Geology of Nepal and its regional frame: Thirty-third William Smith Lecture
J Stöcklin - Journal of the Geological Society, 1980 - lyellcollection.org
Since the opening of Nepal in 1950, a wealth of new information on the geology of the
Himalaya has emanated from this country. The sedimentary history of the Range is most …
Himalaya has emanated from this country. The sedimentary history of the Range is most …
Geology of Himachal Pradesh
SV Srikantia, ON Bhargava - GSI Publications, 1998 - indianjournalofentrepreneurship …
Himachal Pradesh forming an important segment of the Himalaya has been the focus of
study for over hundred years. An attempt has been made in this book to synthesize the …
study for over hundred years. An attempt has been made in this book to synthesize the …
Structure of the Chamba nappe and position of the Main Central Thrust in Kashmir Himalaya
VC Thakur - Journal of Asian Earth Sciences, 1998 - Elsevier
The Chamba nappe, composed of an approximately 8 km thick sequence of Late
Precambrian to Jurassic age rocks is located between the Higher Himalaya Crystallines …
Precambrian to Jurassic age rocks is located between the Higher Himalaya Crystallines …
Metamorphism and tectonics of the Himalaya
BF Windley - Journal of the Geological Society, 1983 - lyellcollection.org
Metamorphism connected with the main growth and deformation stages of the Himalaya
ranges from mid-Cretaceous to the Quaternary. Northward subduction gave rise in the early …
ranges from mid-Cretaceous to the Quaternary. Northward subduction gave rise in the early …
Litho-tectonic sequence and their regional correlation along the Lohit and Dibang valleys, eastern Arunachal Pradesh
DK Misra - Journal of the Geological Society of India, 2009 - Springer
Geological map** between Lohit and Dibang valleys of eastern Arunachal Pradesh
reveals the existence of five thrust bound tectonostratigraphic units. In ascending structural …
reveals the existence of five thrust bound tectonostratigraphic units. In ascending structural …
SHRIMP U-Pb c. 1860 Ma anorogenic magmatic signatures from the NW Himalaya: implications for Palaeoproterozoic assembly of the Columbia Supercontinent
The basal parts of the Higher Himalayan Crystallines (HHC), Lesser Himalayan sedimentary
sequences and mylonite zone at the base of Main Central Thrust (MCT) within the NW …
sequences and mylonite zone at the base of Main Central Thrust (MCT) within the NW …
[PDF][PDF] Himalayan granitoids
S Singh, AK Jain - Journal of the Virtual Explorer, 2003 - researchgate.net
The Himalaya is considered as a typical example of continent-continent collision between
the Indian and Eurasian Plates during Cenozoic time. The Himalayan collision zone …
the Indian and Eurasian Plates during Cenozoic time. The Himalayan collision zone …
Geochemistry of Neogene Siwalik mudstones along Punjab re-entrant, India: Implications for source-area weathering, provenance and tectonic setting
Mudstones from the Neogene Siwalik succession, east of Ravi River, Punjab re-entrant have
been analysed for major, trace and rare earth elements (REEs) used as a reliable proxy to …
been analysed for major, trace and rare earth elements (REEs) used as a reliable proxy to …
[PDF][PDF] Early Proterozoic Rb-Sr whole-rock age for central crystalline gneiss of higher Himalaya, Kumaun
VB Bhanot, VP Singh, AK Kansal… - Geological Society of …, 1977 - samvad.sibmpune.edu.in
Early Proterozoic Rb-Sr Whole:-rock Age for Central Crystalline Gneiss of Higher Himalaya,
Kumaun Page 1 (Jour. Geol. Soc. India, Vol. No.2. Feb. pp. 90 to 91) Early Proterozoic Rb-Sr …
Kumaun Page 1 (Jour. Geol. Soc. India, Vol. No.2. Feb. pp. 90 to 91) Early Proterozoic Rb-Sr …
Tectonics of the Central Crystallines of western Himalaya
VC Thakur - Tectonophysics, 1980 - Elsevier
The crystalline sheet of the Higher Himalaya, referred to as the Central Crystallines, is a
continuous lithotectonic unit which can be traced from the River Kali of eastern Kumaun in …
continuous lithotectonic unit which can be traced from the River Kali of eastern Kumaun in …