Seismicity in Mines:
Recent seismological research has focused on processes other than pure shear failure (double-couple) as an alternative mechanism for some types of seismic events. This has been stimulated by what appears to be anomalous focal mecha nisms observed for several earthquakes of possible volcanic nature i...
Saved in:
| Other Authors: | |
|---|---|
| Format: | Electronic eBook |
| Language: | English |
| Published: |
Basel
Birkhäuser Basel
1989
|
| Series: | Pageoph Topical Volumes
|
| Subjects: | |
| Online Access: | BTU01 Volltext |
| Summary: | Recent seismological research has focused on processes other than pure shear failure (double-couple) as an alternative mechanism for some types of seismic events. This has been stimulated by what appears to be anomalous focal mecha nisms observed for several earthquakes of possible volcanic nature in the 1980 Mammoth Lakes, California sequence (JULIAN and SIPKIN, 1985; SIPKIN, 1986). Although studies have concentrated on earthquakes associated with magmatic processes, possible non-double-couple seismic failure has been observed, but not widely known, in cases of mine seismicity in the past three decades. Such cases have occurred on a world-wide basis; however, no cases until now have been observed in the United States. The existence of non-double-couple failure in mine seismicity has been controversial as it has been for tectonic/volcanic earthquakes. Several of the benchmark studies of mine seismicity in the deep South African gold mines have resulted in the belief that no fundamental distinction in the source mechanism exists between tectonic earthquakes and rock bursts (MCGARR, 1984); both types of events are the result of pure shear failure. However, the reported cases of implo sional focal mechanisms for mine seismicity continue to increase in number and prolong the controversy. During the summer of 1984, a three-dimensional, high resolution micro earthquake network was operated by Woodward-Clyde Consultants (WCC) in the vicinity of two coal mines beneath Gentry Mountain in the eastern Wasatch Plateau of central Utah |
| Physical Description: | 1 Online-Ressource (404 p. 2 illus) |
| ISBN: | 9783034892704 |
| DOI: | 10.1007/978-3-0348-9270-4 |
Staff View
MARC
| LEADER | 00000nmm a2200000zc 4500 | ||
|---|---|---|---|
| 001 | BV045178015 | ||
| 003 | DE-604 | ||
| 005 | 20180911 | ||
| 007 | cr|uuu---uuuuu | ||
| 008 | 180911s1989 |||| o||u| ||||||eng d | ||
| 020 | |a 9783034892704 |9 978-3-0348-9270-4 | ||
| 024 | 7 | |a 10.1007/978-3-0348-9270-4 |2 doi | |
| 035 | |a (ZDB-2-EES)978-3-0348-9270-4 | ||
| 035 | |a (OCoLC)1053830979 | ||
| 035 | |a (DE-599)BVBBV045178015 | ||
| 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 | |
| 245 | 1 | 0 | |a Seismicity in Mines |c edited by Sławomir J. Gibowicz |
| 246 | 1 | 3 | |a Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 129 (1989), No. 3/4 |
| 264 | 1 | |a Basel |b Birkhäuser Basel |c 1989 | |
| 300 | |a 1 Online-Ressource (404 p. 2 illus) | ||
| 336 | |b txt |2 rdacontent | ||
| 337 | |b c |2 rdamedia | ||
| 338 | |b cr |2 rdacarrier | ||
| 490 | 0 | |a Pageoph Topical Volumes | |
| 520 | |a Recent seismological research has focused on processes other than pure shear failure (double-couple) as an alternative mechanism for some types of seismic events. This has been stimulated by what appears to be anomalous focal mecha nisms observed for several earthquakes of possible volcanic nature in the 1980 Mammoth Lakes, California sequence (JULIAN and SIPKIN, 1985; SIPKIN, 1986). Although studies have concentrated on earthquakes associated with magmatic processes, possible non-double-couple seismic failure has been observed, but not widely known, in cases of mine seismicity in the past three decades. Such cases have occurred on a world-wide basis; however, no cases until now have been observed in the United States. The existence of non-double-couple failure in mine seismicity has been controversial as it has been for tectonic/volcanic earthquakes. Several of the benchmark studies of mine seismicity in the deep South African gold mines have resulted in the belief that no fundamental distinction in the source mechanism exists between tectonic earthquakes and rock bursts (MCGARR, 1984); both types of events are the result of pure shear failure. However, the reported cases of implo sional focal mechanisms for mine seismicity continue to increase in number and prolong the controversy. During the summer of 1984, a three-dimensional, high resolution micro earthquake network was operated by Woodward-Clyde Consultants (WCC) in the vicinity of two coal mines beneath Gentry Mountain in the eastern Wasatch Plateau of central Utah | ||
| 650 | 4 | |a Earth Sciences | |
| 650 | 4 | |a Geophysics/Geodesy | |
| 650 | 4 | |a Earth sciences | |
| 650 | 4 | |a Geophysics | |
| 700 | 1 | |a Gibowicz, Sławomir J. |4 edt | |
| 776 | 0 | 8 | |i Erscheint auch als |n Druck-Ausgabe |z 9783764322731 |
| 856 | 4 | 0 | |u https://doi.org/10.1007/978-3-0348-9270-4 |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:BVB01-030567245 | ||
| 966 | e | |u https://doi.org/10.1007/978-3-0348-9270-4 |l BTU01 |p ZDB-2-EES |q ZDB-2-EES_Archiv |x Verlag |3 Volltext | |
Record in the Search Index
| _version_ | 1804178867732086784 |
|---|---|
| any_adam_object | |
| author2 | Gibowicz, Sławomir J. |
| author2_role | edt |
| author2_variant | s j g sj sjg |
| author_facet | Gibowicz, Sławomir J. |
| building | Verbundindex |
| bvnumber | BV045178015 |
| collection | ZDB-2-EES |
| ctrlnum | (ZDB-2-EES)978-3-0348-9270-4 (OCoLC)1053830979 (DE-599)BVBBV045178015 |
| 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 | 10.1007/978-3-0348-9270-4 |
| format | Electronic eBook |
| fullrecord | <?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>03041nmm a2200445zc 4500</leader><controlfield tag="001">BV045178015</controlfield><controlfield tag="003">DE-604</controlfield><controlfield tag="005">20180911 </controlfield><controlfield tag="007">cr|uuu---uuuuu</controlfield><controlfield tag="008">180911s1989 |||| o||u| ||||||eng d</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9783034892704</subfield><subfield code="9">978-3-0348-9270-4</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-3-0348-9270-4</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ZDB-2-EES)978-3-0348-9270-4</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1053830979</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)BVBBV045178015</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="245" ind1="1" ind2="0"><subfield code="a">Seismicity in Mines</subfield><subfield code="c">edited by Sławomir J. Gibowicz</subfield></datafield><datafield tag="246" ind1="1" ind2="3"><subfield code="a">Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 129 (1989), No. 3/4</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Basel</subfield><subfield code="b">Birkhäuser Basel</subfield><subfield code="c">1989</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (404 p. 2 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="490" ind1="0" ind2=" "><subfield code="a">Pageoph Topical Volumes</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Recent seismological research has focused on processes other than pure shear failure (double-couple) as an alternative mechanism for some types of seismic events. This has been stimulated by what appears to be anomalous focal mecha nisms observed for several earthquakes of possible volcanic nature in the 1980 Mammoth Lakes, California sequence (JULIAN and SIPKIN, 1985; SIPKIN, 1986). Although studies have concentrated on earthquakes associated with magmatic processes, possible non-double-couple seismic failure has been observed, but not widely known, in cases of mine seismicity in the past three decades. Such cases have occurred on a world-wide basis; however, no cases until now have been observed in the United States. The existence of non-double-couple failure in mine seismicity has been controversial as it has been for tectonic/volcanic earthquakes. Several of the benchmark studies of mine seismicity in the deep South African gold mines have resulted in the belief that no fundamental distinction in the source mechanism exists between tectonic earthquakes and rock bursts (MCGARR, 1984); both types of events are the result of pure shear failure. However, the reported cases of implo sional focal mechanisms for mine seismicity continue to increase in number and prolong the controversy. During the summer of 1984, a three-dimensional, high resolution micro earthquake network was operated by Woodward-Clyde Consultants (WCC) in the vicinity of two coal mines beneath Gentry Mountain in the eastern Wasatch Plateau of central Utah</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">Gibowicz, Sławomir J.</subfield><subfield code="4">edt</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">9783764322731</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1007/978-3-0348-9270-4</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:BVB01-030567245</subfield></datafield><datafield tag="966" ind1="e" ind2=" "><subfield code="u">https://doi.org/10.1007/978-3-0348-9270-4</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.BV045178015 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:48Z |
| institution | BVB |
| isbn | 9783034892704 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030567245 |
| oclc_num | 1053830979 |
| open_access_boolean | |
| owner | DE-634 |
| owner_facet | DE-634 |
| physical | 1 Online-Ressource (404 p. 2 illus) |
| psigel | ZDB-2-EES ZDB-2-EES_Archiv ZDB-2-EES ZDB-2-EES_Archiv |
| publishDate | 1989 |
| publishDateSearch | 1989 |
| publishDateSort | 1989 |
| publisher | Birkhäuser Basel |
| record_format | marc |
| series2 | Pageoph Topical Volumes |
| spelling | Seismicity in Mines edited by Sławomir J. Gibowicz Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 129 (1989), No. 3/4 Basel Birkhäuser Basel 1989 1 Online-Ressource (404 p. 2 illus) txt rdacontent c rdamedia cr rdacarrier Pageoph Topical Volumes Recent seismological research has focused on processes other than pure shear failure (double-couple) as an alternative mechanism for some types of seismic events. This has been stimulated by what appears to be anomalous focal mecha nisms observed for several earthquakes of possible volcanic nature in the 1980 Mammoth Lakes, California sequence (JULIAN and SIPKIN, 1985; SIPKIN, 1986). Although studies have concentrated on earthquakes associated with magmatic processes, possible non-double-couple seismic failure has been observed, but not widely known, in cases of mine seismicity in the past three decades. Such cases have occurred on a world-wide basis; however, no cases until now have been observed in the United States. The existence of non-double-couple failure in mine seismicity has been controversial as it has been for tectonic/volcanic earthquakes. Several of the benchmark studies of mine seismicity in the deep South African gold mines have resulted in the belief that no fundamental distinction in the source mechanism exists between tectonic earthquakes and rock bursts (MCGARR, 1984); both types of events are the result of pure shear failure. However, the reported cases of implo sional focal mechanisms for mine seismicity continue to increase in number and prolong the controversy. During the summer of 1984, a three-dimensional, high resolution micro earthquake network was operated by Woodward-Clyde Consultants (WCC) in the vicinity of two coal mines beneath Gentry Mountain in the eastern Wasatch Plateau of central Utah Earth Sciences Geophysics/Geodesy Earth sciences Geophysics Gibowicz, Sławomir J. edt Erscheint auch als Druck-Ausgabe 9783764322731 https://doi.org/10.1007/978-3-0348-9270-4 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Seismicity in Mines Earth Sciences Geophysics/Geodesy Earth sciences Geophysics |
| title | Seismicity in Mines |
| title_alt | Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 129 (1989), No. 3/4 |
| title_auth | Seismicity in Mines |
| title_exact_search | Seismicity in Mines |
| title_full | Seismicity in Mines edited by Sławomir J. Gibowicz |
| title_fullStr | Seismicity in Mines edited by Sławomir J. Gibowicz |
| title_full_unstemmed | Seismicity in Mines edited by Sławomir J. Gibowicz |
| title_short | Seismicity in Mines |
| title_sort | seismicity in mines |
| topic | Earth Sciences Geophysics/Geodesy Earth sciences Geophysics |
| topic_facet | Earth Sciences Geophysics/Geodesy Earth sciences Geophysics |
| url | https://doi.org/10.1007/978-3-0348-9270-4 |
| work_keys_str_mv | AT gibowiczsławomirj seismicityinmines AT gibowiczsławomirj reprintfrompureandappliedgeophysicspageophvolume1291989no34 |