Changes
On November 30, 2024 at 3:50:30 PM UTC, admin:
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Moved Physical property distribution and fracture density of a ~700 m-deep borehole penetrated through the Futagawa fault ruptured during the 2016 Kumamoto earthquake mainshock from organization PANGAEA (Geophysics) to organization PANGAEA (Lithosphere)
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Removed tag P-wave velocity from Physical property distribution and fracture density of a ~700 m-deep borehole penetrated through the Futagawa fault ruptured during the 2016 Kumamoto earthquake mainshock
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Added tag wave velocity to Physical property distribution and fracture density of a ~700 m-deep borehole penetrated through the Futagawa fault ruptured during the 2016 Kumamoto earthquake mainshock
f | 1 | { | f | 1 | { |
2 | "author": "Shibutani, Susumu", | 2 | "author": "Shibutani, Susumu", | ||
3 | "author_email": "", | 3 | "author_email": "", | ||
4 | "citation": [], | 4 | "citation": [], | ||
5 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | 5 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | ||
6 | "doi": "10.1594/PANGAEA.933472", | 6 | "doi": "10.1594/PANGAEA.933472", | ||
7 | "doi_date_published": "2021", | 7 | "doi_date_published": "2021", | ||
8 | "doi_publisher": "", | 8 | "doi_publisher": "", | ||
9 | "doi_status": "True", | 9 | "doi_status": "True", | ||
10 | "extra_authors": [ | 10 | "extra_authors": [ | ||
11 | { | 11 | { | ||
12 | "extra_author": "Lin, Weiren", | 12 | "extra_author": "Lin, Weiren", | ||
13 | "familyName": "Lin", | 13 | "familyName": "Lin", | ||
14 | "givenName": "Weiren", | 14 | "givenName": "Weiren", | ||
15 | "orcid": "0000-0003-3228-2789" | 15 | "orcid": "0000-0003-3228-2789" | ||
16 | } | 16 | } | ||
17 | ], | 17 | ], | ||
18 | "familyName": "Shibutani", | 18 | "familyName": "Shibutani", | ||
19 | "givenName": "Susumu", | 19 | "givenName": "Susumu", | ||
20 | "groups": [], | 20 | "groups": [], | ||
21 | "id": "ae39e3a8-4625-4bc1-9d92-2117e0e8a91e", | 21 | "id": "ae39e3a8-4625-4bc1-9d92-2117e0e8a91e", | ||
22 | "isopen": false, | 22 | "isopen": false, | ||
23 | "license_id": "CC-BY-4.0", | 23 | "license_id": "CC-BY-4.0", | ||
24 | "license_title": "CC-BY-4.0", | 24 | "license_title": "CC-BY-4.0", | ||
25 | "metadata_created": "2024-11-29T10:31:03.407490", | 25 | "metadata_created": "2024-11-29T10:31:03.407490", | ||
n | 26 | "metadata_modified": "2024-11-29T10:31:03.407496", | n | 26 | "metadata_modified": "2024-11-30T15:50:30.075585", |
27 | "name": "png-doi-10-1594-pangaea-933472", | 27 | "name": "png-doi-10-1594-pangaea-933472", | ||
28 | "notes": "To reveal depth distribution of physical properties and | 28 | "notes": "To reveal depth distribution of physical properties and | ||
29 | fracture density in a seismic fault drilling borehole called FDB-1, | 29 | fracture density in a seismic fault drilling borehole called FDB-1, | ||
30 | wireline log data and core descriptions were analyzed. The borehole | 30 | wireline log data and core descriptions were analyzed. The borehole | ||
31 | was penetrated through the Futagawa fault ruptured during the 2016 | 31 | was penetrated through the Futagawa fault ruptured during the 2016 | ||
32 | Kumamoto earthquake mainshock. Its location is in the active Aso | 32 | Kumamoto earthquake mainshock. Its location is in the active Aso | ||
33 | volcanic region, SW Japan. The borehole drilling and data acquisition | 33 | volcanic region, SW Japan. The borehole drilling and data acquisition | ||
34 | were conducted in 2017\u20132018, ~1.5 years after the earthquake, by | 34 | were conducted in 2017\u20132018, ~1.5 years after the earthquake, by | ||
35 | a consignment project conducted by Kyoto University, Japan funded by | 35 | a consignment project conducted by Kyoto University, Japan funded by | ||
36 | the Nuclear Regulation Authority, Japan. The log data and the core | 36 | the Nuclear Regulation Authority, Japan. The log data and the core | ||
37 | descriptions used for fracture density analyses were originally | 37 | descriptions used for fracture density analyses were originally | ||
38 | summarized in a free-access report in Japanese by Kyoto University in | 38 | summarized in a free-access report in Japanese by Kyoto University in | ||
39 | 2018 (https://www.nsr.go.jp/data/000256426.pdf). The data sets consist | 39 | 2018 (https://www.nsr.go.jp/data/000256426.pdf). The data sets consist | ||
40 | of (i) log data including borehole diameter, temperature, gamma ray, | 40 | of (i) log data including borehole diameter, temperature, gamma ray, | ||
41 | spontaneous potential, resistivity, P-wave velocity obtained by | 41 | spontaneous potential, resistivity, P-wave velocity obtained by | ||
42 | downhole borehole logging; (ii) depth and dip angle categories of all | 42 | downhole borehole logging; (ii) depth and dip angle categories of all | ||
43 | fractures observed from drill core samples, (iii) fracture density for | 43 | fractures observed from drill core samples, (iii) fracture density for | ||
44 | each dip angle category in each one-meter intervals from 302 m to 666 | 44 | each dip angle category in each one-meter intervals from 302 m to 666 | ||
45 | m; (iv) dip angle and downdip azimuth of fractures from borehole | 45 | m; (iv) dip angle and downdip azimuth of fractures from borehole | ||
46 | televiewer images. \\n\\nAll the data was obtained from the same depth | 46 | televiewer images. \\n\\nAll the data was obtained from the same depth | ||
47 | interval from ~302 m to ~666 m in the vertical borehole FDB-1, where | 47 | interval from ~302 m to ~666 m in the vertical borehole FDB-1, where | ||
48 | core samples were retrieved, and wireline downhole geophysical logs | 48 | core samples were retrieved, and wireline downhole geophysical logs | ||
49 | were conducted. The conventional log operations providing (i) log data | 49 | were conducted. The conventional log operations providing (i) log data | ||
50 | were carried out by Geophysical Surveying Co., Ltd. | 50 | were carried out by Geophysical Surveying Co., Ltd. | ||
51 | (https://www.gsct.co.jp/). Digital log data were sampled at an | 51 | (https://www.gsct.co.jp/). Digital log data were sampled at an | ||
52 | interval of 10 cm. All fractures were macroscopically identified by | 52 | interval of 10 cm. All fractures were macroscopically identified by | ||
53 | core description, and (ii) number of fractures, depth and their dip | 53 | core description, and (ii) number of fractures, depth and their dip | ||
54 | angle categories were recorded. The categories were defined as L, M, | 54 | angle categories were recorded. The categories were defined as L, M, | ||
55 | and H indicating fracture dip angles; \u201cL\u201d means <30\u00b0 | 55 | and H indicating fracture dip angles; \u201cL\u201d means <30\u00b0 | ||
56 | from the horizontal plane; \u201cM\u201d: \u226530\u00b0 and | 56 | from the horizontal plane; \u201cM\u201d: \u226530\u00b0 and | ||
57 | <60\u00b0; \u201cH\u201d: \u226560\u00b0. Therefore, (iii) fracture | 57 | <60\u00b0; \u201cH\u201d: \u226560\u00b0. Therefore, (iii) fracture | ||
58 | density for each dip angle category in each one-meter intervals were | 58 | density for each dip angle category in each one-meter intervals were | ||
59 | calculated using (ii) numbers of fracture. In addition, (iv) fractures | 59 | calculated using (ii) numbers of fracture. In addition, (iv) fractures | ||
60 | were also identified from borehole televiewer images, and fracture | 60 | were also identified from borehole televiewer images, and fracture | ||
61 | density was calculated. Dip angles and downdip azimuth of all the | 61 | density was calculated. Dip angles and downdip azimuth of all the | ||
62 | fractures observed from the borehole images were obtained by curve | 62 | fractures observed from the borehole images were obtained by curve | ||
63 | fitting using a trigonometric function. It should be added that the | 63 | fitting using a trigonometric function. It should be added that the | ||
64 | numbers of fractures observed from core samples and borehole images, | 64 | numbers of fractures observed from core samples and borehole images, | ||
65 | respectively were not the same due to the different methods", | 65 | respectively were not the same due to the different methods", | ||
66 | "num_resources": 0, | 66 | "num_resources": 0, | ||
67 | "num_tags": 8, | 67 | "num_tags": 8, | ||
68 | "orcid": "0000-0002-4462-155X", | 68 | "orcid": "0000-0002-4462-155X", | ||
69 | "organization": { | 69 | "organization": { | ||
70 | "approval_status": "approved", | 70 | "approval_status": "approved", | ||
n | 71 | "created": "2024-11-29T10:29:57.814346", | n | 71 | "created": "2024-11-30T15:47:13.444138", |
72 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 72 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
73 | Science): The information system PANGAEA is operated as an Open Access | 73 | Science): The information system PANGAEA is operated as an Open Access | ||
74 | library aimed at archiving, publishing and distributing georeferenced | 74 | library aimed at archiving, publishing and distributing georeferenced | ||
75 | data from earth system research. PANGAEA guarantees long-term | 75 | data from earth system research. PANGAEA guarantees long-term | ||
76 | availability (greater than 10 years) of its content. PANGAEA is open | 76 | availability (greater than 10 years) of its content. PANGAEA is open | ||
77 | to any project, institution, or individual scientist to use or to | 77 | to any project, institution, or individual scientist to use or to | ||
78 | archive and publish data. PANGAEA focuses on georeferenced | 78 | archive and publish data. PANGAEA focuses on georeferenced | ||
79 | observational data, experimental data, and models/simulations. | 79 | observational data, experimental data, and models/simulations. | ||
80 | Citability, comprehensive metadata descriptions, interoperability of | 80 | Citability, comprehensive metadata descriptions, interoperability of | ||
81 | data and metadata, a high degree of structural and semantic | 81 | data and metadata, a high degree of structural and semantic | ||
82 | harmonization of the data inventory as well as the commitment of the | 82 | harmonization of the data inventory as well as the commitment of the | ||
83 | hosting institutions ensures FAIRness of archived data.", | 83 | hosting institutions ensures FAIRness of archived data.", | ||
n | 84 | "id": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 84 | "id": "6012878a-1da5-4a37-b3af-fb4949ca1642", |
85 | "image_url": "pangaea_topicgeophysics.png", | 85 | "image_url": "pangaea_topiclithosphere.png", | ||
86 | "is_organization": true, | 86 | "is_organization": true, | ||
n | 87 | "name": "pangaea_geophysics", | n | 87 | "name": "pangaea_lithosphere", |
88 | "state": "active", | 88 | "state": "active", | ||
n | 89 | "title": "PANGAEA (Geophysics)", | n | 89 | "title": "PANGAEA (Lithosphere)", |
90 | "type": "organization" | 90 | "type": "organization" | ||
91 | }, | 91 | }, | ||
n | 92 | "owner_org": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 92 | "owner_org": "6012878a-1da5-4a37-b3af-fb4949ca1642", |
93 | "private": false, | 93 | "private": false, | ||
94 | "publication_year": "2021", | 94 | "publication_year": "2021", | ||
95 | "related_identifiers": [ | 95 | "related_identifiers": [ | ||
96 | { | 96 | { | ||
97 | "authors": "Shibutani Susumu,Lin Weiren,Sado Koichiro,Aizawa | 97 | "authors": "Shibutani Susumu,Lin Weiren,Sado Koichiro,Aizawa | ||
98 | Akihiro,Koike Katsuaki,Kyoto University ", | 98 | Akihiro,Koike Katsuaki,Kyoto University ", | ||
99 | "email_authors": | 99 | "email_authors": | ||
100 | "shibutani.susumu.87m@st.kyoto-u.ac.jp,lin@kumst.kyoto-u.ac.jp,,,,", | 100 | "shibutani.susumu.87m@st.kyoto-u.ac.jp,lin@kumst.kyoto-u.ac.jp,,,,", | ||
101 | "identifier": "https://doi.org/10.1029/2021GC009966", | 101 | "identifier": "https://doi.org/10.1029/2021GC009966", | ||
102 | "identifier_type": "DOI", | 102 | "identifier_type": "DOI", | ||
103 | "orcid_authors": | 103 | "orcid_authors": | ||
104 | "0000-0002-4462-155X,0000-0003-3228-2789,,,0000-0003-2195-1369,", | 104 | "0000-0002-4462-155X,0000-0003-3228-2789,,,0000-0003-2195-1369,", | ||
105 | "relation_type": "References", | 105 | "relation_type": "References", | ||
106 | "source": "Geochemistry, Geophysics, Geosystems", | 106 | "source": "Geochemistry, Geophysics, Geosystems", | ||
107 | "title": "An ancient >200 m cumulative normal faulting | 107 | "title": "An ancient >200 m cumulative normal faulting | ||
108 | displacement along the Futagawa fault dextrally ruptured during the | 108 | displacement along the Futagawa fault dextrally ruptured during the | ||
109 | 2016 Kumamoto, Japan, earthquake identified by a multiborehole | 109 | 2016 Kumamoto, Japan, earthquake identified by a multiborehole | ||
110 | drilling program", | 110 | drilling program", | ||
111 | "year": "2022" | 111 | "year": "2022" | ||
112 | }, | 112 | }, | ||
113 | { | 113 | { | ||
114 | "authors": "Shibutani Susumu,Lin Weiren,Sado Koichiro,Aizawa | 114 | "authors": "Shibutani Susumu,Lin Weiren,Sado Koichiro,Aizawa | ||
115 | Akihiro,Koike Katsuaki,Kyoto University ", | 115 | Akihiro,Koike Katsuaki,Kyoto University ", | ||
116 | "email_authors": | 116 | "email_authors": | ||
117 | "shibutani.susumu.87m@st.kyoto-u.ac.jp,lin@kumst.kyoto-u.ac.jp,,,,", | 117 | "shibutani.susumu.87m@st.kyoto-u.ac.jp,lin@kumst.kyoto-u.ac.jp,,,,", | ||
118 | "identifier": "", | 118 | "identifier": "", | ||
119 | "identifier_type": "DOI", | 119 | "identifier_type": "DOI", | ||
120 | "orcid_authors": | 120 | "orcid_authors": | ||
121 | "0000-0002-4462-155X,0000-0003-3228-2789,,,0000-0003-2195-1369,", | 121 | "0000-0002-4462-155X,0000-0003-3228-2789,,,0000-0003-2195-1369,", | ||
122 | "relation_type": "References", | 122 | "relation_type": "References", | ||
123 | "source": "", | 123 | "source": "", | ||
124 | "title": "Read Me - Physical property distribution and fracture | 124 | "title": "Read Me - Physical property distribution and fracture | ||
125 | density of a ~700 m-deep borehole penetrated through the Futagawa | 125 | density of a ~700 m-deep borehole penetrated through the Futagawa | ||
126 | fault ruptured during the 2016 Kumamoto earthquake mainshock", | 126 | fault ruptured during the 2016 Kumamoto earthquake mainshock", | ||
127 | "year": "" | 127 | "year": "" | ||
128 | }, | 128 | }, | ||
129 | { | 129 | { | ||
130 | "authors": "Shibutani Susumu,Lin Weiren,Sado Koichiro,Aizawa | 130 | "authors": "Shibutani Susumu,Lin Weiren,Sado Koichiro,Aizawa | ||
131 | Akihiro,Koike Katsuaki,Kyoto University ", | 131 | Akihiro,Koike Katsuaki,Kyoto University ", | ||
132 | "email_authors": | 132 | "email_authors": | ||
133 | "shibutani.susumu.87m@st.kyoto-u.ac.jp,lin@kumst.kyoto-u.ac.jp,,,,", | 133 | "shibutani.susumu.87m@st.kyoto-u.ac.jp,lin@kumst.kyoto-u.ac.jp,,,,", | ||
134 | "identifier": "https://www.nra.go.jp/data/000256426.pdf", | 134 | "identifier": "https://www.nra.go.jp/data/000256426.pdf", | ||
135 | "identifier_type": "DOI", | 135 | "identifier_type": "DOI", | ||
136 | "orcid_authors": | 136 | "orcid_authors": | ||
137 | "0000-0002-4462-155X,0000-0003-3228-2789,,,0000-0003-2195-1369,", | 137 | "0000-0002-4462-155X,0000-0003-3228-2789,,,0000-0003-2195-1369,", | ||
138 | "relation_type": "References", | 138 | "relation_type": "References", | ||
139 | "source": "Nuclear Regulation Authority, Japan, Technical Report | 139 | "source": "Nuclear Regulation Authority, Japan, Technical Report | ||
140 | (3/3)", | 140 | (3/3)", | ||
141 | "title": "FY29 Commissioned for the disaster prevention on | 141 | "title": "FY29 Commissioned for the disaster prevention on | ||
142 | nuclear facilities (Boring core and Stress measurement using borehole: | 142 | nuclear facilities (Boring core and Stress measurement using borehole: | ||
143 | No.2 Futagawa fault) (in Japanese)", | 143 | No.2 Futagawa fault) (in Japanese)", | ||
144 | "year": "2018" | 144 | "year": "2018" | ||
145 | } | 145 | } | ||
146 | ], | 146 | ], | ||
147 | "relationships_as_object": [], | 147 | "relationships_as_object": [], | ||
148 | "relationships_as_subject": [], | 148 | "relationships_as_subject": [], | ||
149 | "repository_name": "PANGAEA (Data Publisher for Earth & | 149 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
150 | Environmental Science)", | 150 | Environmental Science)", | ||
151 | "resource_type": "application/zip - filename: Shibutani-etal_2021", | 151 | "resource_type": "application/zip - filename: Shibutani-etal_2021", | ||
152 | "resources": [], | 152 | "resources": [], | ||
153 | "source_metadata_created": "2021", | 153 | "source_metadata_created": "2021", | ||
154 | "source_metadata_modified": "", | 154 | "source_metadata_modified": "", | ||
155 | "state": "active", | 155 | "state": "active", | ||
156 | "subject_areas": [ | 156 | "subject_areas": [ | ||
157 | { | 157 | { | ||
158 | "subject_area_additional": "", | 158 | "subject_area_additional": "", | ||
159 | "subject_area_name": "Chemistry" | 159 | "subject_area_name": "Chemistry" | ||
160 | }, | 160 | }, | ||
161 | { | 161 | { | ||
162 | "subject_area_additional": "", | 162 | "subject_area_additional": "", | ||
163 | "subject_area_name": "Geophysics" | 163 | "subject_area_name": "Geophysics" | ||
164 | }, | 164 | }, | ||
165 | { | 165 | { | ||
166 | "subject_area_additional": "", | 166 | "subject_area_additional": "", | ||
167 | "subject_area_name": "Lithosphere" | 167 | "subject_area_name": "Lithosphere" | ||
168 | } | 168 | } | ||
169 | ], | 169 | ], | ||
170 | "tags": [ | 170 | "tags": [ | ||
171 | { | 171 | { | ||
172 | "display_name": "Futagawa fault", | 172 | "display_name": "Futagawa fault", | ||
173 | "id": "12005e25-2f07-4213-b420-138f7e88fdbb", | 173 | "id": "12005e25-2f07-4213-b420-138f7e88fdbb", | ||
174 | "name": "Futagawa fault", | 174 | "name": "Futagawa fault", | ||
175 | "state": "active", | 175 | "state": "active", | ||
176 | "vocabulary_id": null | 176 | "vocabulary_id": null | ||
177 | }, | 177 | }, | ||
178 | { | 178 | { | ||
179 | "display_name": "Futagawa fault drilling Project", | 179 | "display_name": "Futagawa fault drilling Project", | ||
180 | "id": "4f4060ec-2dff-414a-9e62-31127723e570", | 180 | "id": "4f4060ec-2dff-414a-9e62-31127723e570", | ||
181 | "name": "Futagawa fault drilling Project", | 181 | "name": "Futagawa fault drilling Project", | ||
182 | "state": "active", | 182 | "state": "active", | ||
183 | "vocabulary_id": null | 183 | "vocabulary_id": null | ||
184 | }, | 184 | }, | ||
185 | { | 185 | { | ||
186 | "display_name": "Natural gamma ray", | 186 | "display_name": "Natural gamma ray", | ||
187 | "id": "d8eac384-3337-4a93-89a9-ea8457bfd461", | 187 | "id": "d8eac384-3337-4a93-89a9-ea8457bfd461", | ||
188 | "name": "Natural gamma ray", | 188 | "name": "Natural gamma ray", | ||
189 | "state": "active", | 189 | "state": "active", | ||
190 | "vocabulary_id": null | 190 | "vocabulary_id": null | ||
191 | }, | 191 | }, | ||
192 | { | 192 | { | ||
n | 193 | "display_name": "P-wave velocity", | n | ||
194 | "id": "54f56f8e-5479-4e8f-bce9-4cba6de978b0", | ||||
195 | "name": "P-wave velocity", | ||||
196 | "state": "active", | ||||
197 | "vocabulary_id": null | ||||
198 | }, | ||||
199 | { | ||||
200 | "display_name": "downhole logging", | 193 | "display_name": "downhole logging", | ||
201 | "id": "1f3c813f-0ace-4002-9a70-d5ae58344456", | 194 | "id": "1f3c813f-0ace-4002-9a70-d5ae58344456", | ||
202 | "name": "downhole logging", | 195 | "name": "downhole logging", | ||
203 | "state": "active", | 196 | "state": "active", | ||
204 | "vocabulary_id": null | 197 | "vocabulary_id": null | ||
205 | }, | 198 | }, | ||
206 | { | 199 | { | ||
207 | "display_name": "fracture density", | 200 | "display_name": "fracture density", | ||
208 | "id": "14c9d11a-f20f-43ce-a4cf-bffa7002f070", | 201 | "id": "14c9d11a-f20f-43ce-a4cf-bffa7002f070", | ||
209 | "name": "fracture density", | 202 | "name": "fracture density", | ||
210 | "state": "active", | 203 | "state": "active", | ||
211 | "vocabulary_id": null | 204 | "vocabulary_id": null | ||
212 | }, | 205 | }, | ||
213 | { | 206 | { | ||
214 | "display_name": "resistivity", | 207 | "display_name": "resistivity", | ||
215 | "id": "9d410e1c-a898-4cf6-aa51-fc420f222ce3", | 208 | "id": "9d410e1c-a898-4cf6-aa51-fc420f222ce3", | ||
216 | "name": "resistivity", | 209 | "name": "resistivity", | ||
217 | "state": "active", | 210 | "state": "active", | ||
218 | "vocabulary_id": null | 211 | "vocabulary_id": null | ||
219 | }, | 212 | }, | ||
220 | { | 213 | { | ||
221 | "display_name": "volcanic rocks", | 214 | "display_name": "volcanic rocks", | ||
222 | "id": "346da438-a54d-4774-a3f9-26d4a0e552ee", | 215 | "id": "346da438-a54d-4774-a3f9-26d4a0e552ee", | ||
223 | "name": "volcanic rocks", | 216 | "name": "volcanic rocks", | ||
t | t | 217 | "state": "active", | ||
218 | "vocabulary_id": null | ||||
219 | }, | ||||
220 | { | ||||
221 | "display_name": "wave velocity", | ||||
222 | "id": "a38b897e-9835-41d6-b187-cb8c0b5c45f6", | ||||
223 | "name": "wave velocity", | ||||
224 | "state": "active", | 224 | "state": "active", | ||
225 | "vocabulary_id": null | 225 | "vocabulary_id": null | ||
226 | } | 226 | } | ||
227 | ], | 227 | ], | ||
228 | "title": "Physical property distribution and fracture density of a | 228 | "title": "Physical property distribution and fracture density of a | ||
229 | ~700 m-deep borehole penetrated through the Futagawa fault ruptured | 229 | ~700 m-deep borehole penetrated through the Futagawa fault ruptured | ||
230 | during the 2016 Kumamoto earthquake mainshock", | 230 | during the 2016 Kumamoto earthquake mainshock", | ||
231 | "type": "vdataset", | 231 | "type": "vdataset", | ||
232 | "url": "https://doi.org/10.1594/PANGAEA.933472" | 232 | "url": "https://doi.org/10.1594/PANGAEA.933472" | ||
233 | } | 233 | } |