Evidence of Strain Accumulation and Coupling Variation in the Himachal Region of NW Himalaya From Short Term Geodetic Measurements

Himachal region of Northwest Himalaya exhibits the widest structural re‐entrant in Kangra region and significant strain partitioning along the frontal and hinterland out‐of‐sequence faults. We report results of continuous GPS measurements from 10 new sites in the region and analyze them along with t...

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Veröffentlicht in:Tectonics (Washington, D.C.) D.C.), 2023-08, Vol.42 (8), p.n/a
Hauptverfasser: Kumar, Prabhat, Malik, Javed N., Gahalaut, Vineet K., Yadav, Rajeev K., Singh, Gurvinder
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container_issue 8
container_start_page
container_title Tectonics (Washington, D.C.)
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creator Kumar, Prabhat
Malik, Javed N.
Gahalaut, Vineet K.
Yadav, Rajeev K.
Singh, Gurvinder
description Himachal region of Northwest Himalaya exhibits the widest structural re‐entrant in Kangra region and significant strain partitioning along the frontal and hinterland out‐of‐sequence faults. We report results of continuous GPS measurements from 10 new sites in the region and analyze them along with the previously published results to constrain the ongoing arc‐normal and arc‐parallel convergence rates at 16.5 ± 1.1 and 4–5 mm/yr respectively. Thus, the ongoing convergence is oblique by 15°–20°. The Main Himalayan Thrust (MHT) is strongly coupled up to ∼100 km from the Main Frontal Thrust but displays significant variation in coupling in the transition zone across the Kangra re‐entrant and the adjoining western salient. Joint analysis of the coupling variation, the geologically inferred MHT geometry variations and the local topographic anomaly pattern strongly suggest the possibility of a potentially active, strain accumulating segment of MBT along the southern margin of Dhauladhar ranges in Western Himachal region, which is also proposed to be influencing the long‐term topographic growth in the region. Although a general agreement is observed between the long‐term shortening rates along the active faults and the estimated geodetic convergence in this region, the ensuing discussion highlights their complex relationship in terms of temporal and spatial variability in the fault activity and elastic‐inelastic deformation. We use the fault orientation and the estimated convergence rate to geometrically constrain a mean dextral slip‐rate of 4.4–5.7 mm/yr along a recently discovered Khetpurali‐Taksal fault, which is proposed to partition the majority of ongoing arc‐parallel deformation along it. Key Points We estimate the arc‐normal and arc‐parallel convergence rates to be 16.5 ± 1.1 and 4–5 mm/yr respectively in Himachal Himalaya Kangra reentrant is strongly coupled throughout its ∼100 km width; Partial decoupling between 60 and 90 km from Main Frontal Thrust across the western salient Suggested strain accumulation of ∼2.5–3.3 mm/yr on MBT segment; Predicted dextral motion of ∼4.6–5.7 mm/yr on ∼N‐S trending segment of Khetpurali‐Taksal Fault
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We report results of continuous GPS measurements from 10 new sites in the region and analyze them along with the previously published results to constrain the ongoing arc‐normal and arc‐parallel convergence rates at 16.5 ± 1.1 and 4–5 mm/yr respectively. Thus, the ongoing convergence is oblique by 15°–20°. The Main Himalayan Thrust (MHT) is strongly coupled up to ∼100 km from the Main Frontal Thrust but displays significant variation in coupling in the transition zone across the Kangra re‐entrant and the adjoining western salient. Joint analysis of the coupling variation, the geologically inferred MHT geometry variations and the local topographic anomaly pattern strongly suggest the possibility of a potentially active, strain accumulating segment of MBT along the southern margin of Dhauladhar ranges in Western Himachal region, which is also proposed to be influencing the long‐term topographic growth in the region. Although a general agreement is observed between the long‐term shortening rates along the active faults and the estimated geodetic convergence in this region, the ensuing discussion highlights their complex relationship in terms of temporal and spatial variability in the fault activity and elastic‐inelastic deformation. We use the fault orientation and the estimated convergence rate to geometrically constrain a mean dextral slip‐rate of 4.4–5.7 mm/yr along a recently discovered Khetpurali‐Taksal fault, which is proposed to partition the majority of ongoing arc‐parallel deformation along it. Key Points We estimate the arc‐normal and arc‐parallel convergence rates to be 16.5 ± 1.1 and 4–5 mm/yr respectively in Himachal Himalaya Kangra reentrant is strongly coupled throughout its ∼100 km width; Partial decoupling between 60 and 90 km from Main Frontal Thrust across the western salient Suggested strain accumulation of ∼2.5–3.3 mm/yr on MBT segment; Predicted dextral motion of ∼4.6–5.7 mm/yr on ∼N‐S trending segment of Khetpurali‐Taksal Fault</description><identifier>ISSN: 0278-7407</identifier><identifier>EISSN: 1944-9194</identifier><identifier>DOI: 10.1029/2022TC007690</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Accumulation ; Convergence ; convergence rate ; Deformation ; Fault lines ; Geodetic measurements ; geological shortening rate ; GNSS geodesy ; inter‐seismic coupling ; slip‐deficit ; Spatial variability ; Spatial variations ; Topography ; Transition zone</subject><ispartof>Tectonics (Washington, D.C.), 2023-08, Vol.42 (8), p.n/a</ispartof><rights>2023. 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We report results of continuous GPS measurements from 10 new sites in the region and analyze them along with the previously published results to constrain the ongoing arc‐normal and arc‐parallel convergence rates at 16.5 ± 1.1 and 4–5 mm/yr respectively. Thus, the ongoing convergence is oblique by 15°–20°. The Main Himalayan Thrust (MHT) is strongly coupled up to ∼100 km from the Main Frontal Thrust but displays significant variation in coupling in the transition zone across the Kangra re‐entrant and the adjoining western salient. Joint analysis of the coupling variation, the geologically inferred MHT geometry variations and the local topographic anomaly pattern strongly suggest the possibility of a potentially active, strain accumulating segment of MBT along the southern margin of Dhauladhar ranges in Western Himachal region, which is also proposed to be influencing the long‐term topographic growth in the region. Although a general agreement is observed between the long‐term shortening rates along the active faults and the estimated geodetic convergence in this region, the ensuing discussion highlights their complex relationship in terms of temporal and spatial variability in the fault activity and elastic‐inelastic deformation. We use the fault orientation and the estimated convergence rate to geometrically constrain a mean dextral slip‐rate of 4.4–5.7 mm/yr along a recently discovered Khetpurali‐Taksal fault, which is proposed to partition the majority of ongoing arc‐parallel deformation along it. Key Points We estimate the arc‐normal and arc‐parallel convergence rates to be 16.5 ± 1.1 and 4–5 mm/yr respectively in Himachal Himalaya Kangra reentrant is strongly coupled throughout its ∼100 km width; Partial decoupling between 60 and 90 km from Main Frontal Thrust across the western salient Suggested strain accumulation of ∼2.5–3.3 mm/yr on MBT segment; Predicted dextral motion of ∼4.6–5.7 mm/yr on ∼N‐S trending segment of Khetpurali‐Taksal Fault</description><subject>Accumulation</subject><subject>Convergence</subject><subject>convergence rate</subject><subject>Deformation</subject><subject>Fault lines</subject><subject>Geodetic measurements</subject><subject>geological shortening rate</subject><subject>GNSS geodesy</subject><subject>inter‐seismic coupling</subject><subject>slip‐deficit</subject><subject>Spatial variability</subject><subject>Spatial variations</subject><subject>Topography</subject><subject>Transition zone</subject><issn>0278-7407</issn><issn>1944-9194</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp9kEtPwzAQhC0EEqVw4wdY4krAr7yOVVRapAISDXCMbGfTukri4iSgXvnluJQDJy670ujT7M4gdEnJDSUsvWWEsTwjJI5ScoRGNBUiSP08RiPC4iSIBYlP0VnXbQihIoyiEfqafpgSWg3YVnjZO2laPNF6aIZa9sa2WLYlzuywrU27wq_SmYPssX4NeG4aqdeyxs-w2sve5PHtR63lTuI7Zxu8XFvX4xxcg2dgS-iNxg8gu8FBA23fnaOTStYdXPzuMXq5m-bZPFg8ze6zySKQLNk_H5WSVpwxFQpZUUFDlYRacAKcq4qIEEKpmOJaK0WI5CDjUkCqfPCKUZ3yMbo6-G6dfR-g64uNHVzrTxYsCRPBGY-Ep64PlHa26xxUxdb5OG5XUFLsWy7-tuxxfsA_TQ27f9kin2Y5oylN-DfBLH7B</recordid><startdate>202308</startdate><enddate>202308</enddate><creator>Kumar, Prabhat</creator><creator>Malik, Javed N.</creator><creator>Gahalaut, Vineet K.</creator><creator>Yadav, Rajeev K.</creator><creator>Singh, Gurvinder</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0001-9423-9204</orcidid><orcidid>https://orcid.org/0000-0002-7600-8514</orcidid><orcidid>https://orcid.org/0000-0002-0708-7706</orcidid><orcidid>https://orcid.org/0000-0003-2514-4644</orcidid><orcidid>https://orcid.org/0000-0002-6686-670X</orcidid></search><sort><creationdate>202308</creationdate><title>Evidence of Strain Accumulation and Coupling Variation in the Himachal Region of NW Himalaya From Short Term Geodetic Measurements</title><author>Kumar, Prabhat ; Malik, Javed N. ; Gahalaut, Vineet K. ; Yadav, Rajeev K. ; Singh, Gurvinder</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a2878-76da1f322b54af1415b85c430e33bf045e5ab2b3ccbb00a3ea7d4e9b278f21c93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Accumulation</topic><topic>Convergence</topic><topic>convergence rate</topic><topic>Deformation</topic><topic>Fault lines</topic><topic>Geodetic measurements</topic><topic>geological shortening rate</topic><topic>GNSS geodesy</topic><topic>inter‐seismic coupling</topic><topic>slip‐deficit</topic><topic>Spatial variability</topic><topic>Spatial variations</topic><topic>Topography</topic><topic>Transition zone</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kumar, Prabhat</creatorcontrib><creatorcontrib>Malik, Javed N.</creatorcontrib><creatorcontrib>Gahalaut, Vineet K.</creatorcontrib><creatorcontrib>Yadav, Rajeev K.</creatorcontrib><creatorcontrib>Singh, Gurvinder</creatorcontrib><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Tectonics (Washington, D.C.)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kumar, Prabhat</au><au>Malik, Javed N.</au><au>Gahalaut, Vineet K.</au><au>Yadav, Rajeev K.</au><au>Singh, Gurvinder</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Evidence of Strain Accumulation and Coupling Variation in the Himachal Region of NW Himalaya From Short Term Geodetic Measurements</atitle><jtitle>Tectonics (Washington, D.C.)</jtitle><date>2023-08</date><risdate>2023</risdate><volume>42</volume><issue>8</issue><epage>n/a</epage><issn>0278-7407</issn><eissn>1944-9194</eissn><abstract>Himachal region of Northwest Himalaya exhibits the widest structural re‐entrant in Kangra region and significant strain partitioning along the frontal and hinterland out‐of‐sequence faults. We report results of continuous GPS measurements from 10 new sites in the region and analyze them along with the previously published results to constrain the ongoing arc‐normal and arc‐parallel convergence rates at 16.5 ± 1.1 and 4–5 mm/yr respectively. Thus, the ongoing convergence is oblique by 15°–20°. The Main Himalayan Thrust (MHT) is strongly coupled up to ∼100 km from the Main Frontal Thrust but displays significant variation in coupling in the transition zone across the Kangra re‐entrant and the adjoining western salient. Joint analysis of the coupling variation, the geologically inferred MHT geometry variations and the local topographic anomaly pattern strongly suggest the possibility of a potentially active, strain accumulating segment of MBT along the southern margin of Dhauladhar ranges in Western Himachal region, which is also proposed to be influencing the long‐term topographic growth in the region. Although a general agreement is observed between the long‐term shortening rates along the active faults and the estimated geodetic convergence in this region, the ensuing discussion highlights their complex relationship in terms of temporal and spatial variability in the fault activity and elastic‐inelastic deformation. We use the fault orientation and the estimated convergence rate to geometrically constrain a mean dextral slip‐rate of 4.4–5.7 mm/yr along a recently discovered Khetpurali‐Taksal fault, which is proposed to partition the majority of ongoing arc‐parallel deformation along it. Key Points We estimate the arc‐normal and arc‐parallel convergence rates to be 16.5 ± 1.1 and 4–5 mm/yr respectively in Himachal Himalaya Kangra reentrant is strongly coupled throughout its ∼100 km width; Partial decoupling between 60 and 90 km from Main Frontal Thrust across the western salient Suggested strain accumulation of ∼2.5–3.3 mm/yr on MBT segment; Predicted dextral motion of ∼4.6–5.7 mm/yr on ∼N‐S trending segment of Khetpurali‐Taksal Fault</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2022TC007690</doi><tpages>22</tpages><orcidid>https://orcid.org/0000-0001-9423-9204</orcidid><orcidid>https://orcid.org/0000-0002-7600-8514</orcidid><orcidid>https://orcid.org/0000-0002-0708-7706</orcidid><orcidid>https://orcid.org/0000-0003-2514-4644</orcidid><orcidid>https://orcid.org/0000-0002-6686-670X</orcidid></addata></record>
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subjects Accumulation
Convergence
convergence rate
Deformation
Fault lines
Geodetic measurements
geological shortening rate
GNSS geodesy
inter‐seismic coupling
slip‐deficit
Spatial variability
Spatial variations
Topography
Transition zone
title Evidence of Strain Accumulation and Coupling Variation in the Himachal Region of NW Himalaya From Short Term Geodetic Measurements
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