On the propagation of love waves in an infinite cylindrical surface
Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
De, Sasadhar [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1974 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© Birkhäuser-Verlag 1974 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Pure and applied geophysics - Birkhäuser-Verlag, 1964, 112(1974), 1 vom: Jan., Seite 35-45 |
|---|---|
| Übergeordnetes Werk: |
volume:112 ; year:1974 ; number:1 ; month:01 ; pages:35-45 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00875915 |
|---|
| Katalog-ID: |
OLC2069456242 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2069456242 | ||
| 003 | DE-627 | ||
| 005 | 20230323111912.0 | ||
| 007 | tu | ||
| 008 | 200819s1974 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1007/BF00875915 |2 doi | |
| 035 | |a (DE-627)OLC2069456242 | ||
| 035 | |a (DE-He213)BF00875915-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |q VZ |
| 082 | 0 | 4 | |a 550 |q VZ |
| 084 | |a 16,13 |2 ssgn | ||
| 100 | 1 | |a De, Sasadhar |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a On the propagation of love waves in an infinite cylindrical surface |
| 264 | 1 | |c 1974 | |
| 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 © Birkhäuser-Verlag 1974 | ||
| 520 | |a Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered. | ||
| 650 | 4 | |a Isotropic Material | |
| 650 | 4 | |a Earth Model | |
| 650 | 4 | |a Dispersion Equation | |
| 650 | 4 | |a Central Core | |
| 650 | 4 | |a Anisotropic Material | |
| 773 | 0 | 8 | |i Enthalten in |t Pure and applied geophysics |d Birkhäuser-Verlag, 1964 |g 112(1974), 1 vom: Jan., Seite 35-45 |w (DE-627)129538353 |w (DE-600)216719-0 |w (DE-576)014971038 |x 0033-4553 |7 nnns |
| 773 | 1 | 8 | |g volume:112 |g year:1974 |g number:1 |g month:01 |g pages:35-45 |
| 856 | 4 | 1 | |u https://doi.org/10.1007/BF00875915 |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 GBV_ILN_11 | ||
| 912 | |a GBV_ILN_20 | ||
| 912 | |a GBV_ILN_21 | ||
| 912 | |a GBV_ILN_22 | ||
| 912 | |a GBV_ILN_30 | ||
| 912 | |a GBV_ILN_31 | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_47 | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_267 | ||
| 912 | |a GBV_ILN_601 | ||
| 912 | |a GBV_ILN_2010 | ||
| 912 | |a GBV_ILN_2015 | ||
| 912 | |a GBV_ILN_2027 | ||
| 912 | |a GBV_ILN_4012 | ||
| 912 | |a GBV_ILN_4028 | ||
| 912 | |a GBV_ILN_4029 | ||
| 912 | |a GBV_ILN_4035 | ||
| 912 | |a GBV_ILN_4046 | ||
| 912 | |a GBV_ILN_4305 | ||
| 912 | |a GBV_ILN_4307 | ||
| 951 | |a AR | ||
| 952 | |d 112 |j 1974 |e 1 |c 01 |h 35-45 | ||
| author_variant |
s d sd |
|---|---|
| matchkey_str |
article:00334553:1974----::nhpoaainfoeaeiaifntcl |
| hierarchy_sort_str |
1974 |
| publishDate |
1974 |
| allfields |
10.1007/BF00875915 doi (DE-627)OLC2069456242 (DE-He213)BF00875915-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn De, Sasadhar verfasserin aut On the propagation of love waves in an infinite cylindrical surface 1974 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1974 Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered. Isotropic Material Earth Model Dispersion Equation Central Core Anisotropic Material Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 112(1974), 1 vom: Jan., Seite 35-45 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:112 year:1974 number:1 month:01 pages:35-45 https://doi.org/10.1007/BF00875915 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 112 1974 1 01 35-45 |
| spelling |
10.1007/BF00875915 doi (DE-627)OLC2069456242 (DE-He213)BF00875915-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn De, Sasadhar verfasserin aut On the propagation of love waves in an infinite cylindrical surface 1974 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1974 Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered. Isotropic Material Earth Model Dispersion Equation Central Core Anisotropic Material Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 112(1974), 1 vom: Jan., Seite 35-45 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:112 year:1974 number:1 month:01 pages:35-45 https://doi.org/10.1007/BF00875915 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 112 1974 1 01 35-45 |
| allfields_unstemmed |
10.1007/BF00875915 doi (DE-627)OLC2069456242 (DE-He213)BF00875915-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn De, Sasadhar verfasserin aut On the propagation of love waves in an infinite cylindrical surface 1974 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1974 Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered. Isotropic Material Earth Model Dispersion Equation Central Core Anisotropic Material Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 112(1974), 1 vom: Jan., Seite 35-45 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:112 year:1974 number:1 month:01 pages:35-45 https://doi.org/10.1007/BF00875915 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 112 1974 1 01 35-45 |
| allfieldsGer |
10.1007/BF00875915 doi (DE-627)OLC2069456242 (DE-He213)BF00875915-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn De, Sasadhar verfasserin aut On the propagation of love waves in an infinite cylindrical surface 1974 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1974 Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered. Isotropic Material Earth Model Dispersion Equation Central Core Anisotropic Material Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 112(1974), 1 vom: Jan., Seite 35-45 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:112 year:1974 number:1 month:01 pages:35-45 https://doi.org/10.1007/BF00875915 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 112 1974 1 01 35-45 |
| allfieldsSound |
10.1007/BF00875915 doi (DE-627)OLC2069456242 (DE-He213)BF00875915-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn De, Sasadhar verfasserin aut On the propagation of love waves in an infinite cylindrical surface 1974 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Birkhäuser-Verlag 1974 Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered. Isotropic Material Earth Model Dispersion Equation Central Core Anisotropic Material Enthalten in Pure and applied geophysics Birkhäuser-Verlag, 1964 112(1974), 1 vom: Jan., Seite 35-45 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:112 year:1974 number:1 month:01 pages:35-45 https://doi.org/10.1007/BF00875915 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 AR 112 1974 1 01 35-45 |
| language |
English |
| source |
Enthalten in Pure and applied geophysics 112(1974), 1 vom: Jan., Seite 35-45 volume:112 year:1974 number:1 month:01 pages:35-45 |
| sourceStr |
Enthalten in Pure and applied geophysics 112(1974), 1 vom: Jan., Seite 35-45 volume:112 year:1974 number:1 month:01 pages:35-45 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Isotropic Material Earth Model Dispersion Equation Central Core Anisotropic Material |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Pure and applied geophysics |
| authorswithroles_txt_mv |
De, Sasadhar @@aut@@ |
| publishDateDaySort_date |
1974-01-01T00:00:00Z |
| hierarchy_top_id |
129538353 |
| dewey-sort |
3550 |
| id |
OLC2069456242 |
| 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">OLC2069456242</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230323111912.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1974 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF00875915</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2069456242</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF00875915-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="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">De, Sasadhar</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">On the propagation of love waves in an infinite cylindrical surface</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1974</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">© Birkhäuser-Verlag 1974</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Isotropic Material</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Dispersion Equation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Central Core</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Anisotropic Material</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Pure and applied geophysics</subfield><subfield code="d">Birkhäuser-Verlag, 1964</subfield><subfield code="g">112(1974), 1 vom: Jan., Seite 35-45</subfield><subfield code="w">(DE-627)129538353</subfield><subfield code="w">(DE-600)216719-0</subfield><subfield code="w">(DE-576)014971038</subfield><subfield code="x">0033-4553</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:112</subfield><subfield code="g">year:1974</subfield><subfield code="g">number:1</subfield><subfield code="g">month:01</subfield><subfield code="g">pages:35-45</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF00875915</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">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</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_30</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</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_267</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_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</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_4028</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4029</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">112</subfield><subfield code="j">1974</subfield><subfield code="e">1</subfield><subfield code="c">01</subfield><subfield code="h">35-45</subfield></datafield></record></collection>
|
| author |
De, Sasadhar |
| spellingShingle |
De, Sasadhar ddc 550 ssgn 16,13 misc Isotropic Material misc Earth Model misc Dispersion Equation misc Central Core misc Anisotropic Material On the propagation of love waves in an infinite cylindrical surface |
| authorStr |
De, Sasadhar |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)129538353 |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0033-4553 |
| topic_title |
550 VZ 16,13 ssgn On the propagation of love waves in an infinite cylindrical surface Isotropic Material Earth Model Dispersion Equation Central Core Anisotropic Material |
| topic |
ddc 550 ssgn 16,13 misc Isotropic Material misc Earth Model misc Dispersion Equation misc Central Core misc Anisotropic Material |
| topic_unstemmed |
ddc 550 ssgn 16,13 misc Isotropic Material misc Earth Model misc Dispersion Equation misc Central Core misc Anisotropic Material |
| topic_browse |
ddc 550 ssgn 16,13 misc Isotropic Material misc Earth Model misc Dispersion Equation misc Central Core misc Anisotropic Material |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Pure and applied geophysics |
| hierarchy_parent_id |
129538353 |
| dewey-tens |
550 - Earth sciences & geology |
| hierarchy_top_title |
Pure and applied geophysics |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 |
| title |
On the propagation of love waves in an infinite cylindrical surface |
| ctrlnum |
(DE-627)OLC2069456242 (DE-He213)BF00875915-p |
| title_full |
On the propagation of love waves in an infinite cylindrical surface |
| author_sort |
De, Sasadhar |
| journal |
Pure and applied geophysics |
| journalStr |
Pure and applied geophysics |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
1974 |
| contenttype_str_mv |
txt |
| container_start_page |
35 |
| author_browse |
De, Sasadhar |
| container_volume |
112 |
| class |
550 VZ 16,13 ssgn |
| format_se |
Aufsätze |
| author-letter |
De, Sasadhar |
| doi_str_mv |
10.1007/BF00875915 |
| dewey-full |
550 |
| title_sort |
on the propagation of love waves in an infinite cylindrical surface |
| title_auth |
On the propagation of love waves in an infinite cylindrical surface |
| abstract |
Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered. © Birkhäuser-Verlag 1974 |
| abstractGer |
Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered. © Birkhäuser-Verlag 1974 |
| abstract_unstemmed |
Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered. © Birkhäuser-Verlag 1974 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_20 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4305 GBV_ILN_4307 |
| container_issue |
1 |
| title_short |
On the propagation of love waves in an infinite cylindrical surface |
| url |
https://doi.org/10.1007/BF00875915 |
| remote_bool |
false |
| ppnlink |
129538353 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/BF00875915 |
| up_date |
2024-07-03T22:14:48.033Z |
| _version_ |
1803597788516188160 |
| 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">OLC2069456242</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230323111912.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1974 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF00875915</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2069456242</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF00875915-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="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">De, Sasadhar</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">On the propagation of love waves in an infinite cylindrical surface</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1974</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">© Birkhäuser-Verlag 1974</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Summary In the first part of this paper the propagation of Love type waves in an infinite cylindrical surface of transversely isotropic material with a central core of different material is investigated. In the second part, the propagation of such waves over a circular cylindrical surface of layered earth model of cylindrically aeolotropic material is considered and the corresponding dispersion equation is derived. The change in the dispersion equation for such waves, due to harmonic variation in the thickness of the cylindrical crustal layer when the earth is composed of anisotropic material, has also been considered.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Isotropic Material</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Dispersion Equation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Central Core</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Anisotropic Material</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Pure and applied geophysics</subfield><subfield code="d">Birkhäuser-Verlag, 1964</subfield><subfield code="g">112(1974), 1 vom: Jan., Seite 35-45</subfield><subfield code="w">(DE-627)129538353</subfield><subfield code="w">(DE-600)216719-0</subfield><subfield code="w">(DE-576)014971038</subfield><subfield code="x">0033-4553</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:112</subfield><subfield code="g">year:1974</subfield><subfield code="g">number:1</subfield><subfield code="g">month:01</subfield><subfield code="g">pages:35-45</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF00875915</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">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</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_30</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</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_267</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_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</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_4028</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4029</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">112</subfield><subfield code="j">1974</subfield><subfield code="e">1</subfield><subfield code="c">01</subfield><subfield code="h">35-45</subfield></datafield></record></collection>
|
| score |
7.399687 |