Changes
On November 30, 2024 at 2:02:16 PM UTC, admin:
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Moved Point-count analyses of grains from the Nankai subduction zone (Japan) at IODP Site 348-C0002 from organization PANGAEA (Geophysics) to organization PANGAEA (Paleontology)
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Removed tag deep-marine sediments from Point-count analyses of grains from the Nankai subduction zone (Japan) at IODP Site 348-C0002
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Added the following tags to Point-count analyses of grains from the Nankai subduction zone (Japan) at IODP Site 348-C0002
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.969334", | 6 | "doi": "10.1594/PANGAEA.969334", | ||
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": "6711307d-e7ec-43f1-94d2-a06c2d273e2f", | 27 | "id": "6711307d-e7ec-43f1-94d2-a06c2d273e2f", | ||
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": "2024-11-29T11:21:56.483085", | 31 | "metadata_created": "2024-11-29T11:21:56.483085", | ||
n | 32 | "metadata_modified": "2024-11-29T11:21:56.483092", | n | 32 | "metadata_modified": "2024-11-30T14:02:16.135619", |
33 | "name": "png-doi-10-1594-pangaea-969334", | 33 | "name": "png-doi-10-1594-pangaea-969334", | ||
34 | "notes": "For petrographic analyses, point counting was used to | 34 | "notes": "For petrographic analyses, point counting was used to | ||
35 | quantitatively estimate the modal composition of sand and sandstones | 35 | quantitatively estimate the modal composition of sand and sandstones | ||
36 | by totalling the occurrence of various mineral grains within a | 36 | by totalling the occurrence of various mineral grains within a | ||
37 | representative sample. The Gazzi-Dickinson methos was chosen for this | 37 | representative sample. The Gazzi-Dickinson methos was chosen for this | ||
38 | study. A total of 80 cutting and core samples from IODP Expedition 348 | 38 | study. A total of 80 cutting and core samples from IODP Expedition 348 | ||
39 | were used for this study, covering a total depth transect from | 39 | were used for this study, covering a total depth transect from | ||
40 | 1,140.5-3,000.5 mbsf of the Nankai Accretionary Prism (SW Japan) at | 40 | 1,140.5-3,000.5 mbsf of the Nankai Accretionary Prism (SW Japan) at | ||
41 | sites C0002N and C0002P. All 80 samples were prepared for thin | 41 | sites C0002N and C0002P. All 80 samples were prepared for thin | ||
42 | sections for quantitative modal compositional analysis at The Open | 42 | sections for quantitative modal compositional analysis at The Open | ||
43 | University (United Kingdom). Samples were sieved to remove clay and | 43 | University (United Kingdom). Samples were sieved to remove clay and | ||
44 | silt from the unconsolidated material. Approximately 10 grams of sands | 44 | silt from the unconsolidated material. Approximately 10 grams of sands | ||
45 | were then separated from the sieved samples and mixed with epoxy. The | 45 | were then separated from the sieved samples and mixed with epoxy. The | ||
46 | epoxy grain mounts were sliced to thin section thickness, cemented to | 46 | epoxy grain mounts were sliced to thin section thickness, cemented to | ||
47 | glass slides with epoxy resin, and then thin sections were completed | 47 | glass slides with epoxy resin, and then thin sections were completed | ||
48 | in the usual method. Point-count analyses involved 400 points per | 48 | in the usual method. Point-count analyses involved 400 points per | ||
49 | sample. Each grain was assigned to a classification category (e.g., | 49 | sample. Each grain was assigned to a classification category (e.g., | ||
50 | monocrystalline quartz, polycrystalline quartz, feldspar, volcanic | 50 | monocrystalline quartz, polycrystalline quartz, feldspar, volcanic | ||
51 | lithic, sedimentary lithics, etc).", | 51 | lithic, sedimentary lithics, etc).", | ||
52 | "num_resources": 0, | 52 | "num_resources": 0, | ||
n | 53 | "num_tags": 3, | n | 53 | "num_tags": 4, |
54 | "orcid": "0000-0002-5034-937X", | 54 | "orcid": "0000-0002-5034-937X", | ||
55 | "organization": { | 55 | "organization": { | ||
56 | "approval_status": "approved", | 56 | "approval_status": "approved", | ||
n | 57 | "created": "2024-11-29T10:29:57.814346", | n | 57 | "created": "2024-11-30T13:39:52.424343", |
58 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 58 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
59 | Science): The information system PANGAEA is operated as an Open Access | 59 | Science): The information system PANGAEA is operated as an Open Access | ||
60 | library aimed at archiving, publishing and distributing georeferenced | 60 | library aimed at archiving, publishing and distributing georeferenced | ||
61 | data from earth system research. PANGAEA guarantees long-term | 61 | data from earth system research. PANGAEA guarantees long-term | ||
62 | availability (greater than 10 years) of its content. PANGAEA is open | 62 | availability (greater than 10 years) of its content. PANGAEA is open | ||
63 | to any project, institution, or individual scientist to use or to | 63 | to any project, institution, or individual scientist to use or to | ||
64 | archive and publish data. PANGAEA focuses on georeferenced | 64 | archive and publish data. PANGAEA focuses on georeferenced | ||
65 | observational data, experimental data, and models/simulations. | 65 | observational data, experimental data, and models/simulations. | ||
66 | Citability, comprehensive metadata descriptions, interoperability of | 66 | Citability, comprehensive metadata descriptions, interoperability of | ||
67 | data and metadata, a high degree of structural and semantic | 67 | data and metadata, a high degree of structural and semantic | ||
68 | harmonization of the data inventory as well as the commitment of the | 68 | harmonization of the data inventory as well as the commitment of the | ||
69 | hosting institutions ensures FAIRness of archived data.", | 69 | hosting institutions ensures FAIRness of archived data.", | ||
n | 70 | "id": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 70 | "id": "2155a83b-7d71-4ebb-88a3-6bb2a056a25e", |
71 | "image_url": "pangaea_topicgeophysics.png", | 71 | "image_url": "pangaea_topicpaleontology.png", | ||
72 | "is_organization": true, | 72 | "is_organization": true, | ||
n | 73 | "name": "pangaea_geophysics", | n | 73 | "name": "pangaea_paleontology", |
74 | "state": "active", | 74 | "state": "active", | ||
n | 75 | "title": "PANGAEA (Geophysics)", | n | 75 | "title": "PANGAEA (Paleontology)", |
76 | "type": "organization" | 76 | "type": "organization" | ||
77 | }, | 77 | }, | ||
n | 78 | "owner_org": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 78 | "owner_org": "2155a83b-7d71-4ebb-88a3-6bb2a056a25e", |
79 | "private": false, | 79 | "private": false, | ||
80 | "publication_year": "2024", | 80 | "publication_year": "2024", | ||
81 | "related_identifiers": [ | 81 | "related_identifiers": [ | ||
82 | { | 82 | { | ||
83 | "authors": "Cornard Pauline,Dawson H L,Pickering K T", | 83 | "authors": "Cornard Pauline,Dawson H L,Pickering K T", | ||
84 | "email_authors": "cornard@uni-bremen.de,,", | 84 | "email_authors": "cornard@uni-bremen.de,,", | ||
85 | "identifier": "https://doi.org/10.1029/2023GC011393", | 85 | "identifier": "https://doi.org/10.1029/2023GC011393", | ||
86 | "identifier_type": "DOI", | 86 | "identifier_type": "DOI", | ||
87 | "orcid_authors": "0000-0002-5034-937X,0000-0002-5362-4058,", | 87 | "orcid_authors": "0000-0002-5034-937X,0000-0002-5362-4058,", | ||
88 | "relation_type": "References", | 88 | "relation_type": "References", | ||
89 | "source": "Geochemistry, Geophysics, Geosystems", | 89 | "source": "Geochemistry, Geophysics, Geosystems", | ||
90 | "title": "Sediment Provenance Along the Middle | 90 | "title": "Sediment Provenance Along the Middle | ||
91 | Miocene\u2010Pleistocene Nankai Subduction Zone From Sediment | 91 | Miocene\u2010Pleistocene Nankai Subduction Zone From Sediment | ||
92 | Transport to Accretion: Implications for Stratigraphy in the | 92 | Transport to Accretion: Implications for Stratigraphy in the | ||
93 | Accretionary Prism", | 93 | Accretionary Prism", | ||
94 | "year": "2024" | 94 | "year": "2024" | ||
95 | } | 95 | } | ||
96 | ], | 96 | ], | ||
97 | "relationships_as_object": [], | 97 | "relationships_as_object": [], | ||
98 | "relationships_as_subject": [], | 98 | "relationships_as_subject": [], | ||
99 | "repository_name": "PANGAEA (Data Publisher for Earth & | 99 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
100 | Environmental Science)", | 100 | Environmental Science)", | ||
101 | "resource_type": "text/tab-separated-values - filename: | 101 | "resource_type": "text/tab-separated-values - filename: | ||
102 | Conrad-etal_S1_point-count_grains", | 102 | Conrad-etal_S1_point-count_grains", | ||
103 | "resources": [], | 103 | "resources": [], | ||
104 | "source_metadata_created": "2024", | 104 | "source_metadata_created": "2024", | ||
105 | "source_metadata_modified": "", | 105 | "source_metadata_modified": "", | ||
106 | "state": "active", | 106 | "state": "active", | ||
107 | "subject_areas": [ | 107 | "subject_areas": [ | ||
108 | { | 108 | { | ||
109 | "subject_area_additional": "", | 109 | "subject_area_additional": "", | ||
110 | "subject_area_name": "BiologicalClassification" | 110 | "subject_area_name": "BiologicalClassification" | ||
111 | }, | 111 | }, | ||
112 | { | 112 | { | ||
113 | "subject_area_additional": "", | 113 | "subject_area_additional": "", | ||
114 | "subject_area_name": "Chemistry" | 114 | "subject_area_name": "Chemistry" | ||
115 | }, | 115 | }, | ||
116 | { | 116 | { | ||
117 | "subject_area_additional": "", | 117 | "subject_area_additional": "", | ||
118 | "subject_area_name": "Geophysics" | 118 | "subject_area_name": "Geophysics" | ||
119 | }, | 119 | }, | ||
120 | { | 120 | { | ||
121 | "subject_area_additional": "", | 121 | "subject_area_additional": "", | ||
122 | "subject_area_name": "Lithosphere" | 122 | "subject_area_name": "Lithosphere" | ||
123 | }, | 123 | }, | ||
124 | { | 124 | { | ||
125 | "subject_area_additional": "", | 125 | "subject_area_additional": "", | ||
126 | "subject_area_name": "Paleontology" | 126 | "subject_area_name": "Paleontology" | ||
127 | } | 127 | } | ||
128 | ], | 128 | ], | ||
129 | "tags": [ | 129 | "tags": [ | ||
130 | { | 130 | { | ||
t | t | 131 | "display_name": "deep", | ||
132 | "id": "5ef4b3b4-37a7-4009-8d0d-a9c1dd6ba210", | ||||
133 | "name": "deep", | ||||
134 | "state": "active", | ||||
135 | "vocabulary_id": null | ||||
136 | }, | ||||
137 | { | ||||
131 | "display_name": "deep-marine sediments", | 138 | "display_name": "marine sediments", | ||
132 | "id": "e577cda8-4d06-405c-a57b-8a145f93af84", | 139 | "id": "aaea24b3-cd98-4748-be2a-b2922c6812d5", | ||
133 | "name": "deep-marine sediments", | 140 | "name": "marine sediments", | ||
134 | "state": "active", | 141 | "state": "active", | ||
135 | "vocabulary_id": null | 142 | "vocabulary_id": null | ||
136 | }, | 143 | }, | ||
137 | { | 144 | { | ||
138 | "display_name": "petrography analysis", | 145 | "display_name": "petrography analysis", | ||
139 | "id": "f7986138-ca95-4cc1-82ce-bbe79a331750", | 146 | "id": "f7986138-ca95-4cc1-82ce-bbe79a331750", | ||
140 | "name": "petrography analysis", | 147 | "name": "petrography analysis", | ||
141 | "state": "active", | 148 | "state": "active", | ||
142 | "vocabulary_id": null | 149 | "vocabulary_id": null | ||
143 | }, | 150 | }, | ||
144 | { | 151 | { | ||
145 | "display_name": "zircon age dating", | 152 | "display_name": "zircon age dating", | ||
146 | "id": "612b281c-731e-40a8-8b50-ecc8a0b123de", | 153 | "id": "612b281c-731e-40a8-8b50-ecc8a0b123de", | ||
147 | "name": "zircon age dating", | 154 | "name": "zircon age dating", | ||
148 | "state": "active", | 155 | "state": "active", | ||
149 | "vocabulary_id": null | 156 | "vocabulary_id": null | ||
150 | } | 157 | } | ||
151 | ], | 158 | ], | ||
152 | "title": "Point-count analyses of grains from the Nankai subduction | 159 | "title": "Point-count analyses of grains from the Nankai subduction | ||
153 | zone (Japan) at IODP Site 348-C0002", | 160 | zone (Japan) at IODP Site 348-C0002", | ||
154 | "type": "vdataset", | 161 | "type": "vdataset", | ||
155 | "url": "https://doi.org/10.1594/PANGAEA.969334" | 162 | "url": "https://doi.org/10.1594/PANGAEA.969334" | ||
156 | } | 163 | } |