U–Pb age data of detrital zircons from Tethyan Himalaya (TH) strata, Lesser Himalaya (LH) strata, Cryogenian Blaini Formation (LH), Cryogenian Manjir Formation (TH), and Ediacaran Phe Formation (TH)
The Jurassic-Cretaceous (Upper Tethyan) flysch well exposed in the Thakkhola Section, Nepal, was dep...
The Jurassic-Cretaceous (Upper Tethyan) flysch well exposed in the Thakkhola Section, Nepal, was dep...
SHRIMP U-Pb dating of zircons from a peralkaline S-type Lesser Himalayan granite from the Kathmandu ...
AbstractSubstantial part of the northern margin of Indian plate is subducted beneath the Eurasian pl...
The isotope geochronology of isochronously deposited Cambrian strata from different tectonostratigra...
The isotope geochronology of isochronously deposited Cambrian strata from different tectonostratigra...
Orthogneiss within the Paleoproterozoic strata of Lesser Himalayan sequence across the Himalaya has ...
The lower Lesser Himalayan sequence marks the northern extremity of the exposed Indian plate, and i...
The lower Lesser Himalayan sequence marks the northern extremity of the exposed Indian plate, and i...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The Himalayan orogen is a type example of continent-continent collision. Knowledge of the timing of ...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The metamorphic core of the Himalaya is composed of Indian cratonic rocks with two distinct crustal ...
AbstractSubstantial part of the northern margin of Indian plate is subducted beneath the Eurasian pl...
The Jurassic-Cretaceous (Upper Tethyan) flysch well exposed in the Thakkhola Section, Nepal, was dep...
The Jurassic-Cretaceous (Upper Tethyan) flysch well exposed in the Thakkhola Section, Nepal, was dep...
SHRIMP U-Pb dating of zircons from a peralkaline S-type Lesser Himalayan granite from the Kathmandu ...
AbstractSubstantial part of the northern margin of Indian plate is subducted beneath the Eurasian pl...
The isotope geochronology of isochronously deposited Cambrian strata from different tectonostratigra...
The isotope geochronology of isochronously deposited Cambrian strata from different tectonostratigra...
Orthogneiss within the Paleoproterozoic strata of Lesser Himalayan sequence across the Himalaya has ...
The lower Lesser Himalayan sequence marks the northern extremity of the exposed Indian plate, and i...
The lower Lesser Himalayan sequence marks the northern extremity of the exposed Indian plate, and i...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The Himalayan orogen is a type example of continent-continent collision. Knowledge of the timing of ...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The collision of India and Asia can be defined as a process that started with the closing of the Tet...
The metamorphic core of the Himalaya is composed of Indian cratonic rocks with two distinct crustal ...
AbstractSubstantial part of the northern margin of Indian plate is subducted beneath the Eurasian pl...
The Jurassic-Cretaceous (Upper Tethyan) flysch well exposed in the Thakkhola Section, Nepal, was dep...
The Jurassic-Cretaceous (Upper Tethyan) flysch well exposed in the Thakkhola Section, Nepal, was dep...
SHRIMP U-Pb dating of zircons from a peralkaline S-type Lesser Himalayan granite from the Kathmandu ...