Neotectonism and reactivation of tectonic elements in eastern part of Shillong Plateau, India: constraints from morpho-tectonic analyses

ABSTRACTThe Shillong Plateau is the only elevated topography in the Himalayan foreland bounded and crisscrossed by several prominent faults and shear zones. The plateau is situated in a complex tectonic compressional set up, owing to which the fault systems both at the periphery and within tend to b...

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Main Authors: Krishanu Nath, Shampa Halder, Dimpi Gogoi, Bashab Nandan Mahanta, Tapos Kumar Goswami, Ranjan Kumar Sarma
Format: Article
Language:English
Published: Taylor & Francis Group 2024-04-01
Series:Geology, Ecology, and Landscapes
Subjects:
Online Access:https://www.tandfonline.com/doi/10.1080/24749508.2024.2338973
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author Krishanu Nath
Shampa Halder
Dimpi Gogoi
Bashab Nandan Mahanta
Tapos Kumar Goswami
Ranjan Kumar Sarma
author_facet Krishanu Nath
Shampa Halder
Dimpi Gogoi
Bashab Nandan Mahanta
Tapos Kumar Goswami
Ranjan Kumar Sarma
author_sort Krishanu Nath
collection DOAJ
description ABSTRACTThe Shillong Plateau is the only elevated topography in the Himalayan foreland bounded and crisscrossed by several prominent faults and shear zones. The plateau is situated in a complex tectonic compressional set up, owing to which the fault systems both at the periphery and within tend to be neotectonically active. Due to the elevation difference of the plateau with the Brahmaputra and Meghna River valleys flanking it, coupled with the impervious lithologies present, an intricate network of drainage system has developed in the plateau. In this paper, morphometric and structural analyses of four selected drainage basins from the east-central part of Shillong Plateau have been carried out to comprehend the effects of neotectonic reactivation of fault systems and associated basin tilting which in turn controls the development of drainage pattern. This has led to the understanding of the effects of the ever-evolving fluvial landforms on the anthroposphere in this part of Indian sub-continent, where the agrarian-economy is completely dependent on the intricate fluvial systems.
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spelling doaj.art-2b3d8f7564944f30ba0f9b64fa4ec87b2024-04-09T15:47:26ZengTaylor & Francis GroupGeology, Ecology, and Landscapes2474-95082024-04-0111810.1080/24749508.2024.2338973Neotectonism and reactivation of tectonic elements in eastern part of Shillong Plateau, India: constraints from morpho-tectonic analysesKrishanu Nath0Shampa Halder1Dimpi Gogoi2Bashab Nandan Mahanta3Tapos Kumar Goswami4Ranjan Kumar Sarma5Geological Survey of India, Central Headquarters, Kolkata, West Bengal, IndiaGeological Survey of India, Eastern Region, Kolkata, West Bengal, IndiaGeological Survey of India, Eastern Region, Kolkata, West Bengal, IndiaGeological Survey of India, North-eastern Region, Shillong, Meghalaya, IndiaDepartment of Applied Geology, Dibrugarh University, Dibrugarh, Assam, IndiaDepartment of Applied Geology, Dibrugarh University, Dibrugarh, Assam, IndiaABSTRACTThe Shillong Plateau is the only elevated topography in the Himalayan foreland bounded and crisscrossed by several prominent faults and shear zones. The plateau is situated in a complex tectonic compressional set up, owing to which the fault systems both at the periphery and within tend to be neotectonically active. Due to the elevation difference of the plateau with the Brahmaputra and Meghna River valleys flanking it, coupled with the impervious lithologies present, an intricate network of drainage system has developed in the plateau. In this paper, morphometric and structural analyses of four selected drainage basins from the east-central part of Shillong Plateau have been carried out to comprehend the effects of neotectonic reactivation of fault systems and associated basin tilting which in turn controls the development of drainage pattern. This has led to the understanding of the effects of the ever-evolving fluvial landforms on the anthroposphere in this part of Indian sub-continent, where the agrarian-economy is completely dependent on the intricate fluvial systems.https://www.tandfonline.com/doi/10.1080/24749508.2024.2338973Shillong plateauneotectonicsmorpho-structural analysesbasin asymmetry
spellingShingle Krishanu Nath
Shampa Halder
Dimpi Gogoi
Bashab Nandan Mahanta
Tapos Kumar Goswami
Ranjan Kumar Sarma
Neotectonism and reactivation of tectonic elements in eastern part of Shillong Plateau, India: constraints from morpho-tectonic analyses
Geology, Ecology, and Landscapes
Shillong plateau
neotectonics
morpho-structural analyses
basin asymmetry
title Neotectonism and reactivation of tectonic elements in eastern part of Shillong Plateau, India: constraints from morpho-tectonic analyses
title_full Neotectonism and reactivation of tectonic elements in eastern part of Shillong Plateau, India: constraints from morpho-tectonic analyses
title_fullStr Neotectonism and reactivation of tectonic elements in eastern part of Shillong Plateau, India: constraints from morpho-tectonic analyses
title_full_unstemmed Neotectonism and reactivation of tectonic elements in eastern part of Shillong Plateau, India: constraints from morpho-tectonic analyses
title_short Neotectonism and reactivation of tectonic elements in eastern part of Shillong Plateau, India: constraints from morpho-tectonic analyses
title_sort neotectonism and reactivation of tectonic elements in eastern part of shillong plateau india constraints from morpho tectonic analyses
topic Shillong plateau
neotectonics
morpho-structural analyses
basin asymmetry
url https://www.tandfonline.com/doi/10.1080/24749508.2024.2338973
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