Changes
On November 30, 2024 at 7:10:34 PM UTC, admin:
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Moved Photomicrographs of representative mineralogy from the Nankai subduction zone (Japan) from organization PANGAEA (Geophysics) to organization PANGAEA (Lithosphere)
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Removed tag deep-marine sediments from Photomicrographs of representative mineralogy from the Nankai subduction zone (Japan)
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Added the following tags to Photomicrographs of representative mineralogy from the Nankai subduction zone (Japan)
f | 1 | { | f | 1 | { |
2 | "author": "Cornard, Pauline", | 2 | "author": "Cornard, Pauline", | ||
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.969329", | 6 | "doi": "10.1594/PANGAEA.969329", | ||
7 | "doi_date_published": "2024", | 7 | "doi_date_published": "2024", | ||
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": "Dawson, Harriet", | 12 | "extra_author": "Dawson, Harriet", | ||
13 | "familyName": "Dawson", | 13 | "familyName": "Dawson", | ||
14 | "givenName": "Harriet", | 14 | "givenName": "Harriet", | ||
15 | "orcid": "" | 15 | "orcid": "" | ||
16 | }, | 16 | }, | ||
17 | { | 17 | { | ||
18 | "extra_author": "Pickering, Kevin T", | 18 | "extra_author": "Pickering, Kevin T", | ||
19 | "familyName": "Pickering", | 19 | "familyName": "Pickering", | ||
20 | "givenName": "Kevin T", | 20 | "givenName": "Kevin T", | ||
21 | "orcid": "" | 21 | "orcid": "" | ||
22 | } | 22 | } | ||
23 | ], | 23 | ], | ||
24 | "familyName": "Cornard", | 24 | "familyName": "Cornard", | ||
25 | "givenName": "Pauline", | 25 | "givenName": "Pauline", | ||
26 | "groups": [], | 26 | "groups": [], | ||
27 | "id": "711c5f9f-d0e0-4a3b-81c7-053a15299e77", | 27 | "id": "711c5f9f-d0e0-4a3b-81c7-053a15299e77", | ||
28 | "isopen": false, | 28 | "isopen": false, | ||
29 | "license_id": "CC-BY-4.0", | 29 | "license_id": "CC-BY-4.0", | ||
30 | "license_title": "CC-BY-4.0", | 30 | "license_title": "CC-BY-4.0", | ||
31 | "metadata_created": "2024-11-29T11:21:56.234483", | 31 | "metadata_created": "2024-11-29T11:21:56.234483", | ||
n | 32 | "metadata_modified": "2024-11-29T11:21:56.234489", | n | 32 | "metadata_modified": "2024-11-30T19:10:34.255090", |
33 | "name": "png-doi-10-1594-pangaea-969329", | 33 | "name": "png-doi-10-1594-pangaea-969329", | ||
34 | "notes": "Photomicrographs of representative mineralogy are here | 34 | "notes": "Photomicrographs of representative mineralogy are here | ||
35 | presented for each unit defined in our study. Unit A is dominated by | 35 | presented for each unit defined in our study. Unit A is dominated by | ||
36 | quartz and feldspar whereas clay minerals, clinopyroxene and micas are | 36 | quartz and feldspar whereas clay minerals, clinopyroxene and micas are | ||
37 | in minor proportions (S4.1 and S4.2). Quartz, especially | 37 | in minor proportions (S4.1 and S4.2). Quartz, especially | ||
38 | polycrystalline quartz, is dominant within the Unit B whereas micas | 38 | polycrystalline quartz, is dominant within the Unit B whereas micas | ||
39 | and clinopyroxene are low in abundance (S4.3 and S4.4). Unit C is | 39 | and clinopyroxene are low in abundance (S4.3 and S4.4). Unit C is | ||
40 | characterized by a high content in clay minerals as well as feldspar | 40 | characterized by a high content in clay minerals as well as feldspar | ||
41 | and monocrystalline quartz (S4.5). Unit D is characterized by a high | 41 | and monocrystalline quartz (S4.5). Unit D is characterized by a high | ||
42 | content of polycrystalline quartz (chert) and feldspar (S4.6 and | 42 | content of polycrystalline quartz (chert) and feldspar (S4.6 and | ||
43 | S4.7).", | 43 | S4.7).", | ||
44 | "num_resources": 0, | 44 | "num_resources": 0, | ||
n | 45 | "num_tags": 3, | n | 45 | "num_tags": 4, |
46 | "orcid": "0000-0002-5034-937X", | 46 | "orcid": "0000-0002-5034-937X", | ||
47 | "organization": { | 47 | "organization": { | ||
48 | "approval_status": "approved", | 48 | "approval_status": "approved", | ||
n | 49 | "created": "2024-11-29T10:29:57.814346", | n | 49 | "created": "2024-11-30T15:47:13.444138", |
50 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 50 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
51 | Science): The information system PANGAEA is operated as an Open Access | 51 | Science): The information system PANGAEA is operated as an Open Access | ||
52 | library aimed at archiving, publishing and distributing georeferenced | 52 | library aimed at archiving, publishing and distributing georeferenced | ||
53 | data from earth system research. PANGAEA guarantees long-term | 53 | data from earth system research. PANGAEA guarantees long-term | ||
54 | availability (greater than 10 years) of its content. PANGAEA is open | 54 | availability (greater than 10 years) of its content. PANGAEA is open | ||
55 | to any project, institution, or individual scientist to use or to | 55 | to any project, institution, or individual scientist to use or to | ||
56 | archive and publish data. PANGAEA focuses on georeferenced | 56 | archive and publish data. PANGAEA focuses on georeferenced | ||
57 | observational data, experimental data, and models/simulations. | 57 | observational data, experimental data, and models/simulations. | ||
58 | Citability, comprehensive metadata descriptions, interoperability of | 58 | Citability, comprehensive metadata descriptions, interoperability of | ||
59 | data and metadata, a high degree of structural and semantic | 59 | data and metadata, a high degree of structural and semantic | ||
60 | harmonization of the data inventory as well as the commitment of the | 60 | harmonization of the data inventory as well as the commitment of the | ||
61 | hosting institutions ensures FAIRness of archived data.", | 61 | hosting institutions ensures FAIRness of archived data.", | ||
n | 62 | "id": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 62 | "id": "6012878a-1da5-4a37-b3af-fb4949ca1642", |
63 | "image_url": "pangaea_topicgeophysics.png", | 63 | "image_url": "pangaea_topiclithosphere.png", | ||
64 | "is_organization": true, | 64 | "is_organization": true, | ||
n | 65 | "name": "pangaea_geophysics", | n | 65 | "name": "pangaea_lithosphere", |
66 | "state": "active", | 66 | "state": "active", | ||
n | 67 | "title": "PANGAEA (Geophysics)", | n | 67 | "title": "PANGAEA (Lithosphere)", |
68 | "type": "organization" | 68 | "type": "organization" | ||
69 | }, | 69 | }, | ||
n | 70 | "owner_org": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 70 | "owner_org": "6012878a-1da5-4a37-b3af-fb4949ca1642", |
71 | "private": false, | 71 | "private": false, | ||
72 | "publication_year": "2024", | 72 | "publication_year": "2024", | ||
73 | "related_identifiers": [ | 73 | "related_identifiers": [ | ||
74 | { | 74 | { | ||
75 | "authors": "Cornard Pauline,Dawson H L,Pickering K T", | 75 | "authors": "Cornard Pauline,Dawson H L,Pickering K T", | ||
76 | "email_authors": "cornard@uni-bremen.de,,", | 76 | "email_authors": "cornard@uni-bremen.de,,", | ||
77 | "identifier": "https://doi.org/10.1029/2023GC011393", | 77 | "identifier": "https://doi.org/10.1029/2023GC011393", | ||
78 | "identifier_type": "DOI", | 78 | "identifier_type": "DOI", | ||
79 | "orcid_authors": "0000-0002-5034-937X,0000-0002-5362-4058,", | 79 | "orcid_authors": "0000-0002-5034-937X,0000-0002-5362-4058,", | ||
80 | "relation_type": "References", | 80 | "relation_type": "References", | ||
81 | "source": "Geochemistry, Geophysics, Geosystems", | 81 | "source": "Geochemistry, Geophysics, Geosystems", | ||
82 | "title": "Sediment Provenance Along the Middle | 82 | "title": "Sediment Provenance Along the Middle | ||
83 | Miocene\u2010Pleistocene Nankai Subduction Zone From Sediment | 83 | Miocene\u2010Pleistocene Nankai Subduction Zone From Sediment | ||
84 | Transport to Accretion: Implications for Stratigraphy in the | 84 | Transport to Accretion: Implications for Stratigraphy in the | ||
85 | Accretionary Prism", | 85 | Accretionary Prism", | ||
86 | "year": "2024" | 86 | "year": "2024" | ||
87 | } | 87 | } | ||
88 | ], | 88 | ], | ||
89 | "relationships_as_object": [], | 89 | "relationships_as_object": [], | ||
90 | "relationships_as_subject": [], | 90 | "relationships_as_subject": [], | ||
91 | "repository_name": "PANGAEA (Data Publisher for Earth & | 91 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
92 | Environmental Science)", | 92 | Environmental Science)", | ||
93 | "resource_type": "text/tab-separated-values - filename: | 93 | "resource_type": "text/tab-separated-values - filename: | ||
94 | Conrad-etal_S4_photomicrographs", | 94 | Conrad-etal_S4_photomicrographs", | ||
95 | "resources": [], | 95 | "resources": [], | ||
96 | "source_metadata_created": "2024", | 96 | "source_metadata_created": "2024", | ||
97 | "source_metadata_modified": "", | 97 | "source_metadata_modified": "", | ||
98 | "state": "active", | 98 | "state": "active", | ||
99 | "subject_areas": [ | 99 | "subject_areas": [ | ||
100 | { | 100 | { | ||
101 | "subject_area_additional": "", | 101 | "subject_area_additional": "", | ||
102 | "subject_area_name": "Chemistry" | 102 | "subject_area_name": "Chemistry" | ||
103 | }, | 103 | }, | ||
104 | { | 104 | { | ||
105 | "subject_area_additional": "", | 105 | "subject_area_additional": "", | ||
106 | "subject_area_name": "Geophysics" | 106 | "subject_area_name": "Geophysics" | ||
107 | }, | 107 | }, | ||
108 | { | 108 | { | ||
109 | "subject_area_additional": "", | 109 | "subject_area_additional": "", | ||
110 | "subject_area_name": "Lithosphere" | 110 | "subject_area_name": "Lithosphere" | ||
111 | } | 111 | } | ||
112 | ], | 112 | ], | ||
113 | "tags": [ | 113 | "tags": [ | ||
114 | { | 114 | { | ||
t | t | 115 | "display_name": "deep", | ||
116 | "id": "5ef4b3b4-37a7-4009-8d0d-a9c1dd6ba210", | ||||
117 | "name": "deep", | ||||
118 | "state": "active", | ||||
119 | "vocabulary_id": null | ||||
120 | }, | ||||
121 | { | ||||
115 | "display_name": "deep-marine sediments", | 122 | "display_name": "marine sediments", | ||
116 | "id": "e577cda8-4d06-405c-a57b-8a145f93af84", | 123 | "id": "aaea24b3-cd98-4748-be2a-b2922c6812d5", | ||
117 | "name": "deep-marine sediments", | 124 | "name": "marine sediments", | ||
118 | "state": "active", | 125 | "state": "active", | ||
119 | "vocabulary_id": null | 126 | "vocabulary_id": null | ||
120 | }, | 127 | }, | ||
121 | { | 128 | { | ||
122 | "display_name": "petrography analysis", | 129 | "display_name": "petrography analysis", | ||
123 | "id": "f7986138-ca95-4cc1-82ce-bbe79a331750", | 130 | "id": "f7986138-ca95-4cc1-82ce-bbe79a331750", | ||
124 | "name": "petrography analysis", | 131 | "name": "petrography analysis", | ||
125 | "state": "active", | 132 | "state": "active", | ||
126 | "vocabulary_id": null | 133 | "vocabulary_id": null | ||
127 | }, | 134 | }, | ||
128 | { | 135 | { | ||
129 | "display_name": "zircon age dating", | 136 | "display_name": "zircon age dating", | ||
130 | "id": "612b281c-731e-40a8-8b50-ecc8a0b123de", | 137 | "id": "612b281c-731e-40a8-8b50-ecc8a0b123de", | ||
131 | "name": "zircon age dating", | 138 | "name": "zircon age dating", | ||
132 | "state": "active", | 139 | "state": "active", | ||
133 | "vocabulary_id": null | 140 | "vocabulary_id": null | ||
134 | } | 141 | } | ||
135 | ], | 142 | ], | ||
136 | "title": "Photomicrographs of representative mineralogy from the | 143 | "title": "Photomicrographs of representative mineralogy from the | ||
137 | Nankai subduction zone (Japan)", | 144 | Nankai subduction zone (Japan)", | ||
138 | "type": "vdataset", | 145 | "type": "vdataset", | ||
139 | "url": "https://doi.org/10.1594/PANGAEA.969329" | 146 | "url": "https://doi.org/10.1594/PANGAEA.969329" | ||
140 | } | 147 | } |