Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc
Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting pl...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Manglik, A. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Anmerkung: |
© Geological Society of India, Bengaluru, India 2022 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of the Geological Society of India - New Delhi : Springer India, 1959, 98(2022), 1 vom: Jan., Seite 57-61 |
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| Übergeordnetes Werk: |
volume:98 ; year:2022 ; number:1 ; month:01 ; pages:57-61 |
| Links: |
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| DOI / URN: |
10.1007/s12594-022-1928-y |
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| Katalog-ID: |
SPR050416227 |
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| 520 | |a Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting plate. For the Himalayan collision belt, segmentation of the Indian lithosphere along the arc has been suggested based on seismological and GPS studies, and by analysis of topography and Bouguer gravity anomaly data. These studies, confined to the Himalaya-Tibet region, linked major segmentation boundaries to three transverse ridges in the Ganga basin. Since the formation of the Indo-Gangetic foreland basin is also controlled by the thermomechanical properties of the underthrusting Indian plate, in the present work, we study the Himalaya-foreland basin system for possible segmentation of the Indian lithosphere. We analyse the foreland basin width vis-à-vis the disposition of major thrust faults along several profiles cutting across the Himalayan arc to test a possible correlation between these two parameters. The results suggest a major segmentation boundary along the Indo-Nepal border in addition to other previously discussed segmentations coinciding with major transverse ridges in the Ganga basin. This segmentation boundary coincides with the Great Boundary fault separating the Aravalli Delhi fold belt (ADFB) from the Vindhyan basin further south. We infer a possible role of this boundary in limiting westward propagation of the rupture front of the 1505 paleo-seismic event and seismicity of the ADFB through coupling between the Himalayan collision belt and the intraplate Indian shield region. | ||
| 700 | 1 | |a Kandregula, R. S. |4 aut | |
| 700 | 1 | |a Pavankumar, G. |4 aut | |
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10.1007/s12594-022-1928-y doi (DE-627)SPR050416227 (SPR)s12594-022-1928-y-e DE-627 ger DE-627 rakwb eng Manglik, A. verfasserin aut Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India, Bengaluru, India 2022 Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting plate. For the Himalayan collision belt, segmentation of the Indian lithosphere along the arc has been suggested based on seismological and GPS studies, and by analysis of topography and Bouguer gravity anomaly data. These studies, confined to the Himalaya-Tibet region, linked major segmentation boundaries to three transverse ridges in the Ganga basin. Since the formation of the Indo-Gangetic foreland basin is also controlled by the thermomechanical properties of the underthrusting Indian plate, in the present work, we study the Himalaya-foreland basin system for possible segmentation of the Indian lithosphere. We analyse the foreland basin width vis-à-vis the disposition of major thrust faults along several profiles cutting across the Himalayan arc to test a possible correlation between these two parameters. The results suggest a major segmentation boundary along the Indo-Nepal border in addition to other previously discussed segmentations coinciding with major transverse ridges in the Ganga basin. This segmentation boundary coincides with the Great Boundary fault separating the Aravalli Delhi fold belt (ADFB) from the Vindhyan basin further south. We infer a possible role of this boundary in limiting westward propagation of the rupture front of the 1505 paleo-seismic event and seismicity of the ADFB through coupling between the Himalayan collision belt and the intraplate Indian shield region. Kandregula, R. S. aut Pavankumar, G. aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 98(2022), 1 vom: Jan., Seite 57-61 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:98 year:2022 number:1 month:01 pages:57-61 https://dx.doi.org/10.1007/s12594-022-1928-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 98 2022 1 01 57-61 |
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10.1007/s12594-022-1928-y doi (DE-627)SPR050416227 (SPR)s12594-022-1928-y-e DE-627 ger DE-627 rakwb eng Manglik, A. verfasserin aut Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India, Bengaluru, India 2022 Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting plate. For the Himalayan collision belt, segmentation of the Indian lithosphere along the arc has been suggested based on seismological and GPS studies, and by analysis of topography and Bouguer gravity anomaly data. These studies, confined to the Himalaya-Tibet region, linked major segmentation boundaries to three transverse ridges in the Ganga basin. Since the formation of the Indo-Gangetic foreland basin is also controlled by the thermomechanical properties of the underthrusting Indian plate, in the present work, we study the Himalaya-foreland basin system for possible segmentation of the Indian lithosphere. We analyse the foreland basin width vis-à-vis the disposition of major thrust faults along several profiles cutting across the Himalayan arc to test a possible correlation between these two parameters. The results suggest a major segmentation boundary along the Indo-Nepal border in addition to other previously discussed segmentations coinciding with major transverse ridges in the Ganga basin. This segmentation boundary coincides with the Great Boundary fault separating the Aravalli Delhi fold belt (ADFB) from the Vindhyan basin further south. We infer a possible role of this boundary in limiting westward propagation of the rupture front of the 1505 paleo-seismic event and seismicity of the ADFB through coupling between the Himalayan collision belt and the intraplate Indian shield region. Kandregula, R. S. aut Pavankumar, G. aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 98(2022), 1 vom: Jan., Seite 57-61 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:98 year:2022 number:1 month:01 pages:57-61 https://dx.doi.org/10.1007/s12594-022-1928-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 98 2022 1 01 57-61 |
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10.1007/s12594-022-1928-y doi (DE-627)SPR050416227 (SPR)s12594-022-1928-y-e DE-627 ger DE-627 rakwb eng Manglik, A. verfasserin aut Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India, Bengaluru, India 2022 Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting plate. For the Himalayan collision belt, segmentation of the Indian lithosphere along the arc has been suggested based on seismological and GPS studies, and by analysis of topography and Bouguer gravity anomaly data. These studies, confined to the Himalaya-Tibet region, linked major segmentation boundaries to three transverse ridges in the Ganga basin. Since the formation of the Indo-Gangetic foreland basin is also controlled by the thermomechanical properties of the underthrusting Indian plate, in the present work, we study the Himalaya-foreland basin system for possible segmentation of the Indian lithosphere. We analyse the foreland basin width vis-à-vis the disposition of major thrust faults along several profiles cutting across the Himalayan arc to test a possible correlation between these two parameters. The results suggest a major segmentation boundary along the Indo-Nepal border in addition to other previously discussed segmentations coinciding with major transverse ridges in the Ganga basin. This segmentation boundary coincides with the Great Boundary fault separating the Aravalli Delhi fold belt (ADFB) from the Vindhyan basin further south. We infer a possible role of this boundary in limiting westward propagation of the rupture front of the 1505 paleo-seismic event and seismicity of the ADFB through coupling between the Himalayan collision belt and the intraplate Indian shield region. Kandregula, R. S. aut Pavankumar, G. aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 98(2022), 1 vom: Jan., Seite 57-61 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:98 year:2022 number:1 month:01 pages:57-61 https://dx.doi.org/10.1007/s12594-022-1928-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 98 2022 1 01 57-61 |
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10.1007/s12594-022-1928-y doi (DE-627)SPR050416227 (SPR)s12594-022-1928-y-e DE-627 ger DE-627 rakwb eng Manglik, A. verfasserin aut Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India, Bengaluru, India 2022 Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting plate. For the Himalayan collision belt, segmentation of the Indian lithosphere along the arc has been suggested based on seismological and GPS studies, and by analysis of topography and Bouguer gravity anomaly data. These studies, confined to the Himalaya-Tibet region, linked major segmentation boundaries to three transverse ridges in the Ganga basin. Since the formation of the Indo-Gangetic foreland basin is also controlled by the thermomechanical properties of the underthrusting Indian plate, in the present work, we study the Himalaya-foreland basin system for possible segmentation of the Indian lithosphere. We analyse the foreland basin width vis-à-vis the disposition of major thrust faults along several profiles cutting across the Himalayan arc to test a possible correlation between these two parameters. The results suggest a major segmentation boundary along the Indo-Nepal border in addition to other previously discussed segmentations coinciding with major transverse ridges in the Ganga basin. This segmentation boundary coincides with the Great Boundary fault separating the Aravalli Delhi fold belt (ADFB) from the Vindhyan basin further south. We infer a possible role of this boundary in limiting westward propagation of the rupture front of the 1505 paleo-seismic event and seismicity of the ADFB through coupling between the Himalayan collision belt and the intraplate Indian shield region. Kandregula, R. S. aut Pavankumar, G. aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 98(2022), 1 vom: Jan., Seite 57-61 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:98 year:2022 number:1 month:01 pages:57-61 https://dx.doi.org/10.1007/s12594-022-1928-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 98 2022 1 01 57-61 |
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10.1007/s12594-022-1928-y doi (DE-627)SPR050416227 (SPR)s12594-022-1928-y-e DE-627 ger DE-627 rakwb eng Manglik, A. verfasserin aut Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India, Bengaluru, India 2022 Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting plate. For the Himalayan collision belt, segmentation of the Indian lithosphere along the arc has been suggested based on seismological and GPS studies, and by analysis of topography and Bouguer gravity anomaly data. These studies, confined to the Himalaya-Tibet region, linked major segmentation boundaries to three transverse ridges in the Ganga basin. Since the formation of the Indo-Gangetic foreland basin is also controlled by the thermomechanical properties of the underthrusting Indian plate, in the present work, we study the Himalaya-foreland basin system for possible segmentation of the Indian lithosphere. We analyse the foreland basin width vis-à-vis the disposition of major thrust faults along several profiles cutting across the Himalayan arc to test a possible correlation between these two parameters. The results suggest a major segmentation boundary along the Indo-Nepal border in addition to other previously discussed segmentations coinciding with major transverse ridges in the Ganga basin. This segmentation boundary coincides with the Great Boundary fault separating the Aravalli Delhi fold belt (ADFB) from the Vindhyan basin further south. We infer a possible role of this boundary in limiting westward propagation of the rupture front of the 1505 paleo-seismic event and seismicity of the ADFB through coupling between the Himalayan collision belt and the intraplate Indian shield region. Kandregula, R. S. aut Pavankumar, G. aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 98(2022), 1 vom: Jan., Seite 57-61 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:98 year:2022 number:1 month:01 pages:57-61 https://dx.doi.org/10.1007/s12594-022-1928-y lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 98 2022 1 01 57-61 |
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Manglik, A. Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc |
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Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc |
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Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc |
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Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc |
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Manglik, A. Kandregula, R. S. Pavankumar, G. |
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foreland basin geometry and disposition of major thrust faults as proxies for identification of segmentation along the himalayan arc |
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Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc |
| abstract |
Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting plate. For the Himalayan collision belt, segmentation of the Indian lithosphere along the arc has been suggested based on seismological and GPS studies, and by analysis of topography and Bouguer gravity anomaly data. These studies, confined to the Himalaya-Tibet region, linked major segmentation boundaries to three transverse ridges in the Ganga basin. Since the formation of the Indo-Gangetic foreland basin is also controlled by the thermomechanical properties of the underthrusting Indian plate, in the present work, we study the Himalaya-foreland basin system for possible segmentation of the Indian lithosphere. We analyse the foreland basin width vis-à-vis the disposition of major thrust faults along several profiles cutting across the Himalayan arc to test a possible correlation between these two parameters. The results suggest a major segmentation boundary along the Indo-Nepal border in addition to other previously discussed segmentations coinciding with major transverse ridges in the Ganga basin. This segmentation boundary coincides with the Great Boundary fault separating the Aravalli Delhi fold belt (ADFB) from the Vindhyan basin further south. We infer a possible role of this boundary in limiting westward propagation of the rupture front of the 1505 paleo-seismic event and seismicity of the ADFB through coupling between the Himalayan collision belt and the intraplate Indian shield region. © Geological Society of India, Bengaluru, India 2022 |
| abstractGer |
Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting plate. For the Himalayan collision belt, segmentation of the Indian lithosphere along the arc has been suggested based on seismological and GPS studies, and by analysis of topography and Bouguer gravity anomaly data. These studies, confined to the Himalaya-Tibet region, linked major segmentation boundaries to three transverse ridges in the Ganga basin. Since the formation of the Indo-Gangetic foreland basin is also controlled by the thermomechanical properties of the underthrusting Indian plate, in the present work, we study the Himalaya-foreland basin system for possible segmentation of the Indian lithosphere. We analyse the foreland basin width vis-à-vis the disposition of major thrust faults along several profiles cutting across the Himalayan arc to test a possible correlation between these two parameters. The results suggest a major segmentation boundary along the Indo-Nepal border in addition to other previously discussed segmentations coinciding with major transverse ridges in the Ganga basin. This segmentation boundary coincides with the Great Boundary fault separating the Aravalli Delhi fold belt (ADFB) from the Vindhyan basin further south. We infer a possible role of this boundary in limiting westward propagation of the rupture front of the 1505 paleo-seismic event and seismicity of the ADFB through coupling between the Himalayan collision belt and the intraplate Indian shield region. © Geological Society of India, Bengaluru, India 2022 |
| abstract_unstemmed |
Abstract Along-arc variation in the geometry of the décollement surface at a convergent margin is one of the significant parameters to assess the likely magnitude of a major/great earthquake. It is linked to the crustal/lithospheric structure and pre-existing tectonic fabric of the underthrusting plate. For the Himalayan collision belt, segmentation of the Indian lithosphere along the arc has been suggested based on seismological and GPS studies, and by analysis of topography and Bouguer gravity anomaly data. These studies, confined to the Himalaya-Tibet region, linked major segmentation boundaries to three transverse ridges in the Ganga basin. Since the formation of the Indo-Gangetic foreland basin is also controlled by the thermomechanical properties of the underthrusting Indian plate, in the present work, we study the Himalaya-foreland basin system for possible segmentation of the Indian lithosphere. We analyse the foreland basin width vis-à-vis the disposition of major thrust faults along several profiles cutting across the Himalayan arc to test a possible correlation between these two parameters. The results suggest a major segmentation boundary along the Indo-Nepal border in addition to other previously discussed segmentations coinciding with major transverse ridges in the Ganga basin. This segmentation boundary coincides with the Great Boundary fault separating the Aravalli Delhi fold belt (ADFB) from the Vindhyan basin further south. We infer a possible role of this boundary in limiting westward propagation of the rupture front of the 1505 paleo-seismic event and seismicity of the ADFB through coupling between the Himalayan collision belt and the intraplate Indian shield region. © Geological Society of India, Bengaluru, India 2022 |
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Foreland Basin Geometry and Disposition of Major Thrust Faults as Proxies for Identification of Segmentation along the Himalayan Arc |
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