Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results
Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Boerner, David E. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1992 |
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| Schlagwörter: |
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| Anmerkung: |
© Kluwer Academic Publishers 1992 |
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| Übergeordnetes Werk: |
Enthalten in: Surveys in geophysics - Kluwer Academic Publishers, 1986, 13(1992), 4-5 vom: Sept., Seite 435-488 |
|---|---|
| Übergeordnetes Werk: |
volume:13 ; year:1992 ; number:4-5 ; month:09 ; pages:435-488 |
| Links: |
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| DOI / URN: |
10.1007/BF01903486 |
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| 520 | |a Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution and minimize interactions with local structure. The major drawbacks include restricted depth penetration, insufficient data sets and a limited number of modelling algorithms. Information about the electrical conductivity at lower crustal depths can be obtained but at the expense of requiring large moment sources, sophisticated processing techniques and data redundancy. Moreover, EM data are sufficiently complicated that numerical modelling is often necessary for quantitative interpretation. It is therefore essential to record enough information to justify the choice of interpretation algorithms, particularly since controlled source EM forward modelling routines are generally very restrictive and not widely available. As most interpretations are based on layered earth models, observations of all the EM field components can be useful for testing the “dimensionality” of the data and for justifying interpretations. | ||
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10.1007/BF01903486 doi (DE-627)OLC2034984145 (DE-He213)BF01903486-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Boerner, David E. verfasserin aut Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1992 Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution and minimize interactions with local structure. The major drawbacks include restricted depth penetration, insufficient data sets and a limited number of modelling algorithms. Information about the electrical conductivity at lower crustal depths can be obtained but at the expense of requiring large moment sources, sophisticated processing techniques and data redundancy. Moreover, EM data are sufficiently complicated that numerical modelling is often necessary for quantitative interpretation. It is therefore essential to record enough information to justify the choice of interpretation algorithms, particularly since controlled source EM forward modelling routines are generally very restrictive and not widely available. As most interpretations are based on layered earth models, observations of all the EM field components can be useful for testing the “dimensionality” of the data and for justifying interpretations. Continental Crust Layered Earth Crustal Depth Large Moment Sophisticated Processing Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 13(1992), 4-5 vom: Sept., Seite 435-488 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:13 year:1992 number:4-5 month:09 pages:435-488 https://doi.org/10.1007/BF01903486 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4035 AR 13 1992 4-5 09 435-488 |
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10.1007/BF01903486 doi (DE-627)OLC2034984145 (DE-He213)BF01903486-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Boerner, David E. verfasserin aut Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1992 Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution and minimize interactions with local structure. The major drawbacks include restricted depth penetration, insufficient data sets and a limited number of modelling algorithms. Information about the electrical conductivity at lower crustal depths can be obtained but at the expense of requiring large moment sources, sophisticated processing techniques and data redundancy. Moreover, EM data are sufficiently complicated that numerical modelling is often necessary for quantitative interpretation. It is therefore essential to record enough information to justify the choice of interpretation algorithms, particularly since controlled source EM forward modelling routines are generally very restrictive and not widely available. As most interpretations are based on layered earth models, observations of all the EM field components can be useful for testing the “dimensionality” of the data and for justifying interpretations. Continental Crust Layered Earth Crustal Depth Large Moment Sophisticated Processing Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 13(1992), 4-5 vom: Sept., Seite 435-488 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:13 year:1992 number:4-5 month:09 pages:435-488 https://doi.org/10.1007/BF01903486 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4035 AR 13 1992 4-5 09 435-488 |
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10.1007/BF01903486 doi (DE-627)OLC2034984145 (DE-He213)BF01903486-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Boerner, David E. verfasserin aut Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1992 Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution and minimize interactions with local structure. The major drawbacks include restricted depth penetration, insufficient data sets and a limited number of modelling algorithms. Information about the electrical conductivity at lower crustal depths can be obtained but at the expense of requiring large moment sources, sophisticated processing techniques and data redundancy. Moreover, EM data are sufficiently complicated that numerical modelling is often necessary for quantitative interpretation. It is therefore essential to record enough information to justify the choice of interpretation algorithms, particularly since controlled source EM forward modelling routines are generally very restrictive and not widely available. As most interpretations are based on layered earth models, observations of all the EM field components can be useful for testing the “dimensionality” of the data and for justifying interpretations. Continental Crust Layered Earth Crustal Depth Large Moment Sophisticated Processing Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 13(1992), 4-5 vom: Sept., Seite 435-488 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:13 year:1992 number:4-5 month:09 pages:435-488 https://doi.org/10.1007/BF01903486 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4035 AR 13 1992 4-5 09 435-488 |
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10.1007/BF01903486 doi (DE-627)OLC2034984145 (DE-He213)BF01903486-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Boerner, David E. verfasserin aut Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1992 Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution and minimize interactions with local structure. The major drawbacks include restricted depth penetration, insufficient data sets and a limited number of modelling algorithms. Information about the electrical conductivity at lower crustal depths can be obtained but at the expense of requiring large moment sources, sophisticated processing techniques and data redundancy. Moreover, EM data are sufficiently complicated that numerical modelling is often necessary for quantitative interpretation. It is therefore essential to record enough information to justify the choice of interpretation algorithms, particularly since controlled source EM forward modelling routines are generally very restrictive and not widely available. As most interpretations are based on layered earth models, observations of all the EM field components can be useful for testing the “dimensionality” of the data and for justifying interpretations. Continental Crust Layered Earth Crustal Depth Large Moment Sophisticated Processing Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 13(1992), 4-5 vom: Sept., Seite 435-488 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:13 year:1992 number:4-5 month:09 pages:435-488 https://doi.org/10.1007/BF01903486 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4035 AR 13 1992 4-5 09 435-488 |
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10.1007/BF01903486 doi (DE-627)OLC2034984145 (DE-He213)BF01903486-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Boerner, David E. verfasserin aut Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results 1992 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1992 Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution and minimize interactions with local structure. The major drawbacks include restricted depth penetration, insufficient data sets and a limited number of modelling algorithms. Information about the electrical conductivity at lower crustal depths can be obtained but at the expense of requiring large moment sources, sophisticated processing techniques and data redundancy. Moreover, EM data are sufficiently complicated that numerical modelling is often necessary for quantitative interpretation. It is therefore essential to record enough information to justify the choice of interpretation algorithms, particularly since controlled source EM forward modelling routines are generally very restrictive and not widely available. As most interpretations are based on layered earth models, observations of all the EM field components can be useful for testing the “dimensionality” of the data and for justifying interpretations. Continental Crust Layered Earth Crustal Depth Large Moment Sophisticated Processing Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 13(1992), 4-5 vom: Sept., Seite 435-488 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:13 year:1992 number:4-5 month:09 pages:435-488 https://doi.org/10.1007/BF01903486 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4035 AR 13 1992 4-5 09 435-488 |
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Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution and minimize interactions with local structure. The major drawbacks include restricted depth penetration, insufficient data sets and a limited number of modelling algorithms. Information about the electrical conductivity at lower crustal depths can be obtained but at the expense of requiring large moment sources, sophisticated processing techniques and data redundancy. Moreover, EM data are sufficiently complicated that numerical modelling is often necessary for quantitative interpretation. It is therefore essential to record enough information to justify the choice of interpretation algorithms, particularly since controlled source EM forward modelling routines are generally very restrictive and not widely available. As most interpretations are based on layered earth models, observations of all the EM field components can be useful for testing the “dimensionality” of the data and for justifying interpretations. © Kluwer Academic Publishers 1992 |
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Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution and minimize interactions with local structure. The major drawbacks include restricted depth penetration, insufficient data sets and a limited number of modelling algorithms. Information about the electrical conductivity at lower crustal depths can be obtained but at the expense of requiring large moment sources, sophisticated processing techniques and data redundancy. Moreover, EM data are sufficiently complicated that numerical modelling is often necessary for quantitative interpretation. It is therefore essential to record enough information to justify the choice of interpretation algorithms, particularly since controlled source EM forward modelling routines are generally very restrictive and not widely available. As most interpretations are based on layered earth models, observations of all the EM field components can be useful for testing the “dimensionality” of the data and for justifying interpretations. © Kluwer Academic Publishers 1992 |
| abstract_unstemmed |
Abstract Controlled source electromagnetic (EM) methods represent a unique set of geophysical experiments which can be used to determine the properties and state of the deep continental crust. Unlike natural source EM methods, an artificial EM source technique can be designed to optimize resolution and minimize interactions with local structure. The major drawbacks include restricted depth penetration, insufficient data sets and a limited number of modelling algorithms. Information about the electrical conductivity at lower crustal depths can be obtained but at the expense of requiring large moment sources, sophisticated processing techniques and data redundancy. Moreover, EM data are sufficiently complicated that numerical modelling is often necessary for quantitative interpretation. It is therefore essential to record enough information to justify the choice of interpretation algorithms, particularly since controlled source EM forward modelling routines are generally very restrictive and not widely available. As most interpretations are based on layered earth models, observations of all the EM field components can be useful for testing the “dimensionality” of the data and for justifying interpretations. © Kluwer Academic Publishers 1992 |
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Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results |
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