Technical feasibility of heavy minerals in Southwestern and Northwestern onshore and offshore regions of Sri Lanka

dc.contributor.advisorRatnayake, NP
dc.contributor.advisorWeerawarnakula, S
dc.contributor.advisorJinadasa, SUP
dc.contributor.authorKananathan, A
dc.date.accept2018
dc.date.accessioned2018
dc.date.available2018
dc.date.issued2018
dc.description.abstractBeach sediments in Sri Lanka consist of industrial grade heavy mineral occurrences. Most of the previous studies have targeted to identify mineral compositions rather than the provenance of these beach sediments. In this study, the offshore and onshore sediments were collected for identifying heavy minerals compositions. In addition, the long-term coastal morphodynamic changes were analyzed in the coastline of Sri Lanka, with the monsoonal changes. These coastal morphodynamic changes were used to identify the coastal sediment accretion and depositional trends, and its relationship to the heavy mineral provenance. Results suggest the concentration of detrital Ilmenite, Zircon, Garnet, Monazite and Rutile in onshore and offshore sediments in varying concentrations. The heavy mineral potential of the northeastern coast was high (average about 45-50% in the Verugal and 70-85% in the Pulmoddai deposits and 3.5-5.0% in the offshore samples from Nilaveli to Kokkilai (in w/w)), compared to the southwestern sediments (average about 10% in onshore and 2% in offshore Gin River mouth). Therefore, no high economic-grade heavy mineral placers have been discovered by offshore investigations. However, it may be possible to occur concentrated heavy minerals in paleo-river channels that were developed due to glacioeustatic sea-level changes. Observed high concentrated heavy minerals in beach and low concentrated offshore sediments suggest the panning system in the surf zone to form enriched placer deposits. The monsoon-derived longshore currents suggest that the sources of heavy minerals in the Pulmoddai and Verugal deposits may have probably influenced by clastic sediment supply in eastern India and Sri Lanka (the Mahaweli River), respectively. Heavy minerals in the western coast can probably derive from Precambrian metamorphic rocks and supplied to coast through river systems in Sri Lanka. The results obtained are well satisfying for the exploitation of the Verugal deposit and the mine plan was described with the considerations of analytical outcomes.en_US
dc.identifier.accnoTH3841en_US
dc.identifier.citationKananathan, A. (2018). Technical feasibility of heavy minerals in Southwestern and Northwestern onshore and offshore regions of Sri Lanka [Master’s theses, University of Moratuwa]. Institutional Repository University of Moratuwa. http://dl.lib.mrt.ac.lk/handle/123/16049
dc.identifier.degreeMaster of Philosophyen_US
dc.identifier.departmentDepartment of Earth Resources Engineeringen_US
dc.identifier.facultyEngineeringen_US
dc.identifier.urihttp://dl.lib.mrt.ac.lk/handle/123/16049
dc.language.isoenen_US
dc.subjectEARTH RESOURCES ENGINEERING-Dissertationsen_US
dc.subjectHEAVY MINERALSen_US
dc.subjectMINERALS-Sedimentationen_US
dc.subjectMINES AND MININGen_US
dc.subjectMINERAL DEPOSIT-Verugalen_US
dc.subjectMINERAL ECONOMICSen_US
dc.titleTechnical feasibility of heavy minerals in Southwestern and Northwestern onshore and offshore regions of Sri Lankaen_US
dc.typeThesis-Full-texten_US

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