Please use this identifier to cite or link to this item: http://hdl.handle.net/10603/67952
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dc.coverage.spatialPhysics
dc.date.accessioned2016-01-05T10:00:32Z-
dc.date.available2016-01-05T10:00:32Z-
dc.identifier.urihttp://hdl.handle.net/10603/67952-
dc.description.abstractThis thesis embodies the results of (i) the geochronological investigation on the co-existing zircon, sphene and apatite minerals from the granite plutons viz. of Hamren, Umroi and Nongkhlow areas of the Assam - Meghalaya plateau by the Fission Track Dating(FTD) technique (ii) track annealing studies of the minerals along with the correction of the observed minerals ages ; (iii) the estimation of the uranium content of the whole rock samples as well as of the dated minerals and (iv) the cooling and uplift rated of the rocks, The calculated fission track ages of the co-existing apatite, sphene and zircon collected from the Hamren, Umroi and Nongkhlow granite plutons of the Assam-Meghalaya plateau are given below in table 1. Table 1 Fission Track Ages of co-existing apatite, sphene and zircon According to the above data, the co-existing minerals of the Umroi and the Nongkhlow granites of Megha-laya show very close ages but lower than those shown by the minerals of the Hamren granite of Assam. The discrepancy of FT ages between co-existing minerals can be explained by different cooling ages of these minerals and the slow crystallization of the rock or by part annealing of apatite and sphene. Further, it may be mentioned that the zircon, sphene and apatite are the minerals having annealing temperatures in the decreasing order and thus their ages reflect meaningful successive geothermal events of gradually lower intensity in the history of these rocks. The results on study of annealing behaviour of the minerals collected from the Umroi, the Nongkhlow and the Hamren granites is shown in the table II. Table II Annealing behaviour of the co-existing apatite and sphene. The study of annealing behaviour of the co-exist-ing apatite and sphene of Umroi and Nongkhlow granite reveals that the apatite and the sphene must be heated upto 3800C and 7030C respectively for one hour for complete fading of tracks. It is seen that the activation energy ranges from 1.48 eV to 2.81 eV for apatite and 2.42 eV to 5.37 eV for sphene as...
dc.format.extent
dc.languageEnglish
dc.relation
dc.rightsuniversity
dc.titleFission track ages of some coexisting minerals in granites of AssamMeghalaya plateau
dc.title.alternative
dc.creator.researcherChakravarty, Arundhati
dc.subject.keywordCo-Existing
dc.subject.keywordCrystallization
dc.subject.keywordDiscrepancy
dc.subject.keywordFission
dc.subject.keywordGeochronological
dc.subject.keywordGranites
dc.subject.keywordMinerals
dc.subject.keywordTemperatures
dc.description.noteData not available
dc.contributor.guidePathak, K M
dc.publisher.placeGuwahati
dc.publisher.universityGauhati University
dc.publisher.institutionDepartment of Physics
dc.date.registeredn.d.
dc.date.completed31/12/1986
dc.date.awardedn.d.
dc.format.dimensions
dc.format.accompanyingmaterialNone
dc.source.universityUniversity
dc.type.degreePh.D.
Appears in Departments:Department of Physics

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01_title page.pdfAttached File14.12 kBAdobe PDFView/Open
02_certificate.pdf20.35 kBAdobe PDFView/Open
03_abstract.pdf78.56 kBAdobe PDFView/Open
04_preface.pdf31.25 kBAdobe PDFView/Open
05_content.pdf72.49 kBAdobe PDFView/Open
06_chapter 1.pdf101 kBAdobe PDFView/Open
07_chapter 2.pdf1.18 MBAdobe PDFView/Open
08_chapter 3.pdf531.99 kBAdobe PDFView/Open
09_chapter 4.pdf1.96 MBAdobe PDFView/Open
10_chapter 5.pdf552.94 kBAdobe PDFView/Open
11_chapter 6.pdf287.12 kBAdobe PDFView/Open
12_chapter 7.pdf600.42 kBAdobe PDFView/Open
13_chapter 8.pdf103.25 kBAdobe PDFView/Open
14_discussion and conclusions.pdf127.49 kBAdobe PDFView/Open
15_bibliography.pdf261.01 kBAdobe PDFView/Open
16_list of publications by the author.pdf18.4 kBAdobe PDFView/Open
17_acknowledgement.pdf29.98 kBAdobe PDFView/Open


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