Please use this identifier to cite or link to this item: http://hdl.handle.net/10603/67644
Title: Fission track studies on some accessory minerals in granites of Meghalaya
Researcher: Talukdar, Bhupen Chandra
Guide(s): Pathak, K M
Keywords: Apatite
Fossil
Granites
Ionisation
Minerals
Mylliem
Sphene
Thermal
University: Gauhati University
Completed Date: 31/07/1983
Abstract: Fission track ages of apatite and sphene minerals from Mylliem granite (MG), South-Khasi batholith (SK) and Nongpoh granite (NG) have been studied in the Departments of Physics and Geology, Gauhati University during 1979-83. The estimated ages are as follows. The results indicate a difference of age between the co-existing apatite and sphene of about 200 m.y. which may be explained by early crystallization of sphene and slow crystallization of the rock (as also evidenced by the very coarse-grained, porphyritic nature of the granites) and/or part annealing of apatite. The annealing behaviour of the minerals is also studied. It is seen that the apatite and sphene collected from Mylliem granite must be heated to temperature above 3980C and 7070C for one hour respectively for complete fading of tracks. It is found that the activation energy ranges from 1.2 eV to 2.4 eV for apatite and from 2.5 eV to 5.4 eV for sphene. The mean fission track ages for muscovites of the pegmatines from Nengkhra, Garo Hills and from Nongkhlow, Khasi Hills are found to be (531+_15) m.y. and (501+_25) m.y. respectively. Study on dependence of track density on anneal-ing time and temperature on muscovite indicates that muscovite will lose all tracks if it remains at a temperature 5270C for one hour. Activation energy of muscovites ranges from 1.0 eV to 2.8 eV. The present investigation uranium concentration in the three granites of Meghalaya ranges from (1.64+_0.04) to (2.94+_0.04) ppm by weight. Uranium concentration in water samples collected from different parts of Assam are measured by using SSNTD. Nothing abnormal in the U-content of various water sources of the region is observed. The results are compared with those of other workers wherever available.
Pagination: 
URI: http://hdl.handle.net/10603/67644
Appears in Departments:Department of Physics

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02_certificate.pdf35.85 kBAdobe PDFView/Open
03_abstract.pdf51.49 kBAdobe PDFView/Open
04_preface.pdf80.67 kBAdobe PDFView/Open
05_content.pdf127.81 kBAdobe PDFView/Open
06_chapter 1.pdf98.5 kBAdobe PDFView/Open
07_chapter 2.pdf257.87 kBAdobe PDFView/Open
08_chapter 3.pdf439.26 kBAdobe PDFView/Open
09_chapter 4.pdf3.32 MBAdobe PDFView/Open
10_chapter 5.pdf684.9 kBAdobe PDFView/Open
11_chapter 6.pdf497.2 kBAdobe PDFView/Open
12_chapter 7.pdf372.87 kBAdobe PDFView/Open
13_chapter 8.pdf113.49 kBAdobe PDFView/Open
14_general conclusion.pdf176.29 kBAdobe PDFView/Open
15_bibliography.pdf250.31 kBAdobe PDFView/Open
16_list of publications of the author.pdf40.68 kBAdobe PDFView/Open
17_acknowledgement.pdf42.69 kBAdobe PDFView/Open
18_appendix i.pdf31.2 kBAdobe PDFView/Open
19_appendix ii.pdf92.36 kBAdobe PDFView/Open


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