Please use this identifier to cite or link to this item: http://hdl.handle.net/10603/69943
Title: Structure and metamorphism of the precambrian rocks of the area between Deoli and Rangshai Goalpara district Assam
Researcher: Bardoloi, Abhijit
Guide(s): Chowdhary, P K
Keywords: Geochronology
Metamorphism
Orthogonal
Petrochemistry
Petrographical
Physiography
Quartzofeldspathic
Terminology
University: Gauhati University
Completed Date: 31/10/1999
Abstract: This thesis embodies the results of (i) the structural study of the rocks belonging to the Precambrian Gneissic Complex of the Assam-Meghalaya plateau in the areas between Deoli and Rangshai in Goalpara district, Assam ; (ii) the petrographical as well as chemical analyses of the rocks ; (iii) the mineral chemistry analyses of the rocks and (iv) the determination of the pressure (P) - temperature(T) condition of metamorphism prevailed during the formation of these rocks, and also the nature and behaviour of fluid regime operative during metamorphism. The rocks types in the study area in order of abundance are : quartzofeldspathic gneisses (occasionally migmatised), metacalcareous rocks (calc-silicate gneisses and hornblende gneisses), metabasic rocks (amphibolites), banded iron formations, basic dykes and quartzofeldspathic veins, pods and lenses. The structural study has revealed that all the major rock types of the area except basic dykes suffered multiple deformations, and three distinct phases of folding, a number of brittle-ductile shear zones and late minor structures including three sets of joints have been recognised. F1 folds are preserved only as hooks in their type-3 interference structure with F2 folds and penetrative as well as pervasive S1 foliations are axial planar to F1 folds. F2 folds are the most dominant folds in the area and are vertical to steeply plunging upright folds. F1 and F2 folds are coaxial as well as coaxial planar with NE-SW striking F2 axial planes. Geometrical analyses of F2 folds indicate that the folds mostly belong to class 1C and they experienced different degrees (0.1-0.7) of flattening. F3 folds are warps with axial planes, striking NW-SE and effected S1 foliations and at some places, the limbs of pre-existing folds. Deformation related to brittle-ductile shear zones effected S1 foliations and at some places, the limbs of F2 folds. This shearing episode was either syn- or post- F2 folding episode. The three sets of joints represent the brittle deformation episode in the...
Pagination: 
URI: http://hdl.handle.net/10603/69943
Appears in Departments:Department of Geological Science

Files in This Item:
File Description SizeFormat 
01_title page.pdfAttached File17.49 kBAdobe PDFView/Open
02_dedicated.pdf13.01 kBAdobe PDFView/Open
03_declaration.pdf21.61 kBAdobe PDFView/Open
04_certificate.pdf154.73 kBAdobe PDFView/Open
05_content.pdf133.22 kBAdobe PDFView/Open
06_tables,figures,plates and maps.pdf12.98 kBAdobe PDFView/Open
07_acknowledgement.pdf52.28 kBAdobe PDFView/Open
08_abstract.pdf119.47 kBAdobe PDFView/Open
09_chapter 1.pdf460.16 kBAdobe PDFView/Open
10_chapter 2.pdf712.02 kBAdobe PDFView/Open
11_chapter 3.pdf3.89 MBAdobe PDFView/Open
12_chapter 4.pdf2.07 MBAdobe PDFView/Open
13_chapter 5.pdf886.61 kBAdobe PDFView/Open
14_chapter 6.pdf993.47 kBAdobe PDFView/Open
15_summary and conclusion.pdf404.6 kBAdobe PDFView/Open
16_bibliography.pdf445 kBAdobe PDFView/Open
17_appendix.pdf26.96 kBAdobe PDFView/Open


Items in Shodhganga are protected by copyright, with all rights reserved, unless otherwise indicated.