Changes
On November 30, 2024 at 7:09:10 PM UTC, admin:
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Moved 2D reflection seismic data from Eivissa Channel, western Mediterranean Sea during RRS Charles Darwin cruise CD178 from organization PANGAEA (Geophysics) to organization PANGAEA (Lithosphere)
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Removed the following tags from 2D reflection seismic data from Eivissa Channel, western Mediterranean Sea during RRS Charles Darwin cruise CD178
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Added the following tags to 2D reflection seismic data from Eivissa Channel, western Mediterranean Sea during RRS Charles Darwin cruise CD178
f | 1 | { | f | 1 | { |
2 | "author": "Berndt, Christian", | 2 | "author": "Berndt, Christian", | ||
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.943523", | 6 | "doi": "10.1594/PANGAEA.943523", | ||
7 | "doi_date_published": "2022", | 7 | "doi_date_published": "2022", | ||
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": "Canals, Miquel", | 12 | "extra_author": "Canals, Miquel", | ||
13 | "familyName": "Canals", | 13 | "familyName": "Canals", | ||
14 | "givenName": "Miquel", | 14 | "givenName": "Miquel", | ||
15 | "orcid": "0000-0001-5267-7601" | 15 | "orcid": "0000-0001-5267-7601" | ||
16 | }, | 16 | }, | ||
17 | { | 17 | { | ||
18 | "extra_author": "Urgeles, Roger", | 18 | "extra_author": "Urgeles, Roger", | ||
19 | "familyName": "Urgeles", | 19 | "familyName": "Urgeles", | ||
20 | "givenName": "Roger", | 20 | "givenName": "Roger", | ||
21 | "orcid": "0000-0001-9438-1753" | 21 | "orcid": "0000-0001-9438-1753" | ||
22 | }, | 22 | }, | ||
23 | { | 23 | { | ||
24 | "extra_author": "Camerlenghi, Angelo", | 24 | "extra_author": "Camerlenghi, Angelo", | ||
25 | "familyName": "Camerlenghi", | 25 | "familyName": "Camerlenghi", | ||
26 | "givenName": "Angelo", | 26 | "givenName": "Angelo", | ||
27 | "orcid": "0000-0002-8128-9533" | 27 | "orcid": "0000-0002-8128-9533" | ||
28 | }, | 28 | }, | ||
29 | { | 29 | { | ||
30 | "extra_author": "Papenberg, Cord", | 30 | "extra_author": "Papenberg, Cord", | ||
31 | "familyName": "Papenberg", | 31 | "familyName": "Papenberg", | ||
32 | "givenName": "Cord", | 32 | "givenName": "Cord", | ||
33 | "orcid": "0000-0001-8790-558X" | 33 | "orcid": "0000-0001-8790-558X" | ||
34 | } | 34 | } | ||
35 | ], | 35 | ], | ||
36 | "familyName": "Berndt", | 36 | "familyName": "Berndt", | ||
37 | "givenName": "Christian", | 37 | "givenName": "Christian", | ||
38 | "groups": [], | 38 | "groups": [], | ||
39 | "id": "d196eae4-5f00-445a-acff-451399abd3ec", | 39 | "id": "d196eae4-5f00-445a-acff-451399abd3ec", | ||
40 | "isopen": false, | 40 | "isopen": false, | ||
41 | "license_id": "CC-BY-4.0", | 41 | "license_id": "CC-BY-4.0", | ||
42 | "license_title": "CC-BY-4.0", | 42 | "license_title": "CC-BY-4.0", | ||
43 | "metadata_created": "2024-11-29T10:32:46.278934", | 43 | "metadata_created": "2024-11-29T10:32:46.278934", | ||
n | 44 | "metadata_modified": "2024-11-29T10:32:46.278943", | n | 44 | "metadata_modified": "2024-11-30T19:09:10.356973", |
45 | "name": "png-doi-10-1594-pangaea-943523", | 45 | "name": "png-doi-10-1594-pangaea-943523", | ||
46 | "notes": "3D reflection seismic data were acquired using the P-Cable | 46 | "notes": "3D reflection seismic data were acquired using the P-Cable | ||
47 | system of the National Oceanographic Centre, Southampton, UK during | 47 | system of the National Oceanographic Centre, Southampton, UK during | ||
48 | cruise 178 Leg 2 onboard RRS Charles Darwin between the 5th and 8th of | 48 | cruise 178 Leg 2 onboard RRS Charles Darwin between the 5th and 8th of | ||
49 | April 2006. The responsible PI's was C. Berndt, Southampton | 49 | April 2006. The responsible PI's was C. Berndt, Southampton | ||
50 | Oceanography Centre, Southampton, UK. The aim of this cruise was to | 50 | Oceanography Centre, Southampton, UK. The aim of this cruise was to | ||
51 | map submarine landslides on the eastern slopes of the Eivissa Channel, | 51 | map submarine landslides on the eastern slopes of the Eivissa Channel, | ||
52 | western Mediterranean Sea located between the islands of | 52 | western Mediterranean Sea located between the islands of | ||
53 | Ibiza-Formentera and the Spanish mainland. Berndt et al. (2012) used | 53 | Ibiza-Formentera and the Spanish mainland. Berndt et al. (2012) used | ||
54 | the acquired data to study repeated slope failure linked to fluid | 54 | the acquired data to study repeated slope failure linked to fluid | ||
55 | migration, while Lafuerza et al. (2012) studied geotechnical aspects | 55 | migration, while Lafuerza et al. (2012) studied geotechnical aspects | ||
56 | of slope stability using this as additional data. Acquisition | 56 | of slope stability using this as additional data. Acquisition | ||
57 | parameters: The source during seismic acquisition consisted of four 40 | 57 | parameters: The source during seismic acquisition consisted of four 40 | ||
58 | in3 Bolt 600B air guns spaced 0.75 m apart and tower at a depth of 1.5 | 58 | in3 Bolt 600B air guns spaced 0.75 m apart and tower at a depth of 1.5 | ||
59 | m about 20 m behind the stern of the vessel (Berndt et al., 2012). The | 59 | m about 20 m behind the stern of the vessel (Berndt et al., 2012). The | ||
60 | air guns are fitted with wave shape kits that emit approximately 10 | 60 | air guns are fitted with wave shape kits that emit approximately 10 | ||
61 | in3 of air prior to the main volume to reduce the bubble pulse. The | 61 | in3 of air prior to the main volume to reduce the bubble pulse. The | ||
62 | air pressure is 2000 psi, and the gun controller triggers the guns to | 62 | air pressure is 2000 psi, and the gun controller triggers the guns to | ||
63 | figure every 7 seconds. The data were collected with 11 single-channel | 63 | figure every 7 seconds. The data were collected with 11 single-channel | ||
64 | analogue streamers that were towed 10 m apart. The seismic cube in the | 64 | analogue streamers that were towed 10 m apart. The seismic cube in the | ||
65 | Eivissa Channel covers an area of ca. 14 km2 (ca. 6.4 EW x 2.2 NS km) | 65 | Eivissa Channel covers an area of ca. 14 km2 (ca. 6.4 EW x 2.2 NS km) | ||
66 | located at 306091.83 4280497.41; 305951.42 4278353.92; 312321.94 | 66 | located at 306091.83 4280497.41; 305951.42 4278353.92; 312321.94 | ||
67 | 4277936.57 in UTM zone 31N. 2D seismic processing: During seismic | 67 | 4277936.57 in UTM zone 31N. 2D seismic processing: During seismic | ||
68 | processing of the 3D dataset significant ghost-artefacts were | 68 | processing of the 3D dataset significant ghost-artefacts were | ||
69 | identified because some of the streamers were towed too deep. This | 69 | identified because some of the streamers were towed too deep. This | ||
70 | required de-ghosting. Unfortunately, these attempts did not yield | 70 | required de-ghosting. Unfortunately, these attempts did not yield | ||
71 | improved quality of the 3D seismic data. This was mainly because the | 71 | improved quality of the 3D seismic data. This was mainly because the | ||
72 | 12.5 m streamers were too short for commonly used de-ghosting | 72 | 12.5 m streamers were too short for commonly used de-ghosting | ||
73 | technique used in the industry. To increase vertical resolution | 73 | technique used in the industry. To increase vertical resolution | ||
74 | individual 2D profiles were extracted from the raw dataset. Processing | 74 | individual 2D profiles were extracted from the raw dataset. Processing | ||
75 | steps included frequency bandpass filtering, burst noise attenuation, | 75 | steps included frequency bandpass filtering, burst noise attenuation, | ||
76 | binning, NMO-correction, stacked, and a Stolt migration with 1520 ms-1 | 76 | binning, NMO-correction, stacked, and a Stolt migration with 1520 ms-1 | ||
77 | was applied that resulted in higher resolution 2D profiles for 85 | 77 | was applied that resulted in higher resolution 2D profiles for 85 | ||
78 | lines and 11 streamers (channels).", | 78 | lines and 11 streamers (channels).", | ||
79 | "num_resources": 0, | 79 | "num_resources": 0, | ||
n | 80 | "num_tags": 15, | n | 80 | "num_tags": 16, |
81 | "orcid": "0000-0001-5055-0180", | 81 | "orcid": "0000-0001-5055-0180", | ||
82 | "organization": { | 82 | "organization": { | ||
83 | "approval_status": "approved", | 83 | "approval_status": "approved", | ||
n | 84 | "created": "2024-11-29T10:29:57.814346", | n | 84 | "created": "2024-11-30T15:47:13.444138", |
85 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 85 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
86 | Science): The information system PANGAEA is operated as an Open Access | 86 | Science): The information system PANGAEA is operated as an Open Access | ||
87 | library aimed at archiving, publishing and distributing georeferenced | 87 | library aimed at archiving, publishing and distributing georeferenced | ||
88 | data from earth system research. PANGAEA guarantees long-term | 88 | data from earth system research. PANGAEA guarantees long-term | ||
89 | availability (greater than 10 years) of its content. PANGAEA is open | 89 | availability (greater than 10 years) of its content. PANGAEA is open | ||
90 | to any project, institution, or individual scientist to use or to | 90 | to any project, institution, or individual scientist to use or to | ||
91 | archive and publish data. PANGAEA focuses on georeferenced | 91 | archive and publish data. PANGAEA focuses on georeferenced | ||
92 | observational data, experimental data, and models/simulations. | 92 | observational data, experimental data, and models/simulations. | ||
93 | Citability, comprehensive metadata descriptions, interoperability of | 93 | Citability, comprehensive metadata descriptions, interoperability of | ||
94 | data and metadata, a high degree of structural and semantic | 94 | data and metadata, a high degree of structural and semantic | ||
95 | harmonization of the data inventory as well as the commitment of the | 95 | harmonization of the data inventory as well as the commitment of the | ||
96 | hosting institutions ensures FAIRness of archived data.", | 96 | hosting institutions ensures FAIRness of archived data.", | ||
n | 97 | "id": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 97 | "id": "6012878a-1da5-4a37-b3af-fb4949ca1642", |
98 | "image_url": "pangaea_topicgeophysics.png", | 98 | "image_url": "pangaea_topiclithosphere.png", | ||
99 | "is_organization": true, | 99 | "is_organization": true, | ||
n | 100 | "name": "pangaea_geophysics", | n | 100 | "name": "pangaea_lithosphere", |
101 | "state": "active", | 101 | "state": "active", | ||
n | 102 | "title": "PANGAEA (Geophysics)", | n | 102 | "title": "PANGAEA (Lithosphere)", |
103 | "type": "organization" | 103 | "type": "organization" | ||
104 | }, | 104 | }, | ||
n | 105 | "owner_org": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 105 | "owner_org": "6012878a-1da5-4a37-b3af-fb4949ca1642", |
106 | "private": false, | 106 | "private": false, | ||
107 | "publication_year": "2022", | 107 | "publication_year": "2022", | ||
108 | "related_identifiers": [ | 108 | "related_identifiers": [ | ||
109 | { | 109 | { | ||
110 | "authors": "Sager Thore Falk,Urlaub Morelia,Kaminski | 110 | "authors": "Sager Thore Falk,Urlaub Morelia,Kaminski | ||
111 | Pauline,Papenberg Cord,Lastras Galderic,Canals Miquel,Berndt | 111 | Pauline,Papenberg Cord,Lastras Galderic,Canals Miquel,Berndt | ||
112 | Christian,Berndt Christian,Costa Sergio,Canals Miquel,Camerlenghi | 112 | Christian,Berndt Christian,Costa Sergio,Canals Miquel,Camerlenghi | ||
113 | Angelo,De Mol Ben,Saunders Martin,Lafuerza Colas Sara,Sultan | 113 | Angelo,De Mol Ben,Saunders Martin,Lafuerza Colas Sara,Sultan | ||
114 | Nabil,Canals Miquel,Lastras Galderic,Cattaneo Antonio,Frigola | 114 | Nabil,Canals Miquel,Lastras Galderic,Cattaneo Antonio,Frigola | ||
115 | Jaime,Costa Sergio,Berndt Christian", | 115 | Jaime,Costa Sergio,Berndt Christian", | ||
116 | "email_authors": | 116 | "email_authors": | ||
117 | b.edu,antonio.cattaneo@ifremer.fr,jfrigola@ub.edu,,cberndt@geomar.de", | 117 | b.edu,antonio.cattaneo@ifremer.fr,jfrigola@ub.edu,,cberndt@geomar.de", | ||
118 | "identifier": "https://doi.org/10.1029/2022GC010469", | 118 | "identifier": "https://doi.org/10.1029/2022GC010469", | ||
119 | "identifier_type": "DOI", | 119 | "identifier_type": "DOI", | ||
120 | "orcid_authors": | 120 | "orcid_authors": | ||
121 | 56-3855,0000-0001-5247-9138,0000-0002-8923-0827,,0000-0001-5055-0180", | 121 | 56-3855,0000-0001-5247-9138,0000-0002-8923-0827,,0000-0001-5055-0180", | ||
122 | "relation_type": "References", | 122 | "relation_type": "References", | ||
123 | "source": "Geochemistry, Geophysics, Geosystems", | 123 | "source": "Geochemistry, Geophysics, Geosystems", | ||
124 | "title": "Development and Emplacement of Ana Slide, Eivissa | 124 | "title": "Development and Emplacement of Ana Slide, Eivissa | ||
125 | Channel, Western Mediterranean Sea", | 125 | Channel, Western Mediterranean Sea", | ||
126 | "year": "2022" | 126 | "year": "2022" | ||
127 | }, | 127 | }, | ||
128 | { | 128 | { | ||
129 | "authors": "Sager Thore Falk,Urlaub Morelia,Kaminski | 129 | "authors": "Sager Thore Falk,Urlaub Morelia,Kaminski | ||
130 | Pauline,Papenberg Cord,Lastras Galderic,Canals Miquel,Berndt | 130 | Pauline,Papenberg Cord,Lastras Galderic,Canals Miquel,Berndt | ||
131 | Christian,Berndt Christian,Costa Sergio,Canals Miquel,Camerlenghi | 131 | Christian,Berndt Christian,Costa Sergio,Canals Miquel,Camerlenghi | ||
132 | Angelo,De Mol Ben,Saunders Martin,Lafuerza Colas Sara,Sultan | 132 | Angelo,De Mol Ben,Saunders Martin,Lafuerza Colas Sara,Sultan | ||
133 | Nabil,Canals Miquel,Lastras Galderic,Cattaneo Antonio,Frigola | 133 | Nabil,Canals Miquel,Lastras Galderic,Cattaneo Antonio,Frigola | ||
134 | Jaime,Costa Sergio,Berndt Christian", | 134 | Jaime,Costa Sergio,Berndt Christian", | ||
135 | "email_authors": | 135 | "email_authors": | ||
136 | b.edu,antonio.cattaneo@ifremer.fr,jfrigola@ub.edu,,cberndt@geomar.de", | 136 | b.edu,antonio.cattaneo@ifremer.fr,jfrigola@ub.edu,,cberndt@geomar.de", | ||
137 | "identifier": "https://doi.org/10.1016/j.epsl.2011.11.045", | 137 | "identifier": "https://doi.org/10.1016/j.epsl.2011.11.045", | ||
138 | "identifier_type": "DOI", | 138 | "identifier_type": "DOI", | ||
139 | "orcid_authors": | 139 | "orcid_authors": | ||
140 | 56-3855,0000-0001-5247-9138,0000-0002-8923-0827,,0000-0001-5055-0180", | 140 | 56-3855,0000-0001-5247-9138,0000-0002-8923-0827,,0000-0001-5055-0180", | ||
141 | "relation_type": "References", | 141 | "relation_type": "References", | ||
142 | "source": "Earth and Planetary Science Letters", | 142 | "source": "Earth and Planetary Science Letters", | ||
143 | "title": "Repeated slope failure linked to fluid migration: The | 143 | "title": "Repeated slope failure linked to fluid migration: The | ||
144 | Ana submarine landslide complex, Eivissa Channel, Western | 144 | Ana submarine landslide complex, Eivissa Channel, Western | ||
145 | Mediterranean Sea", | 145 | Mediterranean Sea", | ||
146 | "year": "2012" | 146 | "year": "2012" | ||
147 | }, | 147 | }, | ||
148 | { | 148 | { | ||
149 | "authors": "Sager Thore Falk,Urlaub Morelia,Kaminski | 149 | "authors": "Sager Thore Falk,Urlaub Morelia,Kaminski | ||
150 | Pauline,Papenberg Cord,Lastras Galderic,Canals Miquel,Berndt | 150 | Pauline,Papenberg Cord,Lastras Galderic,Canals Miquel,Berndt | ||
151 | Christian,Berndt Christian,Costa Sergio,Canals Miquel,Camerlenghi | 151 | Christian,Berndt Christian,Costa Sergio,Canals Miquel,Camerlenghi | ||
152 | Angelo,De Mol Ben,Saunders Martin,Lafuerza Colas Sara,Sultan | 152 | Angelo,De Mol Ben,Saunders Martin,Lafuerza Colas Sara,Sultan | ||
153 | Nabil,Canals Miquel,Lastras Galderic,Cattaneo Antonio,Frigola | 153 | Nabil,Canals Miquel,Lastras Galderic,Cattaneo Antonio,Frigola | ||
154 | Jaime,Costa Sergio,Berndt Christian", | 154 | Jaime,Costa Sergio,Berndt Christian", | ||
155 | "email_authors": | 155 | "email_authors": | ||
156 | b.edu,antonio.cattaneo@ifremer.fr,jfrigola@ub.edu,,cberndt@geomar.de", | 156 | b.edu,antonio.cattaneo@ifremer.fr,jfrigola@ub.edu,,cberndt@geomar.de", | ||
157 | "identifier": "https://doi.org/10.1016/j.margeo.2012.02.010", | 157 | "identifier": "https://doi.org/10.1016/j.margeo.2012.02.010", | ||
158 | "identifier_type": "DOI", | 158 | "identifier_type": "DOI", | ||
159 | "orcid_authors": | 159 | "orcid_authors": | ||
160 | 56-3855,0000-0001-5247-9138,0000-0002-8923-0827,,0000-0001-5055-0180", | 160 | 56-3855,0000-0001-5247-9138,0000-0002-8923-0827,,0000-0001-5055-0180", | ||
161 | "relation_type": "References", | 161 | "relation_type": "References", | ||
162 | "source": "Marine Geology", | 162 | "source": "Marine Geology", | ||
163 | "title": "Failure mechanisms of Ana Slide from geotechnical | 163 | "title": "Failure mechanisms of Ana Slide from geotechnical | ||
164 | evidence, Eivissa Channel, Western Mediterranean Sea", | 164 | evidence, Eivissa Channel, Western Mediterranean Sea", | ||
165 | "year": "2012" | 165 | "year": "2012" | ||
166 | } | 166 | } | ||
167 | ], | 167 | ], | ||
168 | "relationships_as_object": [], | 168 | "relationships_as_object": [], | ||
169 | "relationships_as_subject": [], | 169 | "relationships_as_subject": [], | ||
170 | "repository_name": "PANGAEA (Data Publisher for Earth & | 170 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
171 | Environmental Science)", | 171 | Environmental Science)", | ||
172 | "resource_type": "text/tab-separated-values - filename: | 172 | "resource_type": "text/tab-separated-values - filename: | ||
173 | CD178_2D_seismic_filelist", | 173 | CD178_2D_seismic_filelist", | ||
174 | "resources": [], | 174 | "resources": [], | ||
175 | "source_metadata_created": "2022", | 175 | "source_metadata_created": "2022", | ||
176 | "source_metadata_modified": "", | 176 | "source_metadata_modified": "", | ||
177 | "state": "active", | 177 | "state": "active", | ||
178 | "subject_areas": [ | 178 | "subject_areas": [ | ||
179 | { | 179 | { | ||
180 | "subject_area_additional": "", | 180 | "subject_area_additional": "", | ||
181 | "subject_area_name": "Chemistry" | 181 | "subject_area_name": "Chemistry" | ||
182 | }, | 182 | }, | ||
183 | { | 183 | { | ||
184 | "subject_area_additional": "", | 184 | "subject_area_additional": "", | ||
185 | "subject_area_name": "Geophysics" | 185 | "subject_area_name": "Geophysics" | ||
186 | }, | 186 | }, | ||
187 | { | 187 | { | ||
188 | "subject_area_additional": "", | 188 | "subject_area_additional": "", | ||
189 | "subject_area_name": "Lithosphere" | 189 | "subject_area_name": "Lithosphere" | ||
190 | } | 190 | } | ||
191 | ], | 191 | ], | ||
192 | "tags": [ | 192 | "tags": [ | ||
193 | { | 193 | { | ||
n | 194 | "display_name": "3D seismic P-Cable data", | n | 194 | "display_name": "3D seismic P", |
195 | "id": "d423f79d-b893-4aaa-b0e5-1640f707c526", | 195 | "id": "4d7930bb-3642-4750-ac8f-c0b984c35c44", | ||
196 | "name": "3D seismic P-Cable data", | 196 | "name": "3D seismic P", | ||
197 | "state": "active", | 197 | "state": "active", | ||
198 | "vocabulary_id": null | 198 | "vocabulary_id": null | ||
199 | }, | 199 | }, | ||
200 | { | 200 | { | ||
201 | "display_name": "Ana Slide", | 201 | "display_name": "Ana Slide", | ||
202 | "id": "72497d83-a5a0-45b9-bb64-fb619924eee8", | 202 | "id": "72497d83-a5a0-45b9-bb64-fb619924eee8", | ||
203 | "name": "Ana Slide", | 203 | "name": "Ana Slide", | ||
204 | "state": "active", | 204 | "state": "active", | ||
205 | "vocabulary_id": null | 205 | "vocabulary_id": null | ||
206 | }, | 206 | }, | ||
207 | { | 207 | { | ||
n | n | 208 | "display_name": "Cable", | ||
209 | "id": "b0b1b822-58cc-4bac-9253-3f343d6b50d2", | ||||
210 | "name": "Cable", | ||||
211 | "state": "active", | ||||
212 | "vocabulary_id": null | ||||
213 | }, | ||||
214 | { | ||||
215 | "display_name": "Cable 3D seismic cube", | ||||
216 | "id": "fe5a07fd-ab5c-4d1b-8022-f99691e42d25", | ||||
217 | "name": "Cable 3D seismic cube", | ||||
218 | "state": "active", | ||||
219 | "vocabulary_id": null | ||||
220 | }, | ||||
221 | { | ||||
222 | "display_name": "Cable data", | ||||
223 | "id": "49ef04d4-ac93-4203-a1ec-a8a0ba426264", | ||||
224 | "name": "Cable data", | ||||
225 | "state": "active", | ||||
226 | "vocabulary_id": null | ||||
227 | }, | ||||
228 | { | ||||
208 | "display_name": "Eivissa Channel", | 229 | "display_name": "Eivissa Channel", | ||
209 | "id": "03486bd8-2f16-479c-bfcd-76e417d202c9", | 230 | "id": "03486bd8-2f16-479c-bfcd-76e417d202c9", | ||
210 | "name": "Eivissa Channel", | 231 | "name": "Eivissa Channel", | ||
211 | "state": "active", | 232 | "state": "active", | ||
212 | "vocabulary_id": null | 233 | "vocabulary_id": null | ||
213 | }, | 234 | }, | ||
214 | { | 235 | { | ||
215 | "display_name": "Geomorphology", | 236 | "display_name": "Geomorphology", | ||
216 | "id": "47a95d62-2922-4610-9645-cd724eb5cea8", | 237 | "id": "47a95d62-2922-4610-9645-cd724eb5cea8", | ||
217 | "name": "Geomorphology", | 238 | "name": "Geomorphology", | ||
218 | "state": "active", | 239 | "state": "active", | ||
219 | "vocabulary_id": null | 240 | "vocabulary_id": null | ||
220 | }, | 241 | }, | ||
221 | { | 242 | { | ||
222 | "display_name": "Mediterranean", | 243 | "display_name": "Mediterranean", | ||
223 | "id": "1e88a84b-af34-4881-b402-d2cb8aad852d", | 244 | "id": "1e88a84b-af34-4881-b402-d2cb8aad852d", | ||
224 | "name": "Mediterranean", | 245 | "name": "Mediterranean", | ||
t | 225 | "state": "active", | t | ||
226 | "vocabulary_id": null | ||||
227 | }, | ||||
228 | { | ||||
229 | "display_name": "P-Cable", | ||||
230 | "id": "3bdc4a71-12c4-4f0b-abe1-e3594f5508e8", | ||||
231 | "name": "P-Cable", | ||||
232 | "state": "active", | ||||
233 | "vocabulary_id": null | ||||
234 | }, | ||||
235 | { | ||||
236 | "display_name": "P-Cable 3D seismic cube", | ||||
237 | "id": "e6d38945-130d-4ba7-8202-30e41ee0f153", | ||||
238 | "name": "P-Cable 3D seismic cube", | ||||
239 | "state": "active", | 246 | "state": "active", | ||
240 | "vocabulary_id": null | 247 | "vocabulary_id": null | ||
241 | }, | 248 | }, | ||
242 | { | 249 | { | ||
243 | "display_name": "Spain", | 250 | "display_name": "Spain", | ||
244 | "id": "dd60fd82-643d-4be0-b3ed-cfdfdcd6f5ca", | 251 | "id": "dd60fd82-643d-4be0-b3ed-cfdfdcd6f5ca", | ||
245 | "name": "Spain", | 252 | "name": "Spain", | ||
246 | "state": "active", | 253 | "state": "active", | ||
247 | "vocabulary_id": null | 254 | "vocabulary_id": null | ||
248 | }, | 255 | }, | ||
249 | { | 256 | { | ||
250 | "display_name": "Western Mediterranean", | 257 | "display_name": "Western Mediterranean", | ||
251 | "id": "6f0171cb-ac15-4cac-ab3e-344ff845fb43", | 258 | "id": "6f0171cb-ac15-4cac-ab3e-344ff845fb43", | ||
252 | "name": "Western Mediterranean", | 259 | "name": "Western Mediterranean", | ||
253 | "state": "active", | 260 | "state": "active", | ||
254 | "vocabulary_id": null | 261 | "vocabulary_id": null | ||
255 | }, | 262 | }, | ||
256 | { | 263 | { | ||
257 | "display_name": "Western Mediterranean Sea", | 264 | "display_name": "Western Mediterranean Sea", | ||
258 | "id": "919c24de-b0ff-4ef6-a33a-9464a8545b18", | 265 | "id": "919c24de-b0ff-4ef6-a33a-9464a8545b18", | ||
259 | "name": "Western Mediterranean Sea", | 266 | "name": "Western Mediterranean Sea", | ||
260 | "state": "active", | 267 | "state": "active", | ||
261 | "vocabulary_id": null | 268 | "vocabulary_id": null | ||
262 | }, | 269 | }, | ||
263 | { | 270 | { | ||
264 | "display_name": "geohazards", | 271 | "display_name": "geohazards", | ||
265 | "id": "bee171c4-b88e-45ed-af07-2d37c5b7713e", | 272 | "id": "bee171c4-b88e-45ed-af07-2d37c5b7713e", | ||
266 | "name": "geohazards", | 273 | "name": "geohazards", | ||
267 | "state": "active", | 274 | "state": "active", | ||
268 | "vocabulary_id": null | 275 | "vocabulary_id": null | ||
269 | }, | 276 | }, | ||
270 | { | 277 | { | ||
271 | "display_name": "sediment transport", | 278 | "display_name": "sediment transport", | ||
272 | "id": "70cf6ac6-c4c5-4824-a61c-50ba3d3204e3", | 279 | "id": "70cf6ac6-c4c5-4824-a61c-50ba3d3204e3", | ||
273 | "name": "sediment transport", | 280 | "name": "sediment transport", | ||
274 | "state": "active", | 281 | "state": "active", | ||
275 | "vocabulary_id": null | 282 | "vocabulary_id": null | ||
276 | }, | 283 | }, | ||
277 | { | 284 | { | ||
278 | "display_name": "seismic interpretation", | 285 | "display_name": "seismic interpretation", | ||
279 | "id": "2b77268b-f02d-425e-8ca5-26d9938abb3c", | 286 | "id": "2b77268b-f02d-425e-8ca5-26d9938abb3c", | ||
280 | "name": "seismic interpretation", | 287 | "name": "seismic interpretation", | ||
281 | "state": "active", | 288 | "state": "active", | ||
282 | "vocabulary_id": null | 289 | "vocabulary_id": null | ||
283 | }, | 290 | }, | ||
284 | { | 291 | { | ||
285 | "display_name": "submarine landslide", | 292 | "display_name": "submarine landslide", | ||
286 | "id": "db9e3aaf-0d92-4d4e-b2aa-ebc4a92b6e49", | 293 | "id": "db9e3aaf-0d92-4d4e-b2aa-ebc4a92b6e49", | ||
287 | "name": "submarine landslide", | 294 | "name": "submarine landslide", | ||
288 | "state": "active", | 295 | "state": "active", | ||
289 | "vocabulary_id": null | 296 | "vocabulary_id": null | ||
290 | }, | 297 | }, | ||
291 | { | 298 | { | ||
292 | "display_name": "tectonic geomorphology", | 299 | "display_name": "tectonic geomorphology", | ||
293 | "id": "29541279-69b0-4158-8165-50c980543f40", | 300 | "id": "29541279-69b0-4158-8165-50c980543f40", | ||
294 | "name": "tectonic geomorphology", | 301 | "name": "tectonic geomorphology", | ||
295 | "state": "active", | 302 | "state": "active", | ||
296 | "vocabulary_id": null | 303 | "vocabulary_id": null | ||
297 | } | 304 | } | ||
298 | ], | 305 | ], | ||
299 | "title": "2D reflection seismic data from Eivissa Channel, western | 306 | "title": "2D reflection seismic data from Eivissa Channel, western | ||
300 | Mediterranean Sea during RRS Charles Darwin cruise CD178", | 307 | Mediterranean Sea during RRS Charles Darwin cruise CD178", | ||
301 | "type": "vdataset", | 308 | "type": "vdataset", | ||
302 | "url": "https://doi.org/10.1594/PANGAEA.943523" | 309 | "url": "https://doi.org/10.1594/PANGAEA.943523" | ||
303 | } | 310 | } |