Geological and macroseismic effects of the Muya, 1957 earthquake and palaeoearthquakes in Baikal region View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2010-03

AUTHORS

R. E. Tatevossian, N. G. Mokrushina, A. N. Ovsyuchenko, T. N. Tatevossian

ABSTRACT

Intensity of the Muya, 1957 earthquake is assessed in localities based on macroseismic data and in epicentral area based on effects in natural environment; it is analyzed how these assessments correspond to each other and to instrumental location of epicenter, hypocentral depth, and magnitude; it is evaluated, how seismodislocations of the Muya earthquake could serve as control of palaeoseismostructure parameters in this region. Spatial distribution of macroseismic effect confirms relatively deep source (20–22 km). Deep source agrees with anomalously short surface rupture length (not more than 25 km); only a part of the source exposed on the surface. Comparison with length of palaeoseismostructures shows that it is a regional feature. Epicentral intensity based on surface ruptures is assed X degrees in ESI2007 scale. Ignoring geological effects will underestimate epicentral intensity up to two degrees. Source mechanism with three sub-sources is in agreement with segmentation of surface ruptures. Sub-sources are of strike-slip type with small normal component; essential normal slip at surface is probably not representative for the source and is due to accommodation of strike-slip movement along with a system of sub-parallel en echelon ruptures under tension. More... »

PAGES

152-176

Identifiers

URI

http://scigraph.springernature.com/pub.10.3103/s0747923910020052

DOI

http://dx.doi.org/10.3103/s0747923910020052

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1006002132


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/2008/04", 
        "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
        "name": "Earth Sciences", 
        "type": "DefinedTerm"
      }, 
      {
        "id": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/0403", 
        "inDefinedTermSet": "http://purl.org/au-research/vocabulary/anzsrc-for/2008/", 
        "name": "Geology", 
        "type": "DefinedTerm"
      }
    ], 
    "author": [
      {
        "affiliation": {
          "alternateName": "Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia", 
          "id": "http://www.grid.ac/institutes/grid.435352.6", 
          "name": [
            "Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Tatevossian", 
        "givenName": "R. E.", 
        "id": "sg:person.013756060501.11", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.013756060501.11"
        ], 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia", 
          "id": "http://www.grid.ac/institutes/grid.435352.6", 
          "name": [
            "Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Mokrushina", 
        "givenName": "N. G.", 
        "id": "sg:person.015261773556.83", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.015261773556.83"
        ], 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia", 
          "id": "http://www.grid.ac/institutes/grid.435352.6", 
          "name": [
            "Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Ovsyuchenko", 
        "givenName": "A. N.", 
        "id": "sg:person.015007520355.17", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.015007520355.17"
        ], 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia", 
          "id": "http://www.grid.ac/institutes/grid.435352.6", 
          "name": [
            "Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Tatevossian", 
        "givenName": "T. N.", 
        "id": "sg:person.07750171551.38", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.07750171551.38"
        ], 
        "type": "Person"
      }
    ], 
    "datePublished": "2010-03", 
    "datePublishedReg": "2010-03-01", 
    "description": "Intensity of the Muya, 1957 earthquake is assessed in localities based on macroseismic data and in epicentral area based on effects in natural environment; it is analyzed how these assessments correspond to each other and to instrumental location of epicenter, hypocentral depth, and magnitude; it is evaluated, how seismodislocations of the Muya earthquake could serve as control of palaeoseismostructure parameters in this region. Spatial distribution of macroseismic effect confirms relatively deep source (20\u201322 km). Deep source agrees with anomalously short surface rupture length (not more than 25 km); only a part of the source exposed on the surface. Comparison with length of palaeoseismostructures shows that it is a regional feature. Epicentral intensity based on surface ruptures is assed X degrees in ESI2007 scale. Ignoring geological effects will underestimate epicentral intensity up to two degrees. Source mechanism with three sub-sources is in agreement with segmentation of surface ruptures. Sub-sources are of strike-slip type with small normal component; essential normal slip at surface is probably not representative for the source and is due to accommodation of strike-slip movement along with a system of sub-parallel en echelon ruptures under tension.", 
    "genre": "article", 
    "id": "sg:pub.10.3103/s0747923910020052", 
    "inLanguage": "en", 
    "isAccessibleForFree": false, 
    "isPartOf": [
      {
        "id": "sg:journal.1136303", 
        "issn": [
          "0747-9239", 
          "1934-7871"
        ], 
        "name": "Seismic Instruments", 
        "publisher": "Allerton Press", 
        "type": "Periodical"
      }, 
      {
        "issueNumber": "2", 
        "type": "PublicationIssue"
      }, 
      {
        "type": "PublicationVolume", 
        "volumeNumber": "46"
      }
    ], 
    "keywords": [
      "surface rupture", 
      "deep source", 
      "macroseismic effects", 
      "epicentral intensity", 
      "strike-slip movement", 
      "strike-slip type", 
      "surface rupture length", 
      "small normal component", 
      "instrumental locations", 
      "normal slip", 
      "hypocentral depth", 
      "rupture length", 
      "geological effects", 
      "epicentral area", 
      "macroseismic data", 
      "source mechanism", 
      "Baikal region", 
      "regional features", 
      "earthquakes", 
      "spatial distribution", 
      "palaeoearthquakes", 
      "source", 
      "epicenter", 
      "natural environment", 
      "slip", 
      "depth", 
      "region", 
      "localities", 
      "rupture", 
      "normal component", 
      "echelons", 
      "surface", 
      "intensity", 
      "area", 
      "magnitude", 
      "scale", 
      "location", 
      "part", 
      "distribution", 
      "environment", 
      "movement", 
      "data", 
      "features", 
      "accommodation", 
      "degree", 
      "agreement", 
      "components", 
      "comparison", 
      "assessment", 
      "parameters", 
      "types", 
      "system", 
      "length", 
      "effect", 
      "mechanism", 
      "segmentation", 
      "control", 
      "tension", 
      "seismodislocations", 
      "Muya earthquake", 
      "palaeoseismostructure parameters", 
      "short surface rupture length", 
      "length of palaeoseismostructures", 
      "palaeoseismostructures", 
      "ESI2007 scale", 
      "essential normal slip"
    ], 
    "name": "Geological and macroseismic effects of the Muya, 1957 earthquake and palaeoearthquakes in Baikal region", 
    "pagination": "152-176", 
    "productId": [
      {
        "name": "dimensions_id", 
        "type": "PropertyValue", 
        "value": [
          "pub.1006002132"
        ]
      }, 
      {
        "name": "doi", 
        "type": "PropertyValue", 
        "value": [
          "10.3103/s0747923910020052"
        ]
      }
    ], 
    "sameAs": [
      "https://doi.org/10.3103/s0747923910020052", 
      "https://app.dimensions.ai/details/publication/pub.1006002132"
    ], 
    "sdDataset": "articles", 
    "sdDatePublished": "2022-01-01T18:22", 
    "sdLicense": "https://scigraph.springernature.com/explorer/license/", 
    "sdPublisher": {
      "name": "Springer Nature - SN SciGraph project", 
      "type": "Organization"
    }, 
    "sdSource": "s3://com-springernature-scigraph/baseset/20220101/entities/gbq_results/article/article_522.jsonl", 
    "type": "ScholarlyArticle", 
    "url": "https://doi.org/10.3103/s0747923910020052"
  }
]
 

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.10.3103/s0747923910020052'

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

curl -H 'Accept: application/n-triples' 'https://scigraph.springernature.com/pub.10.3103/s0747923910020052'

Turtle is a human-readable linked data format.

curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.3103/s0747923910020052'

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

curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.3103/s0747923910020052'


 

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

145 TRIPLES      21 PREDICATES      92 URIs      84 LITERALS      6 BLANK NODES

Subject Predicate Object
1 sg:pub.10.3103/s0747923910020052 schema:about anzsrc-for:04
2 anzsrc-for:0403
3 schema:author N85a5c07d278a442ab0c3f21f0e49d33d
4 schema:datePublished 2010-03
5 schema:datePublishedReg 2010-03-01
6 schema:description Intensity of the Muya, 1957 earthquake is assessed in localities based on macroseismic data and in epicentral area based on effects in natural environment; it is analyzed how these assessments correspond to each other and to instrumental location of epicenter, hypocentral depth, and magnitude; it is evaluated, how seismodislocations of the Muya earthquake could serve as control of palaeoseismostructure parameters in this region. Spatial distribution of macroseismic effect confirms relatively deep source (20–22 km). Deep source agrees with anomalously short surface rupture length (not more than 25 km); only a part of the source exposed on the surface. Comparison with length of palaeoseismostructures shows that it is a regional feature. Epicentral intensity based on surface ruptures is assed X degrees in ESI2007 scale. Ignoring geological effects will underestimate epicentral intensity up to two degrees. Source mechanism with three sub-sources is in agreement with segmentation of surface ruptures. Sub-sources are of strike-slip type with small normal component; essential normal slip at surface is probably not representative for the source and is due to accommodation of strike-slip movement along with a system of sub-parallel en echelon ruptures under tension.
7 schema:genre article
8 schema:inLanguage en
9 schema:isAccessibleForFree false
10 schema:isPartOf N50ce0fe356114f4891b10f76f0431b0b
11 Na4b3de78a8bf49888429812cb4db0902
12 sg:journal.1136303
13 schema:keywords Baikal region
14 ESI2007 scale
15 Muya earthquake
16 accommodation
17 agreement
18 area
19 assessment
20 comparison
21 components
22 control
23 data
24 deep source
25 degree
26 depth
27 distribution
28 earthquakes
29 echelons
30 effect
31 environment
32 epicenter
33 epicentral area
34 epicentral intensity
35 essential normal slip
36 features
37 geological effects
38 hypocentral depth
39 instrumental locations
40 intensity
41 length
42 length of palaeoseismostructures
43 localities
44 location
45 macroseismic data
46 macroseismic effects
47 magnitude
48 mechanism
49 movement
50 natural environment
51 normal component
52 normal slip
53 palaeoearthquakes
54 palaeoseismostructure parameters
55 palaeoseismostructures
56 parameters
57 part
58 region
59 regional features
60 rupture
61 rupture length
62 scale
63 segmentation
64 seismodislocations
65 short surface rupture length
66 slip
67 small normal component
68 source
69 source mechanism
70 spatial distribution
71 strike-slip movement
72 strike-slip type
73 surface
74 surface rupture
75 surface rupture length
76 system
77 tension
78 types
79 schema:name Geological and macroseismic effects of the Muya, 1957 earthquake and palaeoearthquakes in Baikal region
80 schema:pagination 152-176
81 schema:productId N1b515294de394aaf8cc600f36ff37b58
82 N8983c56515f749c2be83cbdbb7a31628
83 schema:sameAs https://app.dimensions.ai/details/publication/pub.1006002132
84 https://doi.org/10.3103/s0747923910020052
85 schema:sdDatePublished 2022-01-01T18:22
86 schema:sdLicense https://scigraph.springernature.com/explorer/license/
87 schema:sdPublisher N2cac345cd23240019f14384a0bc296e0
88 schema:url https://doi.org/10.3103/s0747923910020052
89 sgo:license sg:explorer/license/
90 sgo:sdDataset articles
91 rdf:type schema:ScholarlyArticle
92 N1b515294de394aaf8cc600f36ff37b58 schema:name dimensions_id
93 schema:value pub.1006002132
94 rdf:type schema:PropertyValue
95 N1d18bb0f8ff2491191f45bec24727505 rdf:first sg:person.015261773556.83
96 rdf:rest N46ea2a70b55f4a0c96932ceae75e0226
97 N2cac345cd23240019f14384a0bc296e0 schema:name Springer Nature - SN SciGraph project
98 rdf:type schema:Organization
99 N46ea2a70b55f4a0c96932ceae75e0226 rdf:first sg:person.015007520355.17
100 rdf:rest Nbf692c55209440c687df5c3f367bbb6b
101 N50ce0fe356114f4891b10f76f0431b0b schema:issueNumber 2
102 rdf:type schema:PublicationIssue
103 N85a5c07d278a442ab0c3f21f0e49d33d rdf:first sg:person.013756060501.11
104 rdf:rest N1d18bb0f8ff2491191f45bec24727505
105 N8983c56515f749c2be83cbdbb7a31628 schema:name doi
106 schema:value 10.3103/s0747923910020052
107 rdf:type schema:PropertyValue
108 Na4b3de78a8bf49888429812cb4db0902 schema:volumeNumber 46
109 rdf:type schema:PublicationVolume
110 Nbf692c55209440c687df5c3f367bbb6b rdf:first sg:person.07750171551.38
111 rdf:rest rdf:nil
112 anzsrc-for:04 schema:inDefinedTermSet anzsrc-for:
113 schema:name Earth Sciences
114 rdf:type schema:DefinedTerm
115 anzsrc-for:0403 schema:inDefinedTermSet anzsrc-for:
116 schema:name Geology
117 rdf:type schema:DefinedTerm
118 sg:journal.1136303 schema:issn 0747-9239
119 1934-7871
120 schema:name Seismic Instruments
121 schema:publisher Allerton Press
122 rdf:type schema:Periodical
123 sg:person.013756060501.11 schema:affiliation grid-institutes:grid.435352.6
124 schema:familyName Tatevossian
125 schema:givenName R. E.
126 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.013756060501.11
127 rdf:type schema:Person
128 sg:person.015007520355.17 schema:affiliation grid-institutes:grid.435352.6
129 schema:familyName Ovsyuchenko
130 schema:givenName A. N.
131 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.015007520355.17
132 rdf:type schema:Person
133 sg:person.015261773556.83 schema:affiliation grid-institutes:grid.435352.6
134 schema:familyName Mokrushina
135 schema:givenName N. G.
136 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.015261773556.83
137 rdf:type schema:Person
138 sg:person.07750171551.38 schema:affiliation grid-institutes:grid.435352.6
139 schema:familyName Tatevossian
140 schema:givenName T. N.
141 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.07750171551.38
142 rdf:type schema:Person
143 grid-institutes:grid.435352.6 schema:alternateName Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia
144 schema:name Schmidt Institute of the Physics of the Earth, RAS, Moscow, Russia
145 rdf:type schema:Organization
 




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


...