Origin of mass faulting during seismic activation in the Central Kuznetsk basin View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2011-11-19

AUTHORS

A. N. Ovsyuchenko, E. A. Rogozhin, S. S. Novikov, A. V. Marakhanov, A. S. Lar’kov

ABSTRACT

In 2005, the low magnitude shallow hypocenter swarm seismic activation occurred in the central part of Kuznetsk Depression. It continues until today. The main objects of implemented field works were numerous ruptures appearing on the surface in the vicinity of the town of Polysayevo during the activation period. In addition to chaotically distributed subsidences, slumps, and cracks related to surface saggings above worked mine fields, linear fractures of the Earth’s surface were found. These fractures form regular structural parageneses and comprise a relatively large system of 7.6 km total length. Regular structural parageneses and displacements along the faults of up to 10 cm in amplitude allow us to consider them as surface tectonic fractures. The depth of earthquake hypocenters, based on instrumental data, reaches 5 km; i.e., quakes occur significantly deeper than mine fields, which are located down to a 500 m depth. It is possible to suppose that the summarized impulse effect of seismic activation had led to formation of seismotectonic deformations in the zone of an already existing fault. The difference of the described fractures from typically seismotectonic ruptures is their gradual, slow formation. Approximate time of the start of formation for the studied fractures is several years ago, with continuous renewal up to the present. Another difference of the surface fractures is their remote positions at the distance of 1–2 km west of the epicentral area of the earthquakes swarm. More... »

PAGES

321-336

Identifiers

URI

http://scigraph.springernature.com/pub.10.3103/s0747923911040074

DOI

http://dx.doi.org/10.3103/s0747923911040074

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1018051829


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"
      }, 
      {
        "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"
      }
    ], 
    "author": [
      {
        "affiliation": {
          "alternateName": "Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, Moscow, Russia", 
          "id": "http://www.grid.ac/institutes/grid.4886.2", 
          "name": [
            "Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, 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 Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, Moscow, Russia", 
          "id": "http://www.grid.ac/institutes/grid.4886.2", 
          "name": [
            "Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, Moscow, Russia"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Rogozhin", 
        "givenName": "E. A.", 
        "id": "sg:person.013770423627.08", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.013770423627.08"
        ], 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, Moscow, Russia", 
          "id": "http://www.grid.ac/institutes/grid.4886.2", 
          "name": [
            "Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, Moscow, Russia"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Novikov", 
        "givenName": "S. S.", 
        "id": "sg:person.011425012037.76", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.011425012037.76"
        ], 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, Moscow, Russia", 
          "id": "http://www.grid.ac/institutes/grid.4886.2", 
          "name": [
            "Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, Moscow, Russia"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Marakhanov", 
        "givenName": "A. V.", 
        "id": "sg:person.012416632715.99", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.012416632715.99"
        ], 
        "type": "Person"
      }, 
      {
        "affiliation": {
          "alternateName": "Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, Moscow, Russia", 
          "id": "http://www.grid.ac/institutes/grid.4886.2", 
          "name": [
            "Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol\u2019shaya Gruzinskaya ul. 10, 123995, Moscow, Russia"
          ], 
          "type": "Organization"
        }, 
        "familyName": "Lar\u2019kov", 
        "givenName": "A. S.", 
        "id": "sg:person.013462672555.04", 
        "sameAs": [
          "https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.013462672555.04"
        ], 
        "type": "Person"
      }
    ], 
    "citation": [
      {
        "id": "sg:pub.10.1134/s0016852109060016", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1043399135", 
          "https://doi.org/10.1134/s0016852109060016"
        ], 
        "type": "CreativeWork"
      }, 
      {
        "id": "sg:pub.10.1134/s001685210702001x", 
        "sameAs": [
          "https://app.dimensions.ai/details/publication/pub.1020002802", 
          "https://doi.org/10.1134/s001685210702001x"
        ], 
        "type": "CreativeWork"
      }
    ], 
    "datePublished": "2011-11-19", 
    "datePublishedReg": "2011-11-19", 
    "description": "In 2005, the low magnitude shallow hypocenter swarm seismic activation occurred in the central part of Kuznetsk Depression. It continues until today. The main objects of implemented field works were numerous ruptures appearing on the surface in the vicinity of the town of Polysayevo during the activation period. In addition to chaotically distributed subsidences, slumps, and cracks related to surface saggings above worked mine fields, linear fractures of the Earth\u2019s surface were found. These fractures form regular structural parageneses and comprise a relatively large system of 7.6 km total length. Regular structural parageneses and displacements along the faults of up to 10 cm in amplitude allow us to consider them as surface tectonic fractures. The depth of earthquake hypocenters, based on instrumental data, reaches 5 km; i.e., quakes occur significantly deeper than mine fields, which are located down to a 500 m depth. It is possible to suppose that the summarized impulse effect of seismic activation had led to formation of seismotectonic deformations in the zone of an already existing fault. The difference of the described fractures from typically seismotectonic ruptures is their gradual, slow formation. Approximate time of the start of formation for the studied fractures is several years ago, with continuous renewal up to the present. Another difference of the surface fractures is their remote positions at the distance of 1\u20132 km west of the epicentral area of the earthquakes swarm.", 
    "genre": "article", 
    "id": "sg:pub.10.3103/s0747923911040074", 
    "inLanguage": "en", 
    "isAccessibleForFree": false, 
    "isPartOf": [
      {
        "id": "sg:journal.1136303", 
        "issn": [
          "0747-9239", 
          "1934-7871"
        ], 
        "name": "Seismic Instruments", 
        "publisher": "Allerton Press", 
        "type": "Periodical"
      }, 
      {
        "issueNumber": "4", 
        "type": "PublicationIssue"
      }, 
      {
        "type": "PublicationVolume", 
        "volumeNumber": "47"
      }
    ], 
    "keywords": [
      "seismic activation", 
      "structural parageneses", 
      "seismotectonic deformations", 
      "earthquake hypocenters", 
      "tectonic fractures", 
      "earthquake swarm", 
      "epicentral area", 
      "instrumental data", 
      "Kuznetsk Basin", 
      "Earth's surface", 
      "central part", 
      "Kuznetsk Depression", 
      "numerous ruptures", 
      "mine field", 
      "start of formation", 
      "surface fracture", 
      "parageneses", 
      "field work", 
      "approximate time", 
      "faults", 
      "depth", 
      "linear fracture", 
      "faulting", 
      "hypocenters", 
      "basin", 
      "subsidence", 
      "quake", 
      "slump", 
      "zone", 
      "swarm", 
      "formation", 
      "fractures", 
      "surface", 
      "sagging", 
      "rupture", 
      "deformation", 
      "vicinity", 
      "remote position", 
      "origin", 
      "area", 
      "total length", 
      "displacement", 
      "town", 
      "part", 
      "present", 
      "field", 
      "period", 
      "amplitude", 
      "main object", 
      "data", 
      "today", 
      "renewal", 
      "years", 
      "distance", 
      "cracks", 
      "slow formation", 
      "depression", 
      "differences", 
      "time", 
      "continuous renewal", 
      "activation period", 
      "position", 
      "large systems", 
      "start", 
      "system", 
      "addition", 
      "length", 
      "work", 
      "effect", 
      "impulse effects", 
      "objects", 
      "activation", 
      "low magnitude shallow hypocenter swarm seismic activation", 
      "magnitude shallow hypocenter swarm seismic activation", 
      "shallow hypocenter swarm seismic activation", 
      "hypocenter swarm seismic activation", 
      "swarm seismic activation", 
      "town of Polysayevo", 
      "Polysayevo", 
      "surface saggings", 
      "regular structural parageneses", 
      "surface tectonic fractures", 
      "seismotectonic ruptures", 
      "mass faulting", 
      "Central Kuznetsk basin"
    ], 
    "name": "Origin of mass faulting during seismic activation in the Central Kuznetsk basin", 
    "pagination": "321-336", 
    "productId": [
      {
        "name": "dimensions_id", 
        "type": "PropertyValue", 
        "value": [
          "pub.1018051829"
        ]
      }, 
      {
        "name": "doi", 
        "type": "PropertyValue", 
        "value": [
          "10.3103/s0747923911040074"
        ]
      }
    ], 
    "sameAs": [
      "https://doi.org/10.3103/s0747923911040074", 
      "https://app.dimensions.ai/details/publication/pub.1018051829"
    ], 
    "sdDataset": "articles", 
    "sdDatePublished": "2021-11-01T18:17", 
    "sdLicense": "https://scigraph.springernature.com/explorer/license/", 
    "sdPublisher": {
      "name": "Springer Nature - SN SciGraph project", 
      "type": "Organization"
    }, 
    "sdSource": "s3://com-springernature-scigraph/baseset/20211101/entities/gbq_results/article/article_542.jsonl", 
    "type": "ScholarlyArticle", 
    "url": "https://doi.org/10.3103/s0747923911040074"
  }
]
 

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/s0747923911040074'

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/s0747923911040074'

Turtle is a human-readable linked data format.

curl -H 'Accept: text/turtle' 'https://scigraph.springernature.com/pub.10.3103/s0747923911040074'

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

curl -H 'Accept: application/rdf+xml' 'https://scigraph.springernature.com/pub.10.3103/s0747923911040074'


 

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

183 TRIPLES      22 PREDICATES      113 URIs      102 LITERALS      6 BLANK NODES

Subject Predicate Object
1 sg:pub.10.3103/s0747923911040074 schema:about anzsrc-for:04
2 anzsrc-for:0403
3 anzsrc-for:0404
4 schema:author Ne247e068a86d4fba9f356c73736f667a
5 schema:citation sg:pub.10.1134/s001685210702001x
6 sg:pub.10.1134/s0016852109060016
7 schema:datePublished 2011-11-19
8 schema:datePublishedReg 2011-11-19
9 schema:description In 2005, the low magnitude shallow hypocenter swarm seismic activation occurred in the central part of Kuznetsk Depression. It continues until today. The main objects of implemented field works were numerous ruptures appearing on the surface in the vicinity of the town of Polysayevo during the activation period. In addition to chaotically distributed subsidences, slumps, and cracks related to surface saggings above worked mine fields, linear fractures of the Earth’s surface were found. These fractures form regular structural parageneses and comprise a relatively large system of 7.6 km total length. Regular structural parageneses and displacements along the faults of up to 10 cm in amplitude allow us to consider them as surface tectonic fractures. The depth of earthquake hypocenters, based on instrumental data, reaches 5 km; i.e., quakes occur significantly deeper than mine fields, which are located down to a 500 m depth. It is possible to suppose that the summarized impulse effect of seismic activation had led to formation of seismotectonic deformations in the zone of an already existing fault. The difference of the described fractures from typically seismotectonic ruptures is their gradual, slow formation. Approximate time of the start of formation for the studied fractures is several years ago, with continuous renewal up to the present. Another difference of the surface fractures is their remote positions at the distance of 1–2 km west of the epicentral area of the earthquakes swarm.
10 schema:genre article
11 schema:inLanguage en
12 schema:isAccessibleForFree false
13 schema:isPartOf N93d769b1a03e4405b84cbc1debb1283b
14 Ne10b4c80b04646d89ccb56a96e75403a
15 sg:journal.1136303
16 schema:keywords Central Kuznetsk basin
17 Earth's surface
18 Kuznetsk Basin
19 Kuznetsk Depression
20 Polysayevo
21 activation
22 activation period
23 addition
24 amplitude
25 approximate time
26 area
27 basin
28 central part
29 continuous renewal
30 cracks
31 data
32 deformation
33 depression
34 depth
35 differences
36 displacement
37 distance
38 earthquake hypocenters
39 earthquake swarm
40 effect
41 epicentral area
42 faulting
43 faults
44 field
45 field work
46 formation
47 fractures
48 hypocenter swarm seismic activation
49 hypocenters
50 impulse effects
51 instrumental data
52 large systems
53 length
54 linear fracture
55 low magnitude shallow hypocenter swarm seismic activation
56 magnitude shallow hypocenter swarm seismic activation
57 main object
58 mass faulting
59 mine field
60 numerous ruptures
61 objects
62 origin
63 parageneses
64 part
65 period
66 position
67 present
68 quake
69 regular structural parageneses
70 remote position
71 renewal
72 rupture
73 sagging
74 seismic activation
75 seismotectonic deformations
76 seismotectonic ruptures
77 shallow hypocenter swarm seismic activation
78 slow formation
79 slump
80 start
81 start of formation
82 structural parageneses
83 subsidence
84 surface
85 surface fracture
86 surface saggings
87 surface tectonic fractures
88 swarm
89 swarm seismic activation
90 system
91 tectonic fractures
92 time
93 today
94 total length
95 town
96 town of Polysayevo
97 vicinity
98 work
99 years
100 zone
101 schema:name Origin of mass faulting during seismic activation in the Central Kuznetsk basin
102 schema:pagination 321-336
103 schema:productId N579382eb180a4cf98246ab4eb9c43c56
104 N73ed46d4d4fd46e3ab32a11d52fbcaf4
105 schema:sameAs https://app.dimensions.ai/details/publication/pub.1018051829
106 https://doi.org/10.3103/s0747923911040074
107 schema:sdDatePublished 2021-11-01T18:17
108 schema:sdLicense https://scigraph.springernature.com/explorer/license/
109 schema:sdPublisher Nd21d46988f654b66905bf9e0b91c9001
110 schema:url https://doi.org/10.3103/s0747923911040074
111 sgo:license sg:explorer/license/
112 sgo:sdDataset articles
113 rdf:type schema:ScholarlyArticle
114 N1b894631cdbb4a598b124e367d757bac rdf:first sg:person.013462672555.04
115 rdf:rest rdf:nil
116 N533e6e2c4be34b81925ba904549aac01 rdf:first sg:person.011425012037.76
117 rdf:rest N8796d839e53b42f5a6b502165b27d637
118 N579382eb180a4cf98246ab4eb9c43c56 schema:name dimensions_id
119 schema:value pub.1018051829
120 rdf:type schema:PropertyValue
121 N73ed46d4d4fd46e3ab32a11d52fbcaf4 schema:name doi
122 schema:value 10.3103/s0747923911040074
123 rdf:type schema:PropertyValue
124 N8796d839e53b42f5a6b502165b27d637 rdf:first sg:person.012416632715.99
125 rdf:rest N1b894631cdbb4a598b124e367d757bac
126 N93d769b1a03e4405b84cbc1debb1283b schema:volumeNumber 47
127 rdf:type schema:PublicationVolume
128 N9f97a861ae904426a671f58b7e3fba7e rdf:first sg:person.013770423627.08
129 rdf:rest N533e6e2c4be34b81925ba904549aac01
130 Nd21d46988f654b66905bf9e0b91c9001 schema:name Springer Nature - SN SciGraph project
131 rdf:type schema:Organization
132 Ne10b4c80b04646d89ccb56a96e75403a schema:issueNumber 4
133 rdf:type schema:PublicationIssue
134 Ne247e068a86d4fba9f356c73736f667a rdf:first sg:person.015007520355.17
135 rdf:rest N9f97a861ae904426a671f58b7e3fba7e
136 anzsrc-for:04 schema:inDefinedTermSet anzsrc-for:
137 schema:name Earth Sciences
138 rdf:type schema:DefinedTerm
139 anzsrc-for:0403 schema:inDefinedTermSet anzsrc-for:
140 schema:name Geology
141 rdf:type schema:DefinedTerm
142 anzsrc-for:0404 schema:inDefinedTermSet anzsrc-for:
143 schema:name Geophysics
144 rdf:type schema:DefinedTerm
145 sg:journal.1136303 schema:issn 0747-9239
146 1934-7871
147 schema:name Seismic Instruments
148 schema:publisher Allerton Press
149 rdf:type schema:Periodical
150 sg:person.011425012037.76 schema:affiliation grid-institutes:grid.4886.2
151 schema:familyName Novikov
152 schema:givenName S. S.
153 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.011425012037.76
154 rdf:type schema:Person
155 sg:person.012416632715.99 schema:affiliation grid-institutes:grid.4886.2
156 schema:familyName Marakhanov
157 schema:givenName A. V.
158 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.012416632715.99
159 rdf:type schema:Person
160 sg:person.013462672555.04 schema:affiliation grid-institutes:grid.4886.2
161 schema:familyName Lar’kov
162 schema:givenName A. S.
163 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.013462672555.04
164 rdf:type schema:Person
165 sg:person.013770423627.08 schema:affiliation grid-institutes:grid.4886.2
166 schema:familyName Rogozhin
167 schema:givenName E. A.
168 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.013770423627.08
169 rdf:type schema:Person
170 sg:person.015007520355.17 schema:affiliation grid-institutes:grid.4886.2
171 schema:familyName Ovsyuchenko
172 schema:givenName A. N.
173 schema:sameAs https://app.dimensions.ai/discover/publication?and_facet_researcher=ur.015007520355.17
174 rdf:type schema:Person
175 sg:pub.10.1134/s001685210702001x schema:sameAs https://app.dimensions.ai/details/publication/pub.1020002802
176 https://doi.org/10.1134/s001685210702001x
177 rdf:type schema:CreativeWork
178 sg:pub.10.1134/s0016852109060016 schema:sameAs https://app.dimensions.ai/details/publication/pub.1043399135
179 https://doi.org/10.1134/s0016852109060016
180 rdf:type schema:CreativeWork
181 grid-institutes:grid.4886.2 schema:alternateName Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol’shaya Gruzinskaya ul. 10, 123995, Moscow, Russia
182 schema:name Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Bol’shaya Gruzinskaya ul. 10, 123995, Moscow, Russia
183 rdf:type schema:Organization
 




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


...