Deformation processes of crustal-scale faults depending on depth: Studies of paleo- and active orogenic belts from Indian continent

概要

Thesis Abstract
Deformation processes of crustal-scale faults depending on depth: Studies of paleo- and
active orogenic belts from Indian continent
(深度に依存する地殻スケール断層の変形過程：インド大陸における古造山帯と
活動的な造山帯の研究)
Dyuti Prakash Sarkar
Department of Earth and Planetary Systems Science,
Graduate School of Science,
Hiroshima University

Content of the thesis
Abstract
Table of contents
List of figures
List of tables
Acknowledgments
Chapter 1 GENERAL INTRODUCTION
Chapter 2 INTEGRATED STUDIES ON DEFORMATION MECHANISMS
AND TECTONIC IMPLICATIONS FROM SERPENTINITES OF
THE RAKHABDEV LINEAMENT IN WESTERN INDIA
Chapter 3 DEFORMATION MICROSTRUCTURES AND DETRITAL ZIRCON
GEOCHRONOLOGY OF FAULT ROCKS FROM MAIN
BOUNDARY THRUST (MBT) IN NORTH-WEST HIMALAYAS
Chapter 4 FAULT
ZONE
ARCHITECTURE
AND
DEFORMATION
MECHANISMS FROM THE NAHAN THRUST (NT) IN
NORTH-WEST HIMALAYAS
Chapter 5 CARBONATE CLUMPED ISOTOPE THERMOMETRY AS AN
ALTERNATIVE
IN
ESTIMATING
DEFORMATION
TEMPERATURES FROM MBT AND NT
Chapter 6 SUMMARY
References