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
Autor*in: |
Boerner, David E. [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
1992 |
---|
Schlagwörter: |
---|
Anmerkung: |
© Kluwer Academic Publishers 1992 |
---|
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: |
---|
DOI / URN: |
10.1007/BF01903486 |
---|
Katalog-ID: |
OLC2034984145 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2034984145 | ||
003 | DE-627 | ||
005 | 20230503063633.0 | ||
007 | tu | ||
008 | 200819s1992 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/BF01903486 |2 doi | |
035 | |a (DE-627)OLC2034984145 | ||
035 | |a (DE-He213)BF01903486-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |q VZ |
084 | |a 16,13 |2 ssgn | ||
100 | 1 | |a Boerner, David E. |e verfasserin |4 aut | |
245 | 1 | 0 | |a Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results |
264 | 1 | |c 1992 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © Kluwer Academic Publishers 1992 | ||
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. | ||
650 | 4 | |a Continental Crust | |
650 | 4 | |a Layered Earth | |
650 | 4 | |a Crustal Depth | |
650 | 4 | |a Large Moment | |
650 | 4 | |a Sophisticated Processing | |
773 | 0 | 8 | |i Enthalten in |t Surveys in geophysics |d Kluwer Academic Publishers, 1986 |g 13(1992), 4-5 vom: Sept., Seite 435-488 |w (DE-627)129582107 |w (DE-600)232801-X |w (DE-576)053589092 |x 0169-3298 |7 nnns |
773 | 1 | 8 | |g volume:13 |g year:1992 |g number:4-5 |g month:09 |g pages:435-488 |
856 | 4 | 1 | |u https://doi.org/10.1007/BF01903486 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-PHY | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OPC-GGO | ||
912 | |a SSG-OPC-GEO | ||
912 | |a SSG-OPC-AST | ||
912 | |a GBV_ILN_11 | ||
912 | |a GBV_ILN_22 | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_47 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_601 | ||
912 | |a GBV_ILN_4012 | ||
912 | |a GBV_ILN_4035 | ||
951 | |a AR | ||
952 | |d 13 |j 1992 |e 4-5 |c 09 |h 435-488 |
author_variant |
d e b de deb |
---|---|
matchkey_str |
article:01693298:1992----::otoldorelcrmgeidesudnterrslsncreai |
hierarchy_sort_str |
1992 |
publishDate |
1992 |
allfields |
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 |
spelling |
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 |
allfields_unstemmed |
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 |
allfieldsGer |
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 |
allfieldsSound |
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 |
language |
English |
source |
Enthalten in Surveys in geophysics 13(1992), 4-5 vom: Sept., Seite 435-488 volume:13 year:1992 number:4-5 month:09 pages:435-488 |
sourceStr |
Enthalten in Surveys in geophysics 13(1992), 4-5 vom: Sept., Seite 435-488 volume:13 year:1992 number:4-5 month:09 pages:435-488 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Continental Crust Layered Earth Crustal Depth Large Moment Sophisticated Processing |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Surveys in geophysics |
authorswithroles_txt_mv |
Boerner, David E. @@aut@@ |
publishDateDaySort_date |
1992-09-01T00:00:00Z |
hierarchy_top_id |
129582107 |
dewey-sort |
3550 |
id |
OLC2034984145 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2034984145</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503063633.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1992 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF01903486</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2034984145</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF01903486-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">16,13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Boerner, David E.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1992</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Kluwer Academic Publishers 1992</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Continental Crust</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Layered Earth</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Crustal Depth</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Large Moment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sophisticated Processing</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Surveys in geophysics</subfield><subfield code="d">Kluwer Academic Publishers, 1986</subfield><subfield code="g">13(1992), 4-5 vom: Sept., Seite 435-488</subfield><subfield code="w">(DE-627)129582107</subfield><subfield code="w">(DE-600)232801-X</subfield><subfield code="w">(DE-576)053589092</subfield><subfield code="x">0169-3298</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:13</subfield><subfield code="g">year:1992</subfield><subfield code="g">number:4-5</subfield><subfield code="g">month:09</subfield><subfield code="g">pages:435-488</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF01903486</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-AST</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_47</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">13</subfield><subfield code="j">1992</subfield><subfield code="e">4-5</subfield><subfield code="c">09</subfield><subfield code="h">435-488</subfield></datafield></record></collection>
|
author |
Boerner, David E. |
spellingShingle |
Boerner, David E. ddc 550 ssgn 16,13 misc Continental Crust misc Layered Earth misc Crustal Depth misc Large Moment misc Sophisticated Processing Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results |
authorStr |
Boerner, David E. |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)129582107 |
format |
Article |
dewey-ones |
550 - Earth sciences |
delete_txt_mv |
keep |
author_role |
aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0169-3298 |
topic_title |
550 VZ 16,13 ssgn Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results Continental Crust Layered Earth Crustal Depth Large Moment Sophisticated Processing |
topic |
ddc 550 ssgn 16,13 misc Continental Crust misc Layered Earth misc Crustal Depth misc Large Moment misc Sophisticated Processing |
topic_unstemmed |
ddc 550 ssgn 16,13 misc Continental Crust misc Layered Earth misc Crustal Depth misc Large Moment misc Sophisticated Processing |
topic_browse |
ddc 550 ssgn 16,13 misc Continental Crust misc Layered Earth misc Crustal Depth misc Large Moment misc Sophisticated Processing |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Surveys in geophysics |
hierarchy_parent_id |
129582107 |
dewey-tens |
550 - Earth sciences & geology |
hierarchy_top_title |
Surveys in geophysics |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)129582107 (DE-600)232801-X (DE-576)053589092 |
title |
Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results |
ctrlnum |
(DE-627)OLC2034984145 (DE-He213)BF01903486-p |
title_full |
Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results |
author_sort |
Boerner, David E. |
journal |
Surveys in geophysics |
journalStr |
Surveys in geophysics |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science |
recordtype |
marc |
publishDateSort |
1992 |
contenttype_str_mv |
txt |
container_start_page |
435 |
author_browse |
Boerner, David E. |
container_volume |
13 |
class |
550 VZ 16,13 ssgn |
format_se |
Aufsätze |
author-letter |
Boerner, David E. |
doi_str_mv |
10.1007/BF01903486 |
dewey-full |
550 |
title_sort |
controlled source electromagnetic deep sounding: theory, results and correlation with natural source results |
title_auth |
Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results |
abstract |
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 |
abstractGer |
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 |
collection_details |
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 |
container_issue |
4-5 |
title_short |
Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results |
url |
https://doi.org/10.1007/BF01903486 |
remote_bool |
false |
ppnlink |
129582107 |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/BF01903486 |
up_date |
2024-07-03T23:18:34.672Z |
_version_ |
1803601801038004224 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2034984145</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503063633.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1992 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF01903486</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2034984145</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF01903486-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">16,13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Boerner, David E.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Controlled source electromagnetic deep sounding: Theory, results and correlation with natural source results</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1992</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Kluwer Academic Publishers 1992</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Continental Crust</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Layered Earth</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Crustal Depth</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Large Moment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sophisticated Processing</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Surveys in geophysics</subfield><subfield code="d">Kluwer Academic Publishers, 1986</subfield><subfield code="g">13(1992), 4-5 vom: Sept., Seite 435-488</subfield><subfield code="w">(DE-627)129582107</subfield><subfield code="w">(DE-600)232801-X</subfield><subfield code="w">(DE-576)053589092</subfield><subfield code="x">0169-3298</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:13</subfield><subfield code="g">year:1992</subfield><subfield code="g">number:4-5</subfield><subfield code="g">month:09</subfield><subfield code="g">pages:435-488</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF01903486</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-AST</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_47</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">13</subfield><subfield code="j">1992</subfield><subfield code="e">4-5</subfield><subfield code="c">09</subfield><subfield code="h">435-488</subfield></datafield></record></collection>
|
score |
7.4007587 |