Geology of the Nepal Himalaya : Regional Perspective of the Classic Collided Orogen /

Bibliographic Details
Main Author: Dhital, Megh Raj. (Author)
Corporate Author: SpringerLink (Online service)
Format: eBook
Language:English
Published: Cham : Springer International Publishing : Imprint: Springer, 2015.
Edition:1st ed. 2015.
Series:Regional Geology Reviews,
Subjects:
Table of Contents:
  • Chapter 1 Introduction
  • Part 1 Geological Setting and Physiography
  • 2 Geological Setting of Himalaya
  • 3 Physiography of Nepal
  • Part 2 Geology of Neighbouring Regions
  • 4 Northwest Himalaya
  • 5 Southeast Himalaya and Adjacent Indian Peninsula
  • Part 3 Lesser Himalaya
  • 6 Introduction to Lesser Himalaya
  • 7 Lesser Himalaya of Mahakali-Seti region
  • 8 Lesser Himalaya of Karnali-Bheri region
  • 9 Lesser Himalaya of Gandaki region
  • 10 Lesser Himalaya of Bagmati-Gosainkund region
  • 11 Lesser Himalaya of Koshi region
  • 12 Lesser Himalaya of Arun-Tamar region
  • Part 4 Higher Himalaya
  • 13 Introduction to Higher Himalaya
  • 14 Higher Himalaya of Mahakali-Seti region
  • 15 Higher Himalaya of Karnali-Bheri region
  • 16 Higher Himalaya of Gandaki region
  • 17 Higher Himalaya of Bagmati-Gosainkund region
  • 18 Higher Himalaya of Koshi region
  • 19 Higher Himalaya of Arun-Tamar region.- 20 Models of Himalayan metamorphism
  • Part 5 Tethys Himalaya
  • 21 Introduction to Tethys Himalaya
  • 22 Tethys Himalaya of Mahakali region
  • 23 Tethys Himalaya of Karnali-Bheri region (Dolpa)
  • 24 Tethys Himalaya of Ganaki region (Thakkhola)
  • 25 Tethys Himalaya of Gandaki region (Manang)
  • 26 Tethys Himalaya of Koshi region (Mount Everest and neighbourhood)
  • Part 6 Siwaliks
  • 27 Introduction to Siwaliks
  • 28 Siwaliks of Mahakali-Seti region
  • 29 Siwaliks of Karnali-Bheri region
  • 30 Siwaliks of Gandaki region
  • 31 Siwaliks of Bagmati-Gosainkund region
  • 32 Siwaliks of Koshi region
  • 33 Siwaliks of Arun-Tamar region
  • Part 7 Terai, intermontane basins, and neotectonics
  • 34 Terai and intermontane basins
  • 35 Neotectonics
  • 36 Conclusions.