Crustal Heterogeneity and Seismotectonics of the National Capital Region, Delhi, India
Abstract To better understand the relationship between crustal heterogeneity and seismotectonics in the National Capital Region (NCR), Delhi, India, we carried out local P- and S-velocity tomography beneath the NCR. First arrival times of the first P- and S-wave from 275 crustal earthquakes recorded...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Gupta, Sandeep [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2012 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Basel AG 2012 |
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| Übergeordnetes Werk: |
Enthalten in: Pure and applied geophysics - SP Birkhäuser Verlag Basel, 1964, 170(2012), 4 vom: 20. Sept., Seite 607-616 |
|---|---|
| Übergeordnetes Werk: |
volume:170 ; year:2012 ; number:4 ; day:20 ; month:09 ; pages:607-616 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00024-012-0572-7 |
|---|
| Katalog-ID: |
OLC2069496732 |
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| 520 | |a Abstract To better understand the relationship between crustal heterogeneity and seismotectonics in the National Capital Region (NCR), Delhi, India, we carried out local P- and S-velocity tomography beneath the NCR. First arrival times of the first P- and S-wave from 275 crustal earthquakes recorded by the Seismic Telemetry Network in and around Delhi of the India Meteorological Department, India, are inverted to obtain crustal P-, S-velocity and VP/VS variations in the region. Our tomographic images of the upper crust reflect well the surface geological and tectonic features. The Delhi fold belt is identified as low VP, high VS and low VP/VS. The Sohna hot spring region is appearing as low VP, low VS and high VP/VS correlating with the possible presence of fluid-filled rocks. The crustal seismicity is distributed in both the high- and low-velocity zones, but most distinctly in the low VP/VS region. | ||
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10.1007/s00024-012-0572-7 doi (DE-627)OLC2069496732 (DE-He213)s00024-012-0572-7-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Gupta, Sandeep verfasserin aut Crustal Heterogeneity and Seismotectonics of the National Capital Region, Delhi, India 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Basel AG 2012 Abstract To better understand the relationship between crustal heterogeneity and seismotectonics in the National Capital Region (NCR), Delhi, India, we carried out local P- and S-velocity tomography beneath the NCR. First arrival times of the first P- and S-wave from 275 crustal earthquakes recorded by the Seismic Telemetry Network in and around Delhi of the India Meteorological Department, India, are inverted to obtain crustal P-, S-velocity and VP/VS variations in the region. Our tomographic images of the upper crust reflect well the surface geological and tectonic features. The Delhi fold belt is identified as low VP, high VS and low VP/VS. The Sohna hot spring region is appearing as low VP, low VS and high VP/VS correlating with the possible presence of fluid-filled rocks. The crustal seismicity is distributed in both the high- and low-velocity zones, but most distinctly in the low VP/VS region. Seismic tomography National Capital Region (NCR) Delhi seismic velocity seismicity Mohanty, William K. aut Prakash, Rajesh aut Shukla, Atindra Kumar aut Enthalten in Pure and applied geophysics SP Birkhäuser Verlag Basel, 1964 170(2012), 4 vom: 20. Sept., Seite 607-616 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:170 year:2012 number:4 day:20 month:09 pages:607-616 https://doi.org/10.1007/s00024-012-0572-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 GBV_ILN_4277 AR 170 2012 4 20 09 607-616 |
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10.1007/s00024-012-0572-7 doi (DE-627)OLC2069496732 (DE-He213)s00024-012-0572-7-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Gupta, Sandeep verfasserin aut Crustal Heterogeneity and Seismotectonics of the National Capital Region, Delhi, India 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Basel AG 2012 Abstract To better understand the relationship between crustal heterogeneity and seismotectonics in the National Capital Region (NCR), Delhi, India, we carried out local P- and S-velocity tomography beneath the NCR. First arrival times of the first P- and S-wave from 275 crustal earthquakes recorded by the Seismic Telemetry Network in and around Delhi of the India Meteorological Department, India, are inverted to obtain crustal P-, S-velocity and VP/VS variations in the region. Our tomographic images of the upper crust reflect well the surface geological and tectonic features. The Delhi fold belt is identified as low VP, high VS and low VP/VS. The Sohna hot spring region is appearing as low VP, low VS and high VP/VS correlating with the possible presence of fluid-filled rocks. The crustal seismicity is distributed in both the high- and low-velocity zones, but most distinctly in the low VP/VS region. Seismic tomography National Capital Region (NCR) Delhi seismic velocity seismicity Mohanty, William K. aut Prakash, Rajesh aut Shukla, Atindra Kumar aut Enthalten in Pure and applied geophysics SP Birkhäuser Verlag Basel, 1964 170(2012), 4 vom: 20. Sept., Seite 607-616 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:170 year:2012 number:4 day:20 month:09 pages:607-616 https://doi.org/10.1007/s00024-012-0572-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 GBV_ILN_4277 AR 170 2012 4 20 09 607-616 |
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10.1007/s00024-012-0572-7 doi (DE-627)OLC2069496732 (DE-He213)s00024-012-0572-7-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Gupta, Sandeep verfasserin aut Crustal Heterogeneity and Seismotectonics of the National Capital Region, Delhi, India 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Basel AG 2012 Abstract To better understand the relationship between crustal heterogeneity and seismotectonics in the National Capital Region (NCR), Delhi, India, we carried out local P- and S-velocity tomography beneath the NCR. First arrival times of the first P- and S-wave from 275 crustal earthquakes recorded by the Seismic Telemetry Network in and around Delhi of the India Meteorological Department, India, are inverted to obtain crustal P-, S-velocity and VP/VS variations in the region. Our tomographic images of the upper crust reflect well the surface geological and tectonic features. The Delhi fold belt is identified as low VP, high VS and low VP/VS. The Sohna hot spring region is appearing as low VP, low VS and high VP/VS correlating with the possible presence of fluid-filled rocks. The crustal seismicity is distributed in both the high- and low-velocity zones, but most distinctly in the low VP/VS region. Seismic tomography National Capital Region (NCR) Delhi seismic velocity seismicity Mohanty, William K. aut Prakash, Rajesh aut Shukla, Atindra Kumar aut Enthalten in Pure and applied geophysics SP Birkhäuser Verlag Basel, 1964 170(2012), 4 vom: 20. Sept., Seite 607-616 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:170 year:2012 number:4 day:20 month:09 pages:607-616 https://doi.org/10.1007/s00024-012-0572-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 GBV_ILN_4277 AR 170 2012 4 20 09 607-616 |
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10.1007/s00024-012-0572-7 doi (DE-627)OLC2069496732 (DE-He213)s00024-012-0572-7-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Gupta, Sandeep verfasserin aut Crustal Heterogeneity and Seismotectonics of the National Capital Region, Delhi, India 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Basel AG 2012 Abstract To better understand the relationship between crustal heterogeneity and seismotectonics in the National Capital Region (NCR), Delhi, India, we carried out local P- and S-velocity tomography beneath the NCR. First arrival times of the first P- and S-wave from 275 crustal earthquakes recorded by the Seismic Telemetry Network in and around Delhi of the India Meteorological Department, India, are inverted to obtain crustal P-, S-velocity and VP/VS variations in the region. Our tomographic images of the upper crust reflect well the surface geological and tectonic features. The Delhi fold belt is identified as low VP, high VS and low VP/VS. The Sohna hot spring region is appearing as low VP, low VS and high VP/VS correlating with the possible presence of fluid-filled rocks. The crustal seismicity is distributed in both the high- and low-velocity zones, but most distinctly in the low VP/VS region. Seismic tomography National Capital Region (NCR) Delhi seismic velocity seismicity Mohanty, William K. aut Prakash, Rajesh aut Shukla, Atindra Kumar aut Enthalten in Pure and applied geophysics SP Birkhäuser Verlag Basel, 1964 170(2012), 4 vom: 20. Sept., Seite 607-616 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:170 year:2012 number:4 day:20 month:09 pages:607-616 https://doi.org/10.1007/s00024-012-0572-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_4028 GBV_ILN_4277 AR 170 2012 4 20 09 607-616 |
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Crustal Heterogeneity and Seismotectonics of the National Capital Region, Delhi, India |
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Gupta, Sandeep |
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Pure and applied geophysics |
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2012 |
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Gupta, Sandeep Mohanty, William K. Prakash, Rajesh Shukla, Atindra Kumar |
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170 |
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Gupta, Sandeep |
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10.1007/s00024-012-0572-7 |
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550 |
| title_sort |
crustal heterogeneity and seismotectonics of the national capital region, delhi, india |
| title_auth |
Crustal Heterogeneity and Seismotectonics of the National Capital Region, Delhi, India |
| abstract |
Abstract To better understand the relationship between crustal heterogeneity and seismotectonics in the National Capital Region (NCR), Delhi, India, we carried out local P- and S-velocity tomography beneath the NCR. First arrival times of the first P- and S-wave from 275 crustal earthquakes recorded by the Seismic Telemetry Network in and around Delhi of the India Meteorological Department, India, are inverted to obtain crustal P-, S-velocity and VP/VS variations in the region. Our tomographic images of the upper crust reflect well the surface geological and tectonic features. The Delhi fold belt is identified as low VP, high VS and low VP/VS. The Sohna hot spring region is appearing as low VP, low VS and high VP/VS correlating with the possible presence of fluid-filled rocks. The crustal seismicity is distributed in both the high- and low-velocity zones, but most distinctly in the low VP/VS region. © Springer Basel AG 2012 |
| abstractGer |
Abstract To better understand the relationship between crustal heterogeneity and seismotectonics in the National Capital Region (NCR), Delhi, India, we carried out local P- and S-velocity tomography beneath the NCR. First arrival times of the first P- and S-wave from 275 crustal earthquakes recorded by the Seismic Telemetry Network in and around Delhi of the India Meteorological Department, India, are inverted to obtain crustal P-, S-velocity and VP/VS variations in the region. Our tomographic images of the upper crust reflect well the surface geological and tectonic features. The Delhi fold belt is identified as low VP, high VS and low VP/VS. The Sohna hot spring region is appearing as low VP, low VS and high VP/VS correlating with the possible presence of fluid-filled rocks. The crustal seismicity is distributed in both the high- and low-velocity zones, but most distinctly in the low VP/VS region. © Springer Basel AG 2012 |
| abstract_unstemmed |
Abstract To better understand the relationship between crustal heterogeneity and seismotectonics in the National Capital Region (NCR), Delhi, India, we carried out local P- and S-velocity tomography beneath the NCR. First arrival times of the first P- and S-wave from 275 crustal earthquakes recorded by the Seismic Telemetry Network in and around Delhi of the India Meteorological Department, India, are inverted to obtain crustal P-, S-velocity and VP/VS variations in the region. Our tomographic images of the upper crust reflect well the surface geological and tectonic features. The Delhi fold belt is identified as low VP, high VS and low VP/VS. The Sohna hot spring region is appearing as low VP, low VS and high VP/VS correlating with the possible presence of fluid-filled rocks. The crustal seismicity is distributed in both the high- and low-velocity zones, but most distinctly in the low VP/VS region. © Springer Basel AG 2012 |
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| title_short |
Crustal Heterogeneity and Seismotectonics of the National Capital Region, Delhi, India |
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https://doi.org/10.1007/s00024-012-0572-7 |
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Mohanty, William K. Prakash, Rajesh Shukla, Atindra Kumar |
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