Seismic Love Waves:
Among seismic waves generated by widely dilferent types of sources, the waves that are the most interest ing and of the longest duration are usually surface waves (which are also called normal waves, interference and channel waves, natural vibrations of layers, etc. ). These waves are distinguished...
Gespeichert in:
| Hauptverfasser: | , , , |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Boston, MA
Springer US
1995
|
| Schlagworte: | |
| Online-Zugang: | BTU01 URL des Erstveröffentlichers |
| Zusammenfassung: | Among seismic waves generated by widely dilferent types of sources, the waves that are the most interest ing and of the longest duration are usually surface waves (which are also called normal waves, interference and channel waves, natural vibrations of layers, etc. ). These waves are distinguished by their dispersion and reso nance, and are used in many investigations - in the determination of the structure of the medium (the existence of surface layers and waveguides), in the determination of the coordinates and properties of the source (in par ticular its energy and mechanism), in the identification of subterranean exploSions, in the mapping of micro- seisms, in the tracing of storms, etc. Outlines of the wide literature concerning surface waves can be found in [2, 9, 40J. Surface waves can be classed as Rayleigh or Love waves, depending on their velocity and polarization: the displacements of particles in Rayleigh waves are parallel, and the displacements in Love waves perpendicular, to the vertical plane containing the direction of propagation (some variation from this polarization is possible close to the source or in the presence of horizontal inhomogeneities in the medium). The present work is devoted to the calculation and investigation of Love waves in a vertically layered medium. The method used is based on the spectral theory of linear differential operators. ' This method is much more effective than previously applied methods based on the approximation of the medium by a set of homogeneous layers |
| Beschreibung: | 1 Online-Ressource (XIV, 91 p. 33 illus) |
| ISBN: | 9781468486049 |
| DOI: | 10.1007/978-1-4684-8604-9 |
Internformat
MARC
| LEADER | 00000nmm a2200000zc 4500 | ||
|---|---|---|---|
| 001 | BV045177698 | ||
| 003 | DE-604 | ||
| 005 | 00000000000000.0 | ||
| 007 | cr|uuu---uuuuu | ||
| 008 | 180911s1995 |||| o||u| ||||||eng d | ||
| 020 | |a 9781468486049 |9 978-1-4684-8604-9 | ||
| 024 | 7 | |a 10.1007/978-1-4684-8604-9 |2 doi | |
| 035 | |a (ZDB-2-EES)978-1-4684-8604-9 | ||
| 035 | |a (OCoLC)1053814754 | ||
| 035 | |a (DE-599)BVBBV045177698 | ||
| 040 | |a DE-604 |b ger |e aacr | ||
| 041 | 0 | |a eng | |
| 049 | |a DE-634 | ||
| 082 | 0 | |a 550 |2 23 | |
| 082 | 0 | |a 526.1 |2 23 | |
| 100 | 1 | |a Andrianova, Z. S. |e Verfasser |4 aut | |
| 245 | 1 | 0 | |a Seismic Love Waves |c by Z. S. Andrianova, A. L. Levshin, V. I. Keilis-Borok, M. G. Neigauz |
| 264 | 1 | |a Boston, MA |b Springer US |c 1995 | |
| 300 | |a 1 Online-Ressource (XIV, 91 p. 33 illus) | ||
| 336 | |b txt |2 rdacontent | ||
| 337 | |b c |2 rdamedia | ||
| 338 | |b cr |2 rdacarrier | ||
| 520 | |a Among seismic waves generated by widely dilferent types of sources, the waves that are the most interest ing and of the longest duration are usually surface waves (which are also called normal waves, interference and channel waves, natural vibrations of layers, etc. ). These waves are distinguished by their dispersion and reso nance, and are used in many investigations - in the determination of the structure of the medium (the existence of surface layers and waveguides), in the determination of the coordinates and properties of the source (in par ticular its energy and mechanism), in the identification of subterranean exploSions, in the mapping of micro- seisms, in the tracing of storms, etc. Outlines of the wide literature concerning surface waves can be found in [2, 9, 40J. Surface waves can be classed as Rayleigh or Love waves, depending on their velocity and polarization: the displacements of particles in Rayleigh waves are parallel, and the displacements in Love waves perpendicular, to the vertical plane containing the direction of propagation (some variation from this polarization is possible close to the source or in the presence of horizontal inhomogeneities in the medium). The present work is devoted to the calculation and investigation of Love waves in a vertically layered medium. The method used is based on the spectral theory of linear differential operators. ' This method is much more effective than previously applied methods based on the approximation of the medium by a set of homogeneous layers | ||
| 650 | 4 | |a Earth Sciences | |
| 650 | 4 | |a Geophysics/Geodesy | |
| 650 | 4 | |a Earth sciences | |
| 650 | 4 | |a Geophysics | |
| 700 | 1 | |a Levshin, A. L. |4 aut | |
| 700 | 1 | |a Keilis-Borok, V. I. |4 aut | |
| 700 | 1 | |a Neigauz, M. G. |4 aut | |
| 776 | 0 | 8 | |i Erscheint auch als |n Druck-Ausgabe |z 9781468486063 |
| 856 | 4 | 0 | |u https://doi.org/10.1007/978-1-4684-8604-9 |x Verlag |z URL des Erstveröffentlichers |3 Volltext |
| 912 | |a ZDB-2-EES | ||
| 940 | 1 | |q ZDB-2-EES_Archiv | |
| 999 | |a oai:aleph.bib-bvb.de:BVB01-030566928 | ||
| 966 | e | |u https://doi.org/10.1007/978-1-4684-8604-9 |l BTU01 |p ZDB-2-EES |q ZDB-2-EES_Archiv |x Verlag |3 Volltext | |
Datensatz im Suchindex
| _version_ | 1804178867018006528 |
|---|---|
| any_adam_object | |
| author | Andrianova, Z. S. Levshin, A. L. Keilis-Borok, V. I. Neigauz, M. G. |
| author_facet | Andrianova, Z. S. Levshin, A. L. Keilis-Borok, V. I. Neigauz, M. G. |
| author_role | aut aut aut aut |
| author_sort | Andrianova, Z. S. |
| author_variant | z s a zs zsa a l l al all v i k b vik vikb m g n mg mgn |
| building | Verbundindex |
| bvnumber | BV045177698 |
| collection | ZDB-2-EES |
| ctrlnum | (ZDB-2-EES)978-1-4684-8604-9 (OCoLC)1053814754 (DE-599)BVBBV045177698 |
| dewey-full | 550 526.1 |
| dewey-hundreds | 500 - Natural sciences and mathematics |
| dewey-ones | 550 - Earth sciences 526 - Mathematical geography |
| dewey-raw | 550 526.1 |
| dewey-search | 550 526.1 |
| dewey-sort | 3550 |
| dewey-tens | 550 - Earth sciences 520 - Astronomy and allied sciences |
| discipline | Geologie / Paläontologie Physik |
| doi_str_mv | 10.1007/978-1-4684-8604-9 |
| format | Electronic eBook |
| fullrecord | <?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>03053nmm a2200457zc 4500</leader><controlfield tag="001">BV045177698</controlfield><controlfield tag="003">DE-604</controlfield><controlfield tag="005">00000000000000.0</controlfield><controlfield tag="007">cr|uuu---uuuuu</controlfield><controlfield tag="008">180911s1995 |||| o||u| ||||||eng d</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9781468486049</subfield><subfield code="9">978-1-4684-8604-9</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-1-4684-8604-9</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ZDB-2-EES)978-1-4684-8604-9</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1053814754</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)BVBBV045177698</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-604</subfield><subfield code="b">ger</subfield><subfield code="e">aacr</subfield></datafield><datafield tag="041" ind1="0" ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="049" ind1=" " ind2=" "><subfield code="a">DE-634</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">550</subfield><subfield code="2">23</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">526.1</subfield><subfield code="2">23</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Andrianova, Z. S.</subfield><subfield code="e">Verfasser</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Seismic Love Waves</subfield><subfield code="c">by Z. S. Andrianova, A. L. Levshin, V. I. Keilis-Borok, M. G. Neigauz</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Boston, MA</subfield><subfield code="b">Springer US</subfield><subfield code="c">1995</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (XIV, 91 p. 33 illus)</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Among seismic waves generated by widely dilferent types of sources, the waves that are the most interest ing and of the longest duration are usually surface waves (which are also called normal waves, interference and channel waves, natural vibrations of layers, etc. ). These waves are distinguished by their dispersion and reso nance, and are used in many investigations - in the determination of the structure of the medium (the existence of surface layers and waveguides), in the determination of the coordinates and properties of the source (in par ticular its energy and mechanism), in the identification of subterranean exploSions, in the mapping of micro- seisms, in the tracing of storms, etc. Outlines of the wide literature concerning surface waves can be found in [2, 9, 40J. Surface waves can be classed as Rayleigh or Love waves, depending on their velocity and polarization: the displacements of particles in Rayleigh waves are parallel, and the displacements in Love waves perpendicular, to the vertical plane containing the direction of propagation (some variation from this polarization is possible close to the source or in the presence of horizontal inhomogeneities in the medium). The present work is devoted to the calculation and investigation of Love waves in a vertically layered medium. The method used is based on the spectral theory of linear differential operators. ' This method is much more effective than previously applied methods based on the approximation of the medium by a set of homogeneous layers</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geophysics/Geodesy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geophysics</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Levshin, A. L.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Keilis-Borok, V. I.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Neigauz, M. G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="776" ind1="0" ind2="8"><subfield code="i">Erscheint auch als</subfield><subfield code="n">Druck-Ausgabe</subfield><subfield code="z">9781468486063</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1007/978-1-4684-8604-9</subfield><subfield code="x">Verlag</subfield><subfield code="z">URL des Erstveröffentlichers</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-2-EES</subfield></datafield><datafield tag="940" ind1="1" ind2=" "><subfield code="q">ZDB-2-EES_Archiv</subfield></datafield><datafield tag="999" ind1=" " ind2=" "><subfield code="a">oai:aleph.bib-bvb.de:BVB01-030566928</subfield></datafield><datafield tag="966" ind1="e" ind2=" "><subfield code="u">https://doi.org/10.1007/978-1-4684-8604-9</subfield><subfield code="l">BTU01</subfield><subfield code="p">ZDB-2-EES</subfield><subfield code="q">ZDB-2-EES_Archiv</subfield><subfield code="x">Verlag</subfield><subfield code="3">Volltext</subfield></datafield></record></collection> |
| id | DE-604.BV045177698 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:47Z |
| institution | BVB |
| isbn | 9781468486049 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030566928 |
| oclc_num | 1053814754 |
| open_access_boolean | |
| owner | DE-634 |
| owner_facet | DE-634 |
| physical | 1 Online-Ressource (XIV, 91 p. 33 illus) |
| psigel | ZDB-2-EES ZDB-2-EES_Archiv ZDB-2-EES ZDB-2-EES_Archiv |
| publishDate | 1995 |
| publishDateSearch | 1995 |
| publishDateSort | 1995 |
| publisher | Springer US |
| record_format | marc |
| spelling | Andrianova, Z. S. Verfasser aut Seismic Love Waves by Z. S. Andrianova, A. L. Levshin, V. I. Keilis-Borok, M. G. Neigauz Boston, MA Springer US 1995 1 Online-Ressource (XIV, 91 p. 33 illus) txt rdacontent c rdamedia cr rdacarrier Among seismic waves generated by widely dilferent types of sources, the waves that are the most interest ing and of the longest duration are usually surface waves (which are also called normal waves, interference and channel waves, natural vibrations of layers, etc. ). These waves are distinguished by their dispersion and reso nance, and are used in many investigations - in the determination of the structure of the medium (the existence of surface layers and waveguides), in the determination of the coordinates and properties of the source (in par ticular its energy and mechanism), in the identification of subterranean exploSions, in the mapping of micro- seisms, in the tracing of storms, etc. Outlines of the wide literature concerning surface waves can be found in [2, 9, 40J. Surface waves can be classed as Rayleigh or Love waves, depending on their velocity and polarization: the displacements of particles in Rayleigh waves are parallel, and the displacements in Love waves perpendicular, to the vertical plane containing the direction of propagation (some variation from this polarization is possible close to the source or in the presence of horizontal inhomogeneities in the medium). The present work is devoted to the calculation and investigation of Love waves in a vertically layered medium. The method used is based on the spectral theory of linear differential operators. ' This method is much more effective than previously applied methods based on the approximation of the medium by a set of homogeneous layers Earth Sciences Geophysics/Geodesy Earth sciences Geophysics Levshin, A. L. aut Keilis-Borok, V. I. aut Neigauz, M. G. aut Erscheint auch als Druck-Ausgabe 9781468486063 https://doi.org/10.1007/978-1-4684-8604-9 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Andrianova, Z. S. Levshin, A. L. Keilis-Borok, V. I. Neigauz, M. G. Seismic Love Waves Earth Sciences Geophysics/Geodesy Earth sciences Geophysics |
| title | Seismic Love Waves |
| title_auth | Seismic Love Waves |
| title_exact_search | Seismic Love Waves |
| title_full | Seismic Love Waves by Z. S. Andrianova, A. L. Levshin, V. I. Keilis-Borok, M. G. Neigauz |
| title_fullStr | Seismic Love Waves by Z. S. Andrianova, A. L. Levshin, V. I. Keilis-Borok, M. G. Neigauz |
| title_full_unstemmed | Seismic Love Waves by Z. S. Andrianova, A. L. Levshin, V. I. Keilis-Borok, M. G. Neigauz |
| title_short | Seismic Love Waves |
| title_sort | seismic love waves |
| topic | Earth Sciences Geophysics/Geodesy Earth sciences Geophysics |
| topic_facet | Earth Sciences Geophysics/Geodesy Earth sciences Geophysics |
| url | https://doi.org/10.1007/978-1-4684-8604-9 |
| work_keys_str_mv | AT andrianovazs seismiclovewaves AT levshinal seismiclovewaves AT keilisborokvi seismiclovewaves AT neigauzmg seismiclovewaves |