia Sorex and surirella pinnata. Diatom species, sedimentary profile sections and mineralogical data suggest that diatomite was deposited in lacustrine-type freshwater shallow lake environment. Chemical data obtained from 10 diatomite samples show that while silica is the bodybuilding material for diatomite. i.e., Silica (SiO2), 76.9%; Alumina (Al2O3), 3.49%; Sodium Oxide (Na2O), 1.52%; Potassium Oxide (K2O), 1.107%; Iron Oxide (Fe2O3), 1.1%; Loss on ignition (LOI) 13.7 and other oxides are below 1%. Studies from technological properties like physical tests, chemistry, and mineralogy and micropaleontology of Abiyata diatomite suggest that calcined diatomite can be used for waste treatment processes in the filter aid industry and as filler material.en_US
dc.identifier.urihttp://10.90.10.223:4000/handle/123456789/30426
dc.language.isoenen_US
dc.publisherAddis Ababa Universityen_US
dc.subjectAbiyataen_US
dc.subjectAmorphous Silicaen_US
dc.subjectDiatomiteen_US
dc.subjectLacustrineen_US
dc.subjectGenesisen_US
dc.subjectMineralogyen_US
dc.titleGeology Mineralogy Geochemistry and Genesis of Abiyata Diatomite in Central Main Ethiopian Riften_US
dc.typeThesisen_US

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