Magnetotelluric Phases: A Case Study from the Sukinda Thrust Area, Eastern India
Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetot...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Roy, K. K. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2000 |
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| Schlagwörter: |
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| Anmerkung: |
© Akadémiai Kiadó 2000 |
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| Übergeordnetes Werk: |
Enthalten in: Acta geodaetica et geophysica Hungarica - Budapest : Akad. Kiadó, 1997, 35(2000), 3 vom: Sept., Seite 265-275 |
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| Übergeordnetes Werk: |
volume:35 ; year:2000 ; number:3 ; month:09 ; pages:265-275 |
| Links: |
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| DOI / URN: |
10.1007/BF03325616 |
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| 520 | |a Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetotellurics are discussed. Behaviours of the phases of rotated TE and TM mode impedances $ ϕ_{TE} $ or $ ϕ_{XY} $, $ ϕ_{TM} $ or $ ϕ_{YX} $; phases of the rotation invariant magnetotelluric tensors $ ϕ_{B} $, $ ϕ_{D} $ and $ ϕ_{C} $; phases of the telluric vectors $ ϕ_{ex} $ and ϕey (discussed in the text) are presented using the field data collected across the Sukinda Collision Zone, District Dhenkanal, Orissa, India. All pseudosections show that phase is a more important tool than the apparent resistivity for qualitative interpretation. Phase pseudosections across the northern margin of the eastern ghats show the existence of a series of vertical faults just north of the collision zone and depth extent of these faults is around 12 to 15 km. Signature of the lithosphere — asthenosphere boundary is also reflected in the phase pseudosections. Electrical conductivity 2D MT models are obtained by joint inversion of apparent resistivity and phase. Phase is a must for magnetotelluric (MT) forward modelling and inversion. | ||
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10.1007/BF03325616 doi (DE-627)SPR037129864 (SPR)BF03325616-e DE-627 ger DE-627 rakwb eng Roy, K. K. verfasserin aut Magnetotelluric Phases: A Case Study from the Sukinda Thrust Area, Eastern India 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetotellurics are discussed. Behaviours of the phases of rotated TE and TM mode impedances $ ϕ_{TE} $ or $ ϕ_{XY} $, $ ϕ_{TM} $ or $ ϕ_{YX} $; phases of the rotation invariant magnetotelluric tensors $ ϕ_{B} $, $ ϕ_{D} $ and $ ϕ_{C} $; phases of the telluric vectors $ ϕ_{ex} $ and ϕey (discussed in the text) are presented using the field data collected across the Sukinda Collision Zone, District Dhenkanal, Orissa, India. All pseudosections show that phase is a more important tool than the apparent resistivity for qualitative interpretation. Phase pseudosections across the northern margin of the eastern ghats show the existence of a series of vertical faults just north of the collision zone and depth extent of these faults is around 12 to 15 km. Signature of the lithosphere — asthenosphere boundary is also reflected in the phase pseudosections. Electrical conductivity 2D MT models are obtained by joint inversion of apparent resistivity and phase. Phase is a must for magnetotelluric (MT) forward modelling and inversion. apparent resistivity (dpeaa)DE-He213 magnetotelluric phases (dpeaa)DE-He213 magnetotellurics (dpeaa)DE-He213 modelling (dpeaa)DE-He213 Srivastava, S. aut Singh, A. K. aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 3 vom: Sept., Seite 265-275 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:3 month:09 pages:265-275 https://dx.doi.org/10.1007/BF03325616 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 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_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 3 09 265-275 |
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10.1007/BF03325616 doi (DE-627)SPR037129864 (SPR)BF03325616-e DE-627 ger DE-627 rakwb eng Roy, K. K. verfasserin aut Magnetotelluric Phases: A Case Study from the Sukinda Thrust Area, Eastern India 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetotellurics are discussed. Behaviours of the phases of rotated TE and TM mode impedances $ ϕ_{TE} $ or $ ϕ_{XY} $, $ ϕ_{TM} $ or $ ϕ_{YX} $; phases of the rotation invariant magnetotelluric tensors $ ϕ_{B} $, $ ϕ_{D} $ and $ ϕ_{C} $; phases of the telluric vectors $ ϕ_{ex} $ and ϕey (discussed in the text) are presented using the field data collected across the Sukinda Collision Zone, District Dhenkanal, Orissa, India. All pseudosections show that phase is a more important tool than the apparent resistivity for qualitative interpretation. Phase pseudosections across the northern margin of the eastern ghats show the existence of a series of vertical faults just north of the collision zone and depth extent of these faults is around 12 to 15 km. Signature of the lithosphere — asthenosphere boundary is also reflected in the phase pseudosections. Electrical conductivity 2D MT models are obtained by joint inversion of apparent resistivity and phase. Phase is a must for magnetotelluric (MT) forward modelling and inversion. apparent resistivity (dpeaa)DE-He213 magnetotelluric phases (dpeaa)DE-He213 magnetotellurics (dpeaa)DE-He213 modelling (dpeaa)DE-He213 Srivastava, S. aut Singh, A. K. aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 3 vom: Sept., Seite 265-275 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:3 month:09 pages:265-275 https://dx.doi.org/10.1007/BF03325616 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 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_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 3 09 265-275 |
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10.1007/BF03325616 doi (DE-627)SPR037129864 (SPR)BF03325616-e DE-627 ger DE-627 rakwb eng Roy, K. K. verfasserin aut Magnetotelluric Phases: A Case Study from the Sukinda Thrust Area, Eastern India 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetotellurics are discussed. Behaviours of the phases of rotated TE and TM mode impedances $ ϕ_{TE} $ or $ ϕ_{XY} $, $ ϕ_{TM} $ or $ ϕ_{YX} $; phases of the rotation invariant magnetotelluric tensors $ ϕ_{B} $, $ ϕ_{D} $ and $ ϕ_{C} $; phases of the telluric vectors $ ϕ_{ex} $ and ϕey (discussed in the text) are presented using the field data collected across the Sukinda Collision Zone, District Dhenkanal, Orissa, India. All pseudosections show that phase is a more important tool than the apparent resistivity for qualitative interpretation. Phase pseudosections across the northern margin of the eastern ghats show the existence of a series of vertical faults just north of the collision zone and depth extent of these faults is around 12 to 15 km. Signature of the lithosphere — asthenosphere boundary is also reflected in the phase pseudosections. Electrical conductivity 2D MT models are obtained by joint inversion of apparent resistivity and phase. Phase is a must for magnetotelluric (MT) forward modelling and inversion. apparent resistivity (dpeaa)DE-He213 magnetotelluric phases (dpeaa)DE-He213 magnetotellurics (dpeaa)DE-He213 modelling (dpeaa)DE-He213 Srivastava, S. aut Singh, A. K. aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 3 vom: Sept., Seite 265-275 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:3 month:09 pages:265-275 https://dx.doi.org/10.1007/BF03325616 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 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_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 3 09 265-275 |
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10.1007/BF03325616 doi (DE-627)SPR037129864 (SPR)BF03325616-e DE-627 ger DE-627 rakwb eng Roy, K. K. verfasserin aut Magnetotelluric Phases: A Case Study from the Sukinda Thrust Area, Eastern India 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetotellurics are discussed. Behaviours of the phases of rotated TE and TM mode impedances $ ϕ_{TE} $ or $ ϕ_{XY} $, $ ϕ_{TM} $ or $ ϕ_{YX} $; phases of the rotation invariant magnetotelluric tensors $ ϕ_{B} $, $ ϕ_{D} $ and $ ϕ_{C} $; phases of the telluric vectors $ ϕ_{ex} $ and ϕey (discussed in the text) are presented using the field data collected across the Sukinda Collision Zone, District Dhenkanal, Orissa, India. All pseudosections show that phase is a more important tool than the apparent resistivity for qualitative interpretation. Phase pseudosections across the northern margin of the eastern ghats show the existence of a series of vertical faults just north of the collision zone and depth extent of these faults is around 12 to 15 km. Signature of the lithosphere — asthenosphere boundary is also reflected in the phase pseudosections. Electrical conductivity 2D MT models are obtained by joint inversion of apparent resistivity and phase. Phase is a must for magnetotelluric (MT) forward modelling and inversion. apparent resistivity (dpeaa)DE-He213 magnetotelluric phases (dpeaa)DE-He213 magnetotellurics (dpeaa)DE-He213 modelling (dpeaa)DE-He213 Srivastava, S. aut Singh, A. K. aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 3 vom: Sept., Seite 265-275 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:3 month:09 pages:265-275 https://dx.doi.org/10.1007/BF03325616 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 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_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 3 09 265-275 |
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10.1007/BF03325616 doi (DE-627)SPR037129864 (SPR)BF03325616-e DE-627 ger DE-627 rakwb eng Roy, K. K. verfasserin aut Magnetotelluric Phases: A Case Study from the Sukinda Thrust Area, Eastern India 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetotellurics are discussed. Behaviours of the phases of rotated TE and TM mode impedances $ ϕ_{TE} $ or $ ϕ_{XY} $, $ ϕ_{TM} $ or $ ϕ_{YX} $; phases of the rotation invariant magnetotelluric tensors $ ϕ_{B} $, $ ϕ_{D} $ and $ ϕ_{C} $; phases of the telluric vectors $ ϕ_{ex} $ and ϕey (discussed in the text) are presented using the field data collected across the Sukinda Collision Zone, District Dhenkanal, Orissa, India. All pseudosections show that phase is a more important tool than the apparent resistivity for qualitative interpretation. Phase pseudosections across the northern margin of the eastern ghats show the existence of a series of vertical faults just north of the collision zone and depth extent of these faults is around 12 to 15 km. Signature of the lithosphere — asthenosphere boundary is also reflected in the phase pseudosections. Electrical conductivity 2D MT models are obtained by joint inversion of apparent resistivity and phase. Phase is a must for magnetotelluric (MT) forward modelling and inversion. apparent resistivity (dpeaa)DE-He213 magnetotelluric phases (dpeaa)DE-He213 magnetotellurics (dpeaa)DE-He213 modelling (dpeaa)DE-He213 Srivastava, S. aut Singh, A. K. aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 3 vom: Sept., Seite 265-275 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:3 month:09 pages:265-275 https://dx.doi.org/10.1007/BF03325616 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 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_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 3 09 265-275 |
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Roy, K. K. misc apparent resistivity misc magnetotelluric phases misc magnetotellurics misc modelling Magnetotelluric Phases: A Case Study from the Sukinda Thrust Area, Eastern India |
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Magnetotelluric Phases: A Case Study from the Sukinda Thrust Area, Eastern India apparent resistivity (dpeaa)DE-He213 magnetotelluric phases (dpeaa)DE-He213 magnetotellurics (dpeaa)DE-He213 modelling (dpeaa)DE-He213 |
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magnetotelluric phases: a case study from the sukinda thrust area, eastern india |
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Magnetotelluric Phases: A Case Study from the Sukinda Thrust Area, Eastern India |
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Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetotellurics are discussed. Behaviours of the phases of rotated TE and TM mode impedances $ ϕ_{TE} $ or $ ϕ_{XY} $, $ ϕ_{TM} $ or $ ϕ_{YX} $; phases of the rotation invariant magnetotelluric tensors $ ϕ_{B} $, $ ϕ_{D} $ and $ ϕ_{C} $; phases of the telluric vectors $ ϕ_{ex} $ and ϕey (discussed in the text) are presented using the field data collected across the Sukinda Collision Zone, District Dhenkanal, Orissa, India. All pseudosections show that phase is a more important tool than the apparent resistivity for qualitative interpretation. Phase pseudosections across the northern margin of the eastern ghats show the existence of a series of vertical faults just north of the collision zone and depth extent of these faults is around 12 to 15 km. Signature of the lithosphere — asthenosphere boundary is also reflected in the phase pseudosections. Electrical conductivity 2D MT models are obtained by joint inversion of apparent resistivity and phase. Phase is a must for magnetotelluric (MT) forward modelling and inversion. © Akadémiai Kiadó 2000 |
| abstractGer |
Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetotellurics are discussed. Behaviours of the phases of rotated TE and TM mode impedances $ ϕ_{TE} $ or $ ϕ_{XY} $, $ ϕ_{TM} $ or $ ϕ_{YX} $; phases of the rotation invariant magnetotelluric tensors $ ϕ_{B} $, $ ϕ_{D} $ and $ ϕ_{C} $; phases of the telluric vectors $ ϕ_{ex} $ and ϕey (discussed in the text) are presented using the field data collected across the Sukinda Collision Zone, District Dhenkanal, Orissa, India. All pseudosections show that phase is a more important tool than the apparent resistivity for qualitative interpretation. Phase pseudosections across the northern margin of the eastern ghats show the existence of a series of vertical faults just north of the collision zone and depth extent of these faults is around 12 to 15 km. Signature of the lithosphere — asthenosphere boundary is also reflected in the phase pseudosections. Electrical conductivity 2D MT models are obtained by joint inversion of apparent resistivity and phase. Phase is a must for magnetotelluric (MT) forward modelling and inversion. © Akadémiai Kiadó 2000 |
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Abstract Phases of the magnetotelluric impedance tensors are more important than the apparent resistivities. Because they suffer minimum static distortion and are useful for both qualitative and quantitative interpretation. In this paper, the nature and behaviours of the family of phases in magnetotellurics are discussed. Behaviours of the phases of rotated TE and TM mode impedances $ ϕ_{TE} $ or $ ϕ_{XY} $, $ ϕ_{TM} $ or $ ϕ_{YX} $; phases of the rotation invariant magnetotelluric tensors $ ϕ_{B} $, $ ϕ_{D} $ and $ ϕ_{C} $; phases of the telluric vectors $ ϕ_{ex} $ and ϕey (discussed in the text) are presented using the field data collected across the Sukinda Collision Zone, District Dhenkanal, Orissa, India. All pseudosections show that phase is a more important tool than the apparent resistivity for qualitative interpretation. Phase pseudosections across the northern margin of the eastern ghats show the existence of a series of vertical faults just north of the collision zone and depth extent of these faults is around 12 to 15 km. Signature of the lithosphere — asthenosphere boundary is also reflected in the phase pseudosections. Electrical conductivity 2D MT models are obtained by joint inversion of apparent resistivity and phase. Phase is a must for magnetotelluric (MT) forward modelling and inversion. © Akadémiai Kiadó 2000 |
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