Petroleum systems and hydrocarbon potential of the North-West Himalaya of India and Pakistan
The Himalayan orogeny has shaped the sedimentary basins of the region, where
continuous deformation formed both 'conventional'and 'unconventional'petroleum systems at …
continuous deformation formed both 'conventional'and 'unconventional'petroleum systems at …
Tracking basement cross-strike discontinuities in the Indian crust beneath the Himalayan orogen using gravity data–relationship to upper crustal faults
The Himalaya is the result of the on-going convergence and collision of India and Asia. The
internal configuration and processes that govern the rise of the Himalayan Mountains and …
internal configuration and processes that govern the rise of the Himalayan Mountains and …
Lithosphere structure in the collision zone of the NW Himalayas revealed by alocal earthquake tomography
In this study, we obtained new 3D seismic tomography models of the crust and uppermost
mantle beneath the northwestern Himalayas down to a depth of 120 km. The data were …
mantle beneath the northwestern Himalayas down to a depth of 120 km. The data were …
Shear wave crustal velocity structure in the Garhwal-Kumaon Himalaya based on noise cross-correlation of Rayleigh wave
SK Verma, N Kumar, D Hazarika, A Paul, DK Yadav… - Tectonophysics, 2023 - Elsevier
The tectonics of the Garwal-Kumaon Himalaya is characterized by thrusts, tectonic windows,
and klippen. We investigate crustal shear wave velocity variations using ambient noise cross …
and klippen. We investigate crustal shear wave velocity variations using ambient noise cross …
[HTML][HTML] Regional gravity field distribution over cratonic domains of the Indian shield: Implications for lithospheric evolution and destruction
A Vasanthi, M Santosh - Geosystems and Geoenvironment, 2022 - Elsevier
The nature of crust and lithospheric mantle evolution of the Archean shields and their
subsequent destruction through intraplate tectonic processes are important in understanding …
subsequent destruction through intraplate tectonic processes are important in understanding …
Structure and geodynamic evolution of the lithosphere below northwest indian shield: constraints from geological, geochronological and multi-scale potential field …
Abstract The Northwest Indian shield (NWIS) comprises of Archean cratons such as the
Bundelkhand (Bh. C), Marwar (MC) and Dharwar (DC), the intervening Proterozoic mobile …
Bundelkhand (Bh. C), Marwar (MC) and Dharwar (DC), the intervening Proterozoic mobile …
Crustal structure and lateral variations in Moho beneath the Delhi fold belt, NW India: Insight from gravity data modeling and inversion
Abstract The Proterozoic Delhi fold belt (DFB) in NW India shows a prominent NNE-SSW
trending gravity high, but its northward extension beneath Gangetic alluvium lack …
trending gravity high, but its northward extension beneath Gangetic alluvium lack …
Lithospheric density structure and effective elastic thickness beneath Himalaya and Tibetan plateau: Inference from the integrated analysis of gravity, geoid, and …
Investigation of deep crustal and lithospheric structures is essential to understand the nature
of geodynamical processes beneath the Himalaya and Tibetan plateau of the India‐Eurasia …
of geodynamical processes beneath the Himalaya and Tibetan plateau of the India‐Eurasia …
Lithosphere, crust and basement ridges across Ganga and Indus basins and seismicity along the Himalayan front, India and Western Fold Belt, Pakistan
Spectral analysis of the digital data of the Bouguer anomaly of North India including Ganga
basin suggest a four layer model with approximate depths of 140, 38, 16 and 7 km. They …
basin suggest a four layer model with approximate depths of 140, 38, 16 and 7 km. They …
Delineation of lithosphere structure and characterization of the Moho geometry under the Himalaya–Karakoram–Tibet collision zone using surface-wave tomography
Group velocities for a period range of 6–60 s for the fundamental mode of the Rayleigh wave
passing across the Himalaya–Karakoram–Tibet orogen are used to delineate the structure …
passing across the Himalaya–Karakoram–Tibet orogen are used to delineate the structure …