Simulated annealing for earthquake location
Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In...
Ausführliche Beschreibung
Autor*in: |
Xiaohan Li [verfasserIn] Guangke Li [verfasserIn] Dawei Jiao [verfasserIn] |
---|
Format: |
E-Artikel |
---|---|
Sprache: |
Chinesisch |
Erschienen: |
2021 |
---|
Schlagwörter: |
---|
Übergeordnetes Werk: |
In: 地震科学进展 - Editorial Office of Progress in Earthquake Sciences, 2023, 51(2021), 5, Seite 223-229 |
---|---|
Übergeordnetes Werk: |
volume:51 ; year:2021 ; number:5 ; pages:223-229 |
Links: |
---|
DOI / URN: |
10.3969/j.issn.2096-7780.2021.05.004 |
---|
Katalog-ID: |
DOAJ087475006 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | DOAJ087475006 | ||
003 | DE-627 | ||
005 | 20230503013230.0 | ||
007 | cr uuu---uuuuu | ||
008 | 230331s2021 xx |||||o 00| ||chi c | ||
024 | 7 | |a 10.3969/j.issn.2096-7780.2021.05.004 |2 doi | |
035 | |a (DE-627)DOAJ087475006 | ||
035 | |a (DE-599)DOAJfe29df8618b44ecb8b9f32cc7357c080 | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a chi | ||
050 | 0 | |a QE1-996.5 | |
050 | 0 | |a TA1-2040 | |
100 | 0 | |a Xiaohan Li |e verfasserin |4 aut | |
245 | 1 | 0 | |a Simulated annealing for earthquake location |
264 | 1 | |c 2021 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a Computermedien |b c |2 rdamedia | ||
338 | |a Online-Ressource |b cr |2 rdacarrier | ||
520 | |a Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm. | ||
650 | 4 | |a earthquake location | |
650 | 4 | |a simulated annealing algorithm | |
650 | 4 | |a optimization algorithm | |
653 | 0 | |a Geology | |
653 | 0 | |a Engineering (General). Civil engineering (General) | |
700 | 0 | |a Guangke Li |e verfasserin |4 aut | |
700 | 0 | |a Dawei Jiao |e verfasserin |4 aut | |
773 | 0 | 8 | |i In |t 地震科学进展 |d Editorial Office of Progress in Earthquake Sciences, 2023 |g 51(2021), 5, Seite 223-229 |w (DE-627)DOAJ087193949 |x 20967780 |7 nnns |
773 | 1 | 8 | |g volume:51 |g year:2021 |g number:5 |g pages:223-229 |
856 | 4 | 0 | |u https://doi.org/10.3969/j.issn.2096-7780.2021.05.004 |z kostenfrei |
856 | 4 | 0 | |u https://doaj.org/article/fe29df8618b44ecb8b9f32cc7357c080 |z kostenfrei |
856 | 4 | 0 | |u https://www.gjdzdt.cn/en/article/doi/10.3969/j.issn.2096-7780.2021.05.004 |z kostenfrei |
856 | 4 | 2 | |u https://doaj.org/toc/2096-7780 |y Journal toc |z kostenfrei |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_DOAJ | ||
912 | |a SSG-OLC-PHA | ||
912 | |a GBV_ILN_342 | ||
951 | |a AR | ||
952 | |d 51 |j 2021 |e 5 |h 223-229 |
author_variant |
x l xl g l gl d j dj |
---|---|
matchkey_str |
article:20967780:2021----::iuaeanaigoerh |
hierarchy_sort_str |
2021 |
callnumber-subject-code |
QE |
publishDate |
2021 |
allfields |
10.3969/j.issn.2096-7780.2021.05.004 doi (DE-627)DOAJ087475006 (DE-599)DOAJfe29df8618b44ecb8b9f32cc7357c080 DE-627 ger DE-627 rakwb chi QE1-996.5 TA1-2040 Xiaohan Li verfasserin aut Simulated annealing for earthquake location 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm. earthquake location simulated annealing algorithm optimization algorithm Geology Engineering (General). Civil engineering (General) Guangke Li verfasserin aut Dawei Jiao verfasserin aut In 地震科学进展 Editorial Office of Progress in Earthquake Sciences, 2023 51(2021), 5, Seite 223-229 (DE-627)DOAJ087193949 20967780 nnns volume:51 year:2021 number:5 pages:223-229 https://doi.org/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/article/fe29df8618b44ecb8b9f32cc7357c080 kostenfrei https://www.gjdzdt.cn/en/article/doi/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/toc/2096-7780 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_342 AR 51 2021 5 223-229 |
spelling |
10.3969/j.issn.2096-7780.2021.05.004 doi (DE-627)DOAJ087475006 (DE-599)DOAJfe29df8618b44ecb8b9f32cc7357c080 DE-627 ger DE-627 rakwb chi QE1-996.5 TA1-2040 Xiaohan Li verfasserin aut Simulated annealing for earthquake location 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm. earthquake location simulated annealing algorithm optimization algorithm Geology Engineering (General). Civil engineering (General) Guangke Li verfasserin aut Dawei Jiao verfasserin aut In 地震科学进展 Editorial Office of Progress in Earthquake Sciences, 2023 51(2021), 5, Seite 223-229 (DE-627)DOAJ087193949 20967780 nnns volume:51 year:2021 number:5 pages:223-229 https://doi.org/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/article/fe29df8618b44ecb8b9f32cc7357c080 kostenfrei https://www.gjdzdt.cn/en/article/doi/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/toc/2096-7780 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_342 AR 51 2021 5 223-229 |
allfields_unstemmed |
10.3969/j.issn.2096-7780.2021.05.004 doi (DE-627)DOAJ087475006 (DE-599)DOAJfe29df8618b44ecb8b9f32cc7357c080 DE-627 ger DE-627 rakwb chi QE1-996.5 TA1-2040 Xiaohan Li verfasserin aut Simulated annealing for earthquake location 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm. earthquake location simulated annealing algorithm optimization algorithm Geology Engineering (General). Civil engineering (General) Guangke Li verfasserin aut Dawei Jiao verfasserin aut In 地震科学进展 Editorial Office of Progress in Earthquake Sciences, 2023 51(2021), 5, Seite 223-229 (DE-627)DOAJ087193949 20967780 nnns volume:51 year:2021 number:5 pages:223-229 https://doi.org/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/article/fe29df8618b44ecb8b9f32cc7357c080 kostenfrei https://www.gjdzdt.cn/en/article/doi/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/toc/2096-7780 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_342 AR 51 2021 5 223-229 |
allfieldsGer |
10.3969/j.issn.2096-7780.2021.05.004 doi (DE-627)DOAJ087475006 (DE-599)DOAJfe29df8618b44ecb8b9f32cc7357c080 DE-627 ger DE-627 rakwb chi QE1-996.5 TA1-2040 Xiaohan Li verfasserin aut Simulated annealing for earthquake location 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm. earthquake location simulated annealing algorithm optimization algorithm Geology Engineering (General). Civil engineering (General) Guangke Li verfasserin aut Dawei Jiao verfasserin aut In 地震科学进展 Editorial Office of Progress in Earthquake Sciences, 2023 51(2021), 5, Seite 223-229 (DE-627)DOAJ087193949 20967780 nnns volume:51 year:2021 number:5 pages:223-229 https://doi.org/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/article/fe29df8618b44ecb8b9f32cc7357c080 kostenfrei https://www.gjdzdt.cn/en/article/doi/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/toc/2096-7780 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_342 AR 51 2021 5 223-229 |
allfieldsSound |
10.3969/j.issn.2096-7780.2021.05.004 doi (DE-627)DOAJ087475006 (DE-599)DOAJfe29df8618b44ecb8b9f32cc7357c080 DE-627 ger DE-627 rakwb chi QE1-996.5 TA1-2040 Xiaohan Li verfasserin aut Simulated annealing for earthquake location 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm. earthquake location simulated annealing algorithm optimization algorithm Geology Engineering (General). Civil engineering (General) Guangke Li verfasserin aut Dawei Jiao verfasserin aut In 地震科学进展 Editorial Office of Progress in Earthquake Sciences, 2023 51(2021), 5, Seite 223-229 (DE-627)DOAJ087193949 20967780 nnns volume:51 year:2021 number:5 pages:223-229 https://doi.org/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/article/fe29df8618b44ecb8b9f32cc7357c080 kostenfrei https://www.gjdzdt.cn/en/article/doi/10.3969/j.issn.2096-7780.2021.05.004 kostenfrei https://doaj.org/toc/2096-7780 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_342 AR 51 2021 5 223-229 |
language |
Chinese |
source |
In 地震科学进展 51(2021), 5, Seite 223-229 volume:51 year:2021 number:5 pages:223-229 |
sourceStr |
In 地震科学进展 51(2021), 5, Seite 223-229 volume:51 year:2021 number:5 pages:223-229 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
earthquake location simulated annealing algorithm optimization algorithm Geology Engineering (General). Civil engineering (General) |
isfreeaccess_bool |
true |
container_title |
地震科学进展 |
authorswithroles_txt_mv |
Xiaohan Li @@aut@@ Guangke Li @@aut@@ Dawei Jiao @@aut@@ |
publishDateDaySort_date |
2021-01-01T00:00:00Z |
hierarchy_top_id |
DOAJ087193949 |
id |
DOAJ087475006 |
language_de |
chinesisch |
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">DOAJ087475006</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503013230.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230331s2021 xx |||||o 00| ||chi c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.3969/j.issn.2096-7780.2021.05.004</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ087475006</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJfe29df8618b44ecb8b9f32cc7357c080</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">chi</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QE1-996.5</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">TA1-2040</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Xiaohan Li</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Simulated annealing for earthquake location</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2021</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">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">earthquake location</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">simulated annealing algorithm</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">optimization algorithm</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Geology</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Engineering (General). Civil engineering (General)</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Guangke Li</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Dawei Jiao</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">地震科学进展</subfield><subfield code="d">Editorial Office of Progress in Earthquake Sciences, 2023</subfield><subfield code="g">51(2021), 5, Seite 223-229</subfield><subfield code="w">(DE-627)DOAJ087193949</subfield><subfield code="x">20967780</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:51</subfield><subfield code="g">year:2021</subfield><subfield code="g">number:5</subfield><subfield code="g">pages:223-229</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.3969/j.issn.2096-7780.2021.05.004</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/fe29df8618b44ecb8b9f32cc7357c080</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://www.gjdzdt.cn/en/article/doi/10.3969/j.issn.2096-7780.2021.05.004</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2096-7780</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</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_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_342</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">51</subfield><subfield code="j">2021</subfield><subfield code="e">5</subfield><subfield code="h">223-229</subfield></datafield></record></collection>
|
callnumber-first |
Q - Science |
author |
Xiaohan Li |
spellingShingle |
Xiaohan Li misc QE1-996.5 misc TA1-2040 misc earthquake location misc simulated annealing algorithm misc optimization algorithm misc Geology misc Engineering (General). Civil engineering (General) Simulated annealing for earthquake location |
authorStr |
Xiaohan Li |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)DOAJ087193949 |
format |
electronic Article |
delete_txt_mv |
keep |
author_role |
aut aut aut |
collection |
DOAJ |
remote_str |
true |
callnumber-label |
QE1-996 |
illustrated |
Not Illustrated |
issn |
20967780 |
topic_title |
QE1-996.5 TA1-2040 Simulated annealing for earthquake location earthquake location simulated annealing algorithm optimization algorithm |
topic |
misc QE1-996.5 misc TA1-2040 misc earthquake location misc simulated annealing algorithm misc optimization algorithm misc Geology misc Engineering (General). Civil engineering (General) |
topic_unstemmed |
misc QE1-996.5 misc TA1-2040 misc earthquake location misc simulated annealing algorithm misc optimization algorithm misc Geology misc Engineering (General). Civil engineering (General) |
topic_browse |
misc QE1-996.5 misc TA1-2040 misc earthquake location misc simulated annealing algorithm misc optimization algorithm misc Geology misc Engineering (General). Civil engineering (General) |
format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
cr |
hierarchy_parent_title |
地震科学进展 |
hierarchy_parent_id |
DOAJ087193949 |
hierarchy_top_title |
地震科学进展 |
isfreeaccess_txt |
true |
familylinks_str_mv |
(DE-627)DOAJ087193949 |
title |
Simulated annealing for earthquake location |
ctrlnum |
(DE-627)DOAJ087475006 (DE-599)DOAJfe29df8618b44ecb8b9f32cc7357c080 |
title_full |
Simulated annealing for earthquake location |
author_sort |
Xiaohan Li |
journal |
地震科学进展 |
journalStr |
地震科学进展 |
callnumber-first-code |
Q |
lang_code |
chi |
isOA_bool |
true |
recordtype |
marc |
publishDateSort |
2021 |
contenttype_str_mv |
txt |
container_start_page |
223 |
author_browse |
Xiaohan Li Guangke Li Dawei Jiao |
container_volume |
51 |
class |
QE1-996.5 TA1-2040 |
format_se |
Elektronische Aufsätze |
author-letter |
Xiaohan Li |
doi_str_mv |
10.3969/j.issn.2096-7780.2021.05.004 |
author2-role |
verfasserin |
title_sort |
simulated annealing for earthquake location |
callnumber |
QE1-996.5 |
title_auth |
Simulated annealing for earthquake location |
abstract |
Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm. |
abstractGer |
Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm. |
abstract_unstemmed |
Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm. |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_342 |
container_issue |
5 |
title_short |
Simulated annealing for earthquake location |
url |
https://doi.org/10.3969/j.issn.2096-7780.2021.05.004 https://doaj.org/article/fe29df8618b44ecb8b9f32cc7357c080 https://www.gjdzdt.cn/en/article/doi/10.3969/j.issn.2096-7780.2021.05.004 https://doaj.org/toc/2096-7780 |
remote_bool |
true |
author2 |
Guangke Li Dawei Jiao |
author2Str |
Guangke Li Dawei Jiao |
ppnlink |
DOAJ087193949 |
callnumber-subject |
QE - Geology |
mediatype_str_mv |
c |
isOA_txt |
true |
hochschulschrift_bool |
false |
doi_str |
10.3969/j.issn.2096-7780.2021.05.004 |
callnumber-a |
QE1-996.5 |
up_date |
2024-07-04T01:50:58.174Z |
_version_ |
1803611388693708800 |
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">DOAJ087475006</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503013230.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230331s2021 xx |||||o 00| ||chi c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.3969/j.issn.2096-7780.2021.05.004</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ087475006</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJfe29df8618b44ecb8b9f32cc7357c080</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">chi</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QE1-996.5</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">TA1-2040</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Xiaohan Li</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Simulated annealing for earthquake location</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2021</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">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Earthquake location is one of the most basic tasks of seismology research such as earthquake monitoring and earthquake prediction. Identification of earthquake location with high efficiency and accuracy is of great significance to the development of works of earthquake prevention and mitigation. In this paper,we invert the earthquake location by simulated annealing algorithm. And then,we change the initial temperature,temperature threshold,cooling-rate,convergence threshold,and disturbance mode respectively to find their influence on the result of simulated annealing algorithm. At last,we summarize and analyze the advantages and disadvantages of simulated annealing algorithm.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">earthquake location</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">simulated annealing algorithm</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">optimization algorithm</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Geology</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Engineering (General). Civil engineering (General)</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Guangke Li</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Dawei Jiao</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">地震科学进展</subfield><subfield code="d">Editorial Office of Progress in Earthquake Sciences, 2023</subfield><subfield code="g">51(2021), 5, Seite 223-229</subfield><subfield code="w">(DE-627)DOAJ087193949</subfield><subfield code="x">20967780</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:51</subfield><subfield code="g">year:2021</subfield><subfield code="g">number:5</subfield><subfield code="g">pages:223-229</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.3969/j.issn.2096-7780.2021.05.004</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/fe29df8618b44ecb8b9f32cc7357c080</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://www.gjdzdt.cn/en/article/doi/10.3969/j.issn.2096-7780.2021.05.004</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2096-7780</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</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_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_342</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">51</subfield><subfield code="j">2021</subfield><subfield code="e">5</subfield><subfield code="h">223-229</subfield></datafield></record></collection>
|
score |
7.3996916 |