Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment
Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variati...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Moroz, Yu. F. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2013 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© Pleiades Publishing, Ltd. 2013 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Izvestiya / Physics of the solid earth - SP MAIK Nauka/Interperiodica, 1994, 49(2013), 2 vom: März, Seite 191-204 |
|---|---|
| Übergeordnetes Werk: |
volume:49 ; year:2013 ; number:2 ; month:03 ; pages:191-204 |
| Links: |
|---|
| DOI / URN: |
10.1134/S1069351313020055 |
|---|
| Katalog-ID: |
OLC2062062907 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2062062907 | ||
| 003 | DE-627 | ||
| 005 | 20230302133040.0 | ||
| 007 | tu | ||
| 008 | 200819s2013 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1134/S1069351313020055 |2 doi | |
| 035 | |a (DE-627)OLC2062062907 | ||
| 035 | |a (DE-He213)S1069351313020055-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 000 |a 550 |q VZ |
| 084 | |a 16,13 |2 ssgn | ||
| 100 | 1 | |a Moroz, Yu. F. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment |
| 264 | 1 | |c 2013 | |
| 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 © Pleiades Publishing, Ltd. 2013 | ||
| 520 | |a Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun. | ||
| 650 | 4 | |a geoelectric field | |
| 650 | 4 | |a geomagnetic field | |
| 650 | 4 | |a annual variations | |
| 650 | 4 | |a impedance | |
| 650 | 4 | |a magnetic tipper | |
| 700 | 1 | |a Moroz, T. A. |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Izvestiya / Physics of the solid earth |d SP MAIK Nauka/Interperiodica, 1994 |g 49(2013), 2 vom: März, Seite 191-204 |w (DE-627)211547654 |w (DE-600)1323491-2 |w (DE-576)285632159 |x 1069-3513 |7 nnns |
| 773 | 1 | 8 | |g volume:49 |g year:2013 |g number:2 |g month:03 |g pages:191-204 |
| 856 | 4 | 1 | |u https://doi.org/10.1134/S1069351313020055 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OLC-OEU | ||
| 912 | |a SSG-OLC-IBL | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a SSG-OPC-GEO | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_70 | ||
| 951 | |a AR | ||
| 952 | |d 49 |j 2013 |e 2 |c 03 |h 191-204 | ||
| author_variant |
y f m yf yfm t a m ta tam |
|---|---|
| matchkey_str |
article:10693513:2013----::nulaitosnheetoantciloteatadlcrclodcii |
| hierarchy_sort_str |
2013 |
| publishDate |
2013 |
| allfields |
10.1134/S1069351313020055 doi (DE-627)OLC2062062907 (DE-He213)S1069351313020055-p DE-627 ger DE-627 rakwb eng 000 550 VZ 16,13 ssgn Moroz, Yu. F. verfasserin aut Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun. geoelectric field geomagnetic field annual variations impedance magnetic tipper Moroz, T. A. aut Enthalten in Izvestiya / Physics of the solid earth SP MAIK Nauka/Interperiodica, 1994 49(2013), 2 vom: März, Seite 191-204 (DE-627)211547654 (DE-600)1323491-2 (DE-576)285632159 1069-3513 nnns volume:49 year:2013 number:2 month:03 pages:191-204 https://doi.org/10.1134/S1069351313020055 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OLC-IBL SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_70 AR 49 2013 2 03 191-204 |
| spelling |
10.1134/S1069351313020055 doi (DE-627)OLC2062062907 (DE-He213)S1069351313020055-p DE-627 ger DE-627 rakwb eng 000 550 VZ 16,13 ssgn Moroz, Yu. F. verfasserin aut Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun. geoelectric field geomagnetic field annual variations impedance magnetic tipper Moroz, T. A. aut Enthalten in Izvestiya / Physics of the solid earth SP MAIK Nauka/Interperiodica, 1994 49(2013), 2 vom: März, Seite 191-204 (DE-627)211547654 (DE-600)1323491-2 (DE-576)285632159 1069-3513 nnns volume:49 year:2013 number:2 month:03 pages:191-204 https://doi.org/10.1134/S1069351313020055 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OLC-IBL SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_70 AR 49 2013 2 03 191-204 |
| allfields_unstemmed |
10.1134/S1069351313020055 doi (DE-627)OLC2062062907 (DE-He213)S1069351313020055-p DE-627 ger DE-627 rakwb eng 000 550 VZ 16,13 ssgn Moroz, Yu. F. verfasserin aut Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun. geoelectric field geomagnetic field annual variations impedance magnetic tipper Moroz, T. A. aut Enthalten in Izvestiya / Physics of the solid earth SP MAIK Nauka/Interperiodica, 1994 49(2013), 2 vom: März, Seite 191-204 (DE-627)211547654 (DE-600)1323491-2 (DE-576)285632159 1069-3513 nnns volume:49 year:2013 number:2 month:03 pages:191-204 https://doi.org/10.1134/S1069351313020055 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OLC-IBL SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_70 AR 49 2013 2 03 191-204 |
| allfieldsGer |
10.1134/S1069351313020055 doi (DE-627)OLC2062062907 (DE-He213)S1069351313020055-p DE-627 ger DE-627 rakwb eng 000 550 VZ 16,13 ssgn Moroz, Yu. F. verfasserin aut Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun. geoelectric field geomagnetic field annual variations impedance magnetic tipper Moroz, T. A. aut Enthalten in Izvestiya / Physics of the solid earth SP MAIK Nauka/Interperiodica, 1994 49(2013), 2 vom: März, Seite 191-204 (DE-627)211547654 (DE-600)1323491-2 (DE-576)285632159 1069-3513 nnns volume:49 year:2013 number:2 month:03 pages:191-204 https://doi.org/10.1134/S1069351313020055 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OLC-IBL SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_70 AR 49 2013 2 03 191-204 |
| allfieldsSound |
10.1134/S1069351313020055 doi (DE-627)OLC2062062907 (DE-He213)S1069351313020055-p DE-627 ger DE-627 rakwb eng 000 550 VZ 16,13 ssgn Moroz, Yu. F. verfasserin aut Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2013 Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun. geoelectric field geomagnetic field annual variations impedance magnetic tipper Moroz, T. A. aut Enthalten in Izvestiya / Physics of the solid earth SP MAIK Nauka/Interperiodica, 1994 49(2013), 2 vom: März, Seite 191-204 (DE-627)211547654 (DE-600)1323491-2 (DE-576)285632159 1069-3513 nnns volume:49 year:2013 number:2 month:03 pages:191-204 https://doi.org/10.1134/S1069351313020055 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OLC-IBL SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_70 AR 49 2013 2 03 191-204 |
| language |
English |
| source |
Enthalten in Izvestiya / Physics of the solid earth 49(2013), 2 vom: März, Seite 191-204 volume:49 year:2013 number:2 month:03 pages:191-204 |
| sourceStr |
Enthalten in Izvestiya / Physics of the solid earth 49(2013), 2 vom: März, Seite 191-204 volume:49 year:2013 number:2 month:03 pages:191-204 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
geoelectric field geomagnetic field annual variations impedance magnetic tipper |
| dewey-raw |
000 |
| isfreeaccess_bool |
false |
| container_title |
Izvestiya / Physics of the solid earth |
| authorswithroles_txt_mv |
Moroz, Yu. F. @@aut@@ Moroz, T. A. @@aut@@ |
| publishDateDaySort_date |
2013-03-01T00:00:00Z |
| hierarchy_top_id |
211547654 |
| dewey-sort |
0 |
| id |
OLC2062062907 |
| 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">OLC2062062907</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230302133040.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2013 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1134/S1069351313020055</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2062062907</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)S1069351313020055-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">000</subfield><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">Moroz, Yu. F.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2013</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">© Pleiades Publishing, Ltd. 2013</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">geoelectric field</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">geomagnetic field</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">annual variations</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">impedance</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">magnetic tipper</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Moroz, T. A.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Izvestiya / Physics of the solid earth</subfield><subfield code="d">SP MAIK Nauka/Interperiodica, 1994</subfield><subfield code="g">49(2013), 2 vom: März, Seite 191-204</subfield><subfield code="w">(DE-627)211547654</subfield><subfield code="w">(DE-600)1323491-2</subfield><subfield code="w">(DE-576)285632159</subfield><subfield code="x">1069-3513</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:49</subfield><subfield code="g">year:2013</subfield><subfield code="g">number:2</subfield><subfield code="g">month:03</subfield><subfield code="g">pages:191-204</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1134/S1069351313020055</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-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-OEU</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-IBL</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">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">49</subfield><subfield code="j">2013</subfield><subfield code="e">2</subfield><subfield code="c">03</subfield><subfield code="h">191-204</subfield></datafield></record></collection>
|
| author |
Moroz, Yu. F. |
| spellingShingle |
Moroz, Yu. F. ddc 000 ssgn 16,13 misc geoelectric field misc geomagnetic field misc annual variations misc impedance misc magnetic tipper Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment |
| authorStr |
Moroz, Yu. F. |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)211547654 |
| format |
Article |
| dewey-ones |
000 - Computer science, information & general works 550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
1069-3513 |
| topic_title |
000 550 VZ 16,13 ssgn Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment geoelectric field geomagnetic field annual variations impedance magnetic tipper |
| topic |
ddc 000 ssgn 16,13 misc geoelectric field misc geomagnetic field misc annual variations misc impedance misc magnetic tipper |
| topic_unstemmed |
ddc 000 ssgn 16,13 misc geoelectric field misc geomagnetic field misc annual variations misc impedance misc magnetic tipper |
| topic_browse |
ddc 000 ssgn 16,13 misc geoelectric field misc geomagnetic field misc annual variations misc impedance misc magnetic tipper |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Izvestiya / Physics of the solid earth |
| hierarchy_parent_id |
211547654 |
| dewey-tens |
000 - Computer science, knowledge & systems 550 - Earth sciences & geology |
| hierarchy_top_title |
Izvestiya / Physics of the solid earth |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)211547654 (DE-600)1323491-2 (DE-576)285632159 |
| title |
Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment |
| ctrlnum |
(DE-627)OLC2062062907 (DE-He213)S1069351313020055-p |
| title_full |
Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment |
| author_sort |
Moroz, Yu. F. |
| journal |
Izvestiya / Physics of the solid earth |
| journalStr |
Izvestiya / Physics of the solid earth |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
000 - Computer science, information & general works 500 - Science |
| recordtype |
marc |
| publishDateSort |
2013 |
| contenttype_str_mv |
txt |
| container_start_page |
191 |
| author_browse |
Moroz, Yu. F. Moroz, T. A. |
| container_volume |
49 |
| class |
000 550 VZ 16,13 ssgn |
| format_se |
Aufsätze |
| author-letter |
Moroz, Yu. F. |
| doi_str_mv |
10.1134/S1069351313020055 |
| dewey-full |
000 550 |
| title_sort |
annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment |
| title_auth |
Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment |
| abstract |
Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun. © Pleiades Publishing, Ltd. 2013 |
| abstractGer |
Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun. © Pleiades Publishing, Ltd. 2013 |
| abstract_unstemmed |
Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun. © Pleiades Publishing, Ltd. 2013 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-OEU SSG-OLC-IBL SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_40 GBV_ILN_70 |
| container_issue |
2 |
| title_short |
Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment |
| url |
https://doi.org/10.1134/S1069351313020055 |
| remote_bool |
false |
| author2 |
Moroz, T. A. |
| author2Str |
Moroz, T. A. |
| ppnlink |
211547654 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1134/S1069351313020055 |
| up_date |
2024-07-03T13:36:54.573Z |
| _version_ |
1803565205629698048 |
| 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">OLC2062062907</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230302133040.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2013 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1134/S1069351313020055</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2062062907</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)S1069351313020055-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">000</subfield><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">Moroz, Yu. F.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Annual variations in the electromagnetic field of the earth and electrical conductivity of the geological environment</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2013</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">© Pleiades Publishing, Ltd. 2013</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Synchronous annual variations in the geoelectric and geomagnetic field are studied on the basis of long-term electromagnetic monitoring. It is shown that the annual geoelectric variations have intraterrestrial origin and are not related to the annual geomagnetic variations. Temporal variations in the magnetotelluric impedance and magnetic tipper, which characterize the electrical conductivity of the geological environment, are analyzed. It is established that annual variations in the magnetotelluric impedance mainly describe the variations in the electrical conductivity of surface crustal layers and are less sensitive to the deep electrical conductivity of the Earth. The annual variations in the imaginary magnetic tipper at the periods of 1000–3000 s probably reflect the changes in conductivity of a deep transversal low-resistive zone (the fault). It is suggested that annual variations in the geoelectrical and geomagnetic fields, as well as in the electrical conductivity of the geological environment, arise as a response to the changes in the geodynamical processes caused by the revolution of the Earth around the Sun.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">geoelectric field</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">geomagnetic field</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">annual variations</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">impedance</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">magnetic tipper</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Moroz, T. A.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Izvestiya / Physics of the solid earth</subfield><subfield code="d">SP MAIK Nauka/Interperiodica, 1994</subfield><subfield code="g">49(2013), 2 vom: März, Seite 191-204</subfield><subfield code="w">(DE-627)211547654</subfield><subfield code="w">(DE-600)1323491-2</subfield><subfield code="w">(DE-576)285632159</subfield><subfield code="x">1069-3513</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:49</subfield><subfield code="g">year:2013</subfield><subfield code="g">number:2</subfield><subfield code="g">month:03</subfield><subfield code="g">pages:191-204</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1134/S1069351313020055</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-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-OEU</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-IBL</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">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">49</subfield><subfield code="j">2013</subfield><subfield code="e">2</subfield><subfield code="c">03</subfield><subfield code="h">191-204</subfield></datafield></record></collection>
|
| score |
7.402011 |