Generation mechanism of large later phases of the 2011 Tohoku-oki tsunami causing damages in Hakodate, Hokkaido, Japan View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2019-12

AUTHORS

Yuichiro Tanioka, Mizuho Shibata, Yusuke Yamanaka, Aditya Riadi Gusman, Kei Ioki

ABSTRACT

The 2011 Tohoku-oki earthquake generated a large tsunami that caused catastrophic damage along the Pacific coast of Japan. The major portion of the damage along the Pacific coast of Tohoku in Japan was mainly caused by the first few cycles of tsunami waves. However, the largest phase of the tsunami arriving surprisingly late in Hakodate in Hokkaido, Japan; that is, approximately 9 h after the origin time of the earthquake. It is important to understand the generation mechanism of this large later phase. The tsunami was numerically computed by solving both linear shallow water equations and non-linear shallow water equations with moving boundary conditions throughout the computational area. The later tsunami phases observed on southern Hokkaido can be much better explained by tsunami waveforms computed by solving the non-linear equations than by those computed by solving the linear equations. This suggests that the later tsunami waves arrived at the Hokkaido coast after propagating along the Pacific coast of the Tohoku region with repeated inundations far inland or reflecting from the coast of Tohoku after the inundation. The spectral analysis of the observed waveform at Hakodate tide gauge shows that the later tsunami that arrived between 7.5 and 9.5 h after the earthquake mainly contains a period of 45–50 min. The normal modes of Hakodate Bay were also computed to obtain the eigen periods, eigenfunctions, and spatial distribution of water heights. The computed tsunami height distributions near Hakodate and the fundamental mode of Hakodate Bay indicate that the large later phases are mainly caused by the resonance of the bay, which has a period of approximately 50 min. The results also indicate that the tsunami wave heights near the Hakodate port area, the most populated area in Hakodate, are the largest in the bay because of the resonance of the fundamental mode of the bay. The results of this study suggest that large future tsunamis might excite the fundamental mode of Hakodate Bay and cause large later phases near the Hakodate port. More... »

PAGES

30

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.1186/s40645-019-0278-x

DOI

http://dx.doi.org/10.1186/s40645-019-0278-x

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1113047057


Indexing Status Check whether this publication has been indexed by Scopus and Web Of Science using the SN Indexing Status Tool
Incoming Citations Browse incoming citations for this publication using opencitations.net

JSON-LD is the canonical representation for SciGraph data.

TIP: You can open this SciGraph record using an external JSON-LD service: JSON-LD Playground Google SDTT

[
  {
    "@context": "https://springernature.github.io/scigraph/jsonld/sgcontext.json", 
    "about": [
      {
        "id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/0404", 
        "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
        "name": "Geophysics", 
        "type": "DefinedTerm"
      }, 
      {
        "id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/04", 
        "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
        "name": "Earth Sciences", 
        "type": "DefinedTerm"
      }
    ], 
    "author": [
      {
        "affiliation": {
          "alternateName": "Hokkaido University", 
          "id": "https://www.grid.ac/institutes/grid.39158.36", 
          "name": [
            "Institute of Seismology and Volcanology, Faculty of Science, Hokkaido University, N10W8 Kita-ku, 060-0810, Sapporo, Hokkaido, Japan"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Tanioka", 
        "givenName": "Yuichiro", 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "Central Japan Railway (Japan)", 
          "id": "https://www.grid.ac/institutes/grid.482864.4", 
          "name": [
            "JR Central Japan Railway Company, 450-6101, Nagoya, Aichi, Japan"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Shibata", 
        "givenName": "Mizuho", 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "University of Tokyo", 
          "id": "https://www.grid.ac/institutes/grid.26999.3d", 
          "name": [
            "Department of Civil Engineering, The University of Tokyo, 113-8656, Tokyo, Japan"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Yamanaka", 
        "givenName": "Yusuke", 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "GNS Science", 
          "id": "https://www.grid.ac/institutes/grid.15638.39", 
          "name": [
            "GNS Science, 1 Fairway Drive, Avalon, 5010, Lower Hutt, New Zealand"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Gusman", 
        "givenName": "Aditya Riadi", 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "National Institute of Advanced Industrial Science and Technology", 
          "id": "https://www.grid.ac/institutes/grid.208504.b", 
          "name": [
            "National Institute of Advanced Industrial Science and Technology, 305-8560, Tsukuba, Japan"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Ioki", 
        "givenName": "Kei", 
        "type": "Person"
      }
    ], 
    "citation": [
      {
        "id": "sg:pub.10.5047/eps.2011.06.010", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1000379326", 
          "https://doi.org/10.5047/eps.2011.06.010"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.4294/jpe1952.35.409", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1003336696"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1002/jgrc.20413", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1010501342"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/j.epsl.2012.06.006", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1010877998"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1142/s0578563412500015", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1013244805"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1186/bf03352676", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1024933466", 
          "https://doi.org/10.1186/bf03352676"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/s00024-012-0492-6", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1034189369", 
          "https://doi.org/10.1007/s00024-012-0492-6"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/s10712-006-9000-9", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1037046732", 
          "https://doi.org/10.1007/s10712-006-9000-9"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1007/s00024-006-0164-5", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1041023221", 
          "https://doi.org/10.1007/s00024-006-0164-5"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/2007gl032129", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1043685482"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/2007jc004402", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1044373747"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1029/2007jc004404", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1049952704"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1016/j.margeo.2014.09.043", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1050046481"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1111/j.1365-246x.1988.tb03873.x", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1052819432"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.5194/adgeo-14-129-2008", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1053014507"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1785/0120120122", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1068471762"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1002/2017jb014749", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1100110608"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1002/2017jb014749", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1100110608"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "https://doi.org/10.1002/2017jb014749", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1100110608"
        ], 
        "type": "CreativeWork"
      }
    ], 
    "datePublished": "2019-12", 
    "datePublishedReg": "2019-12-01", 
    "description": "The 2011 Tohoku-oki earthquake generated a large tsunami that caused catastrophic damage along the Pacific coast of Japan. The major portion of the damage along the Pacific coast of Tohoku in Japan was mainly caused by the first few cycles of tsunami waves. However, the largest phase of the tsunami arriving surprisingly late in Hakodate in Hokkaido, Japan; that is, approximately 9 h after the origin time of the earthquake. It is important to understand the generation mechanism of this large later phase. The tsunami was numerically computed by solving both linear shallow water equations and non-linear shallow water equations with moving boundary conditions throughout the computational area. The later tsunami phases observed on southern Hokkaido can be much better explained by tsunami waveforms computed by solving the non-linear equations than by those computed by solving the linear equations. This suggests that the later tsunami waves arrived at the Hokkaido coast after propagating along the Pacific coast of the Tohoku region with repeated inundations far inland or reflecting from the coast of Tohoku after the inundation. The spectral analysis of the observed waveform at Hakodate tide gauge shows that the later tsunami that arrived between 7.5 and 9.5 h after the earthquake mainly contains a period of 45\u201350 min. The normal modes of Hakodate Bay were also computed to obtain the eigen periods, eigenfunctions, and spatial distribution of water heights. The computed tsunami height distributions near Hakodate and the fundamental mode of Hakodate Bay indicate that the large later phases are mainly caused by the resonance of the bay, which has a period of approximately 50 min. The results also indicate that the tsunami wave heights near the Hakodate port area, the most populated area in Hakodate, are the largest in the bay because of the resonance of the fundamental mode of the bay. The results of this study suggest that large future tsunamis might excite the fundamental mode of Hakodate Bay and cause large later phases near the Hakodate port. ", 
    "genre": "research_article", 
    "id": "sg:pub.10.1186/s40645-019-0278-x", 
    "inLanguage": [
      "en"
    ], 
    "isAccessibleForFree": false, 
    "isPartOf": [
      {
        "id": "sg:journal.1136393", 
        "issn": [
          "2197-4284"
        ], 
        "name": "Progress in Earth and Planetary Science", 
        "type": "Periodical"
      }, 
      {
        "issueNumber": "1", 
        "type": "PublicationIssue"
      }, 
      {
        "type": "PublicationVolume", 
        "volumeNumber": "6"
      }
    ], 
    "name": "Generation mechanism of large later phases of the 2011 Tohoku-oki tsunami causing damages in Hakodate, Hokkaido, Japan", 
    "pagination": "30", 
    "productId": [
      {
        "name": "readcube_id", 
        "type": "PropertyValue", 
        "value": [
          "b71e814a6075fead9c542a503569ed2d558d4a9a3604d86b9a2ae8b3250ab08e"
        ]
      }, 
      {
        "name": "doi", 
        "type": "PropertyValue", 
        "value": [
          "10.1186/s40645-019-0278-x"
        ]
      }, 
      {
        "name": "dimensions_id", 
        "type": "PropertyValue", 
        "value": [
          "pub.1113047057"
        ]
      }
    ], 
    "sameAs": [
      "https://doi.org/10.1186/s40645-019-0278-x", 
      "https://app.dimensions.ai/details/publication/pub.1113047057"
    ], 
    "sdDataset": "articles", 
    "sdDatePublished": "2019-04-11T13:19", 
    "sdLicense": "https://scigraph.springernature.com/explorer/license/", 
    "sdPublisher": {
      "name": "Springer Nature - SN SciGraph project", 
      "type": "Organization"
    }, 
    "sdSource": "s3://com-uberresearch-data-dimensions-target-20181106-alternative/cleanup/v134/2549eaecd7973599484d7c17b260dba0a4ecb94b/merge/v9/a6c9fde33151104705d4d7ff012ea9563521a3ce/jats-lookup/v90/0000000368_0000000368/records_78953_00000001.jsonl", 
    "type": "ScholarlyArticle", 
    "url": "https://link.springer.com/10.1186%2Fs40645-019-0278-x"
  }
]
 

Download the RDF metadata as:  json-ld nt turtle xml License info

HOW TO GET THIS DATA PROGRAMMATICALLY:

JSON-LD is a popular format for linked data which is fully compatible with JSON.

curl -H 'Accept: application/ld+json' 'https://scigraph.springernature.com/pub.10.1186/s40645-019-0278-x'

N-Triples is a line-based linked data format ideal for batch operations.

curl -H 'Accept: application/n-triples' 'https://scigraph.springernature.com/pub.10.1186/s40645-019-0278-x'

Turtle is a human-readable linked data format.

curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.1186/s40645-019-0278-x'

RDF/XML is a standard XML format for linked data.

curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.1186/s40645-019-0278-x'


 

This table displays all metadata directly associated to this object as RDF triples.

151 TRIPLES      21 PREDICATES      44 URIs      19 LITERALS      7 BLANK NODES

Subject Predicate Object
1 sg:pub.10.1186/s40645-019-0278-x schema:about anzsrc-for:04
2 anzsrc-for:0404
3 schema:author N4c212a35fb88438c9c2ada659ba54b95
4 schema:citation sg:pub.10.1007/s00024-006-0164-5
5 sg:pub.10.1007/s00024-012-0492-6
6 sg:pub.10.1007/s10712-006-9000-9
7 sg:pub.10.1186/bf03352676
8 sg:pub.10.5047/eps.2011.06.010
9 https://doi.org/10.1002/2017jb014749
10 https://doi.org/10.1002/jgrc.20413
11 https://doi.org/10.1016/j.epsl.2012.06.006
12 https://doi.org/10.1016/j.margeo.2014.09.043
13 https://doi.org/10.1029/2007gl032129
14 https://doi.org/10.1029/2007jc004402
15 https://doi.org/10.1029/2007jc004404
16 https://doi.org/10.1111/j.1365-246x.1988.tb03873.x
17 https://doi.org/10.1142/s0578563412500015
18 https://doi.org/10.1785/0120120122
19 https://doi.org/10.4294/jpe1952.35.409
20 https://doi.org/10.5194/adgeo-14-129-2008
21 schema:datePublished 2019-12
22 schema:datePublishedReg 2019-12-01
23 schema:description The 2011 Tohoku-oki earthquake generated a large tsunami that caused catastrophic damage along the Pacific coast of Japan. The major portion of the damage along the Pacific coast of Tohoku in Japan was mainly caused by the first few cycles of tsunami waves. However, the largest phase of the tsunami arriving surprisingly late in Hakodate in Hokkaido, Japan; that is, approximately 9 h after the origin time of the earthquake. It is important to understand the generation mechanism of this large later phase. The tsunami was numerically computed by solving both linear shallow water equations and non-linear shallow water equations with moving boundary conditions throughout the computational area. The later tsunami phases observed on southern Hokkaido can be much better explained by tsunami waveforms computed by solving the non-linear equations than by those computed by solving the linear equations. This suggests that the later tsunami waves arrived at the Hokkaido coast after propagating along the Pacific coast of the Tohoku region with repeated inundations far inland or reflecting from the coast of Tohoku after the inundation. The spectral analysis of the observed waveform at Hakodate tide gauge shows that the later tsunami that arrived between 7.5 and 9.5 h after the earthquake mainly contains a period of 45–50 min. The normal modes of Hakodate Bay were also computed to obtain the eigen periods, eigenfunctions, and spatial distribution of water heights. The computed tsunami height distributions near Hakodate and the fundamental mode of Hakodate Bay indicate that the large later phases are mainly caused by the resonance of the bay, which has a period of approximately 50 min. The results also indicate that the tsunami wave heights near the Hakodate port area, the most populated area in Hakodate, are the largest in the bay because of the resonance of the fundamental mode of the bay. The results of this study suggest that large future tsunamis might excite the fundamental mode of Hakodate Bay and cause large later phases near the Hakodate port.
24 schema:genre research_article
25 schema:inLanguage en
26 schema:isAccessibleForFree false
27 schema:isPartOf N14189ee7a57e4246ab350db583bb1938
28 N86cfbd6bffc1420caf5067d3f68ebee6
29 sg:journal.1136393
30 schema:name Generation mechanism of large later phases of the 2011 Tohoku-oki tsunami causing damages in Hakodate, Hokkaido, Japan
31 schema:pagination 30
32 schema:productId N1f7b67733c934dd6815c1d1e9b83995d
33 Nb7b108cbda9648e994a4f6091bfb0ba8
34 Nf4a2e71f416c4dccb20e322201d84c8d
35 schema:sameAs https://app.dimensions.ai/details/publication/pub.1113047057
36 https://doi.org/10.1186/s40645-019-0278-x
37 schema:sdDatePublished 2019-04-11T13:19
38 schema:sdLicense https://scigraph.springernature.com/explorer/license/
39 schema:sdPublisher N88c77f2a91c9475fb3dbbd1ffbf7c5ec
40 schema:url https://link.springer.com/10.1186%2Fs40645-019-0278-x
41 sgo:license sg:explorer/license/
42 sgo:sdDataset articles
43 rdf:type schema:ScholarlyArticle
44 N0b3f2e47697e41e29403bdf3995ffa16 rdf:first N71eef5d19b8b467ea938325f1b07f957
45 rdf:rest Nc7b7ab6719f941f699d353725b301ca6
46 N14189ee7a57e4246ab350db583bb1938 schema:volumeNumber 6
47 rdf:type schema:PublicationVolume
48 N1adb148cbcb04699ad7da6f39c559c2d schema:affiliation https://www.grid.ac/institutes/grid.208504.b
49 schema:familyName Ioki
50 schema:givenName Kei
51 rdf:type schema:Person
52 N1f7b67733c934dd6815c1d1e9b83995d schema:name readcube_id
53 schema:value b71e814a6075fead9c542a503569ed2d558d4a9a3604d86b9a2ae8b3250ab08e
54 rdf:type schema:PropertyValue
55 N4c212a35fb88438c9c2ada659ba54b95 rdf:first Nffe0b5b1d75e443aab580e78763082d9
56 rdf:rest N0b3f2e47697e41e29403bdf3995ffa16
57 N61b906b57107409bb1a020617526828e rdf:first Nf0e38aec2fb0422fab56253ea5b86140
58 rdf:rest N7963e5a4143448a1b1062859bb8e59a0
59 N71eef5d19b8b467ea938325f1b07f957 schema:affiliation https://www.grid.ac/institutes/grid.482864.4
60 schema:familyName Shibata
61 schema:givenName Mizuho
62 rdf:type schema:Person
63 N7963e5a4143448a1b1062859bb8e59a0 rdf:first N1adb148cbcb04699ad7da6f39c559c2d
64 rdf:rest rdf:nil
65 N86cfbd6bffc1420caf5067d3f68ebee6 schema:issueNumber 1
66 rdf:type schema:PublicationIssue
67 N88c77f2a91c9475fb3dbbd1ffbf7c5ec schema:name Springer Nature - SN SciGraph project
68 rdf:type schema:Organization
69 Na143c22a080f493387df26d8043d451e schema:affiliation https://www.grid.ac/institutes/grid.26999.3d
70 schema:familyName Yamanaka
71 schema:givenName Yusuke
72 rdf:type schema:Person
73 Nb7b108cbda9648e994a4f6091bfb0ba8 schema:name doi
74 schema:value 10.1186/s40645-019-0278-x
75 rdf:type schema:PropertyValue
76 Nc7b7ab6719f941f699d353725b301ca6 rdf:first Na143c22a080f493387df26d8043d451e
77 rdf:rest N61b906b57107409bb1a020617526828e
78 Nf0e38aec2fb0422fab56253ea5b86140 schema:affiliation https://www.grid.ac/institutes/grid.15638.39
79 schema:familyName Gusman
80 schema:givenName Aditya Riadi
81 rdf:type schema:Person
82 Nf4a2e71f416c4dccb20e322201d84c8d schema:name dimensions_id
83 schema:value pub.1113047057
84 rdf:type schema:PropertyValue
85 Nffe0b5b1d75e443aab580e78763082d9 schema:affiliation https://www.grid.ac/institutes/grid.39158.36
86 schema:familyName Tanioka
87 schema:givenName Yuichiro
88 rdf:type schema:Person
89 anzsrc-for:04 schema:inDefinedTermSet anzsrc-for:
90 schema:name Earth Sciences
91 rdf:type schema:DefinedTerm
92 anzsrc-for:0404 schema:inDefinedTermSet anzsrc-for:
93 schema:name Geophysics
94 rdf:type schema:DefinedTerm
95 sg:journal.1136393 schema:issn 2197-4284
96 schema:name Progress in Earth and Planetary Science
97 rdf:type schema:Periodical
98 sg:pub.10.1007/s00024-006-0164-5 schema:sameAs https://app.dimensions.ai/details/publication/pub.1041023221
99 https://doi.org/10.1007/s00024-006-0164-5
100 rdf:type schema:CreativeWork
101 sg:pub.10.1007/s00024-012-0492-6 schema:sameAs https://app.dimensions.ai/details/publication/pub.1034189369
102 https://doi.org/10.1007/s00024-012-0492-6
103 rdf:type schema:CreativeWork
104 sg:pub.10.1007/s10712-006-9000-9 schema:sameAs https://app.dimensions.ai/details/publication/pub.1037046732
105 https://doi.org/10.1007/s10712-006-9000-9
106 rdf:type schema:CreativeWork
107 sg:pub.10.1186/bf03352676 schema:sameAs https://app.dimensions.ai/details/publication/pub.1024933466
108 https://doi.org/10.1186/bf03352676
109 rdf:type schema:CreativeWork
110 sg:pub.10.5047/eps.2011.06.010 schema:sameAs https://app.dimensions.ai/details/publication/pub.1000379326
111 https://doi.org/10.5047/eps.2011.06.010
112 rdf:type schema:CreativeWork
113 https://doi.org/10.1002/2017jb014749 schema:sameAs https://app.dimensions.ai/details/publication/pub.1100110608
114 rdf:type schema:CreativeWork
115 https://doi.org/10.1002/jgrc.20413 schema:sameAs https://app.dimensions.ai/details/publication/pub.1010501342
116 rdf:type schema:CreativeWork
117 https://doi.org/10.1016/j.epsl.2012.06.006 schema:sameAs https://app.dimensions.ai/details/publication/pub.1010877998
118 rdf:type schema:CreativeWork
119 https://doi.org/10.1016/j.margeo.2014.09.043 schema:sameAs https://app.dimensions.ai/details/publication/pub.1050046481
120 rdf:type schema:CreativeWork
121 https://doi.org/10.1029/2007gl032129 schema:sameAs https://app.dimensions.ai/details/publication/pub.1043685482
122 rdf:type schema:CreativeWork
123 https://doi.org/10.1029/2007jc004402 schema:sameAs https://app.dimensions.ai/details/publication/pub.1044373747
124 rdf:type schema:CreativeWork
125 https://doi.org/10.1029/2007jc004404 schema:sameAs https://app.dimensions.ai/details/publication/pub.1049952704
126 rdf:type schema:CreativeWork
127 https://doi.org/10.1111/j.1365-246x.1988.tb03873.x schema:sameAs https://app.dimensions.ai/details/publication/pub.1052819432
128 rdf:type schema:CreativeWork
129 https://doi.org/10.1142/s0578563412500015 schema:sameAs https://app.dimensions.ai/details/publication/pub.1013244805
130 rdf:type schema:CreativeWork
131 https://doi.org/10.1785/0120120122 schema:sameAs https://app.dimensions.ai/details/publication/pub.1068471762
132 rdf:type schema:CreativeWork
133 https://doi.org/10.4294/jpe1952.35.409 schema:sameAs https://app.dimensions.ai/details/publication/pub.1003336696
134 rdf:type schema:CreativeWork
135 https://doi.org/10.5194/adgeo-14-129-2008 schema:sameAs https://app.dimensions.ai/details/publication/pub.1053014507
136 rdf:type schema:CreativeWork
137 https://www.grid.ac/institutes/grid.15638.39 schema:alternateName GNS Science
138 schema:name GNS Science, 1 Fairway Drive, Avalon, 5010, Lower Hutt, New Zealand
139 rdf:type schema:Organization
140 https://www.grid.ac/institutes/grid.208504.b schema:alternateName National Institute of Advanced Industrial Science and Technology
141 schema:name National Institute of Advanced Industrial Science and Technology, 305-8560, Tsukuba, Japan
142 rdf:type schema:Organization
143 https://www.grid.ac/institutes/grid.26999.3d schema:alternateName University of Tokyo
144 schema:name Department of Civil Engineering, The University of Tokyo, 113-8656, Tokyo, Japan
145 rdf:type schema:Organization
146 https://www.grid.ac/institutes/grid.39158.36 schema:alternateName Hokkaido University
147 schema:name Institute of Seismology and Volcanology, Faculty of Science, Hokkaido University, N10W8 Kita-ku, 060-0810, Sapporo, Hokkaido, Japan
148 rdf:type schema:Organization
149 https://www.grid.ac/institutes/grid.482864.4 schema:alternateName Central Japan Railway (Japan)
150 schema:name JR Central Japan Railway Company, 450-6101, Nagoya, Aichi, Japan
151 rdf:type schema:Organization
 




Preview window. Press ESC to close (or click here)


...