Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation

A Yin - Earth-Science Reviews, 2006 - Elsevier
Despite a long research history over the past 150 years, the geometry, kinematics, and
dynamic evolution of the Himalayan orogen remain poorly understood. This is mainly due to …

An overview of the stratigraphy and tectonics of the Nepal Himalaya

BN Upreti - Journal of Asian Earth Sciences, 1999 - Elsevier
Nepal can be divided into the following five east–west trending major tectonic zones.(i) The
Terai Tectonic Zone which consists of over one km of Recent alluvium concealing the Churia …

Climate change over the Himalayas

TP Sabin, R Krishnan, R Vellore, P Priya… - … A report of the Ministry of …, 2020 - Springer
• Future climate projections under various CMIP5 scenarios suggest warming of the HKH
region in the range of 2.6–4.6 C by the end of the twenty-first century. While future …

Tectonics of the Himalaya and southern Tibet from two perspectives

KV Hodges - Geological Society of America Bulletin, 2000 - pubs.geoscienceworld.org
Abstract The Himalaya and Tibet provide an unparalleled opportunity to examine the
complex ways in which continents respond to collisional orogenesis. This paper is an …

Stratigraphy, structure, and tectonic evolution of the Himalayan fold‐thrust belt in western Nepal

PG DeCelles, DM Robinson, J Quade, TP Ojha… - …, 2001 - Wiley Online Library
Regional mapping, stratigraphic study, and 40Ar/39Ar geochronology provide the basis for
an incremental restoration of the Himalayan fold‐thrust belt in western Nepal …

Implications of shortening in the Himalayan fold‐thrust belt for uplift of the Tibetan Plateau

PG DeCelles, DM Robinson, G Zandt - Tectonics, 2002 - Wiley Online Library
Recent research in the Himalayan fold‐thrust belt provides two new sets of observations that
are crucial to understanding the evolution of the Himalayan‐Tibetan orogenic system. First …

Channel flow, ductile extrusion and exhumation in continental collision zones: an introduction

L Godin, D Grujic, RD Law… - Geological Society, London …, 2006 - lyellcollection.org
The channel flow model aims to explain features common to metamorphic hinterlands of
some collisional orogens, notably along the Himalaya-Tibet system. Channel flow describes …

Comparisons of the kinematics and deep structures of the Zagros and Himalaya and of the Iranian and Tibetan plateaus and geodynamic implications

D Hatzfeld, P Molnar - Reviews of Geophysics, 2010 - Wiley Online Library
We compare the geologic histories, the deep structures, and the present‐day kinematics of
deformation of the Himalaya and the adjacent Tibetan Plateau with those of the Zagros and …

The South Tibetan detachment and the Manaslu leucogranite: A structural reinterpretation and restoration of the Annapurna-Manaslu Himalaya, Nepal

MP Searle, L Godin - The Journal of geology, 2003 - journals.uchicago.edu
Abstract The South Tibetan Detachment (STD) System comprises both ductile shear zones
and brittle low-angle extensional faults bounding the upper (northern) margin of the high …

The kinematic evolution of the Nepalese Himalaya interpreted from Nd isotopes

DM Robinson, PG DeCelles, PJ Patchett… - Earth and Planetary …, 2001 - Elsevier
Neodymium (Nd) isotopes from the Himalayan fold-thrust belt and its associated foreland
basin deposits are useful for distinguishing between Himalayan tectonostratigraphic zones …