Changes
On October 22, 2024, 8:55:08 PM UTC,
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Updated description of Milankovitch cycles in banded iron formations constrain the Earth–Moon system 2.46 billion years ago. - Data from
This file contains raw X-ray fluorescence and line scan data of regular ‘Knox cyclothem’ alternations in two short intervals (J45de and J60d) of drill-core DD98SGP001. Core DD98SGP001 contains banded iron formation of the lower Paleoproterozoic Joffre Member of the Brockman Iron Formation and was drilled in 1998 at Silvergrass Peak (22°03'29.9''S, 116°50' 06.0''E) in the Hamersley Range, Western Australia; the core is currently stored at the Perth Core Library of the Geological Survey of Western Australia. The scanned interval J45de is from 289.05–290.26 m depth in the core (box 45, rows d and e) and contains cherty iron formation-type cyclothems. The scanned interval 60d is from 358.34–358.73 m depth in the core (box 60, row d) and contains shaley carbonate-type cyclothems.
toThis file contains raw X-ray fluorescence and line scan data of regular 'Knox cyclothem' alternations in two short intervals (J45de and J60d) of drill-core DD98SGP001. Core DD98SGP001 contains banded iron formation of the lower Paleoproterozoic Joffre Member of the Brockman Iron Formation and was drilled in 1998 at Silvergrass Peak (22 03'29.9''S, 116 50' 06.0''E) in the Hamersley Range, Western Australia; the core is currently stored at the Perth Core Library of the Geological Survey of Western Australia. The scanned interval J45de is from 289.05–290.26 m depth in the core (box 45, rows d and e) and contains cherty iron formation-type cyclothems. The scanned interval 60d is from 358.34–358.73 m depth in the core (box 60, row d) and contains shaley carbonate-type cyclothems.
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Changed the version of Milankovitch cycles in banded iron formations constrain the Earth–Moon system 2.46 billion years ago. - Data to 3 (previously 2)
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| 32 | J. Reichart - Royal Netherlands Institute for Sea Research - ORCID: | 32 | J. Reichart - Royal Netherlands Institute for Sea Research - ORCID: | ||
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| 37 | P. Slomp - Royal Netherlands Institute for Sea Research - ORCID: | 37 | P. Slomp - Royal Netherlands Institute for Sea Research - ORCID: | ||
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| 46 | Institute for Sea Research)", | 46 | Institute for Sea Research)", | ||
| 47 | "doi_date_published": "2023-03-22", | 47 | "doi_date_published": "2023-03-22", | ||
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| 61 | "notes": "This file contains raw X-ray fluorescence and line scan | 61 | "notes": "This file contains raw X-ray fluorescence and line scan | ||
| n | 62 | data of regular \u2018Knox cyclothem\u2019 alternations in two short | n | 62 | data of regular 'Knox cyclothem' alternations in two short intervals |
| 63 | intervals (J45de and J60d) of drill-core DD98SGP001. Core DD98SGP001 | 63 | (J45de and J60d) of drill-core DD98SGP001. Core DD98SGP001 contains | ||
| 64 | contains banded iron formation of the lower Paleoproterozoic Joffre | 64 | banded iron formation of the lower Paleoproterozoic Joffre Member of | ||
| 65 | Member of the Brockman Iron Formation and was drilled in 1998 at | 65 | the Brockman Iron Formation and was drilled in 1998 at Silvergrass | ||
| 66 | Silvergrass Peak (22\u00b003'29.9''S, 116\u00b050' 06.0''E) in the | 66 | Peak (22 03'29.9''S, 116 50' 06.0''E) in the Hamersley Range, Western | ||
| 67 | Hamersley Range, Western Australia; the core is currently stored at | 67 | Australia; the core is currently stored at the Perth Core Library of | ||
| 68 | the Perth Core Library of the Geological Survey of Western Australia. | 68 | the Geological Survey of Western Australia. The scanned interval J45de | ||
| 69 | The scanned interval J45de is from 289.05\u2013290.26 m depth in the | 69 | is from 289.05\u2013290.26 m depth in the core (box 45, rows d and e) | ||
| 70 | core (box 45, rows d and e) and contains cherty iron formation-type | 70 | and contains cherty iron formation-type cyclothems. The scanned | ||
| 71 | cyclothems. The scanned interval 60d is from 358.34\u2013358.73 m | 71 | interval 60d is from 358.34\u2013358.73 m depth in the core (box 60, | ||
| 72 | depth in the core (box 60, row d) and contains shaley carbonate-type | 72 | row d) and contains shaley carbonate-type cyclothems.", | ||
| 73 | cyclothems.", | ||||
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| 140 | "state": "active", | 139 | "state": "active", | ||
| 141 | "subject": "Earth and Environmental Sciences", | 140 | "subject": "Earth and Environmental Sciences", | ||
| 142 | "tags": [ | 141 | "tags": [ | ||
| 143 | { | 142 | { | ||
| 144 | "display_name": "Precambrian", | 143 | "display_name": "Precambrian", | ||
| 145 | "id": "887a6d9b-1db8-43ef-ab73-c89efd0ed233", | 144 | "id": "887a6d9b-1db8-43ef-ab73-c89efd0ed233", | ||
| 146 | "name": "Precambrian", | 145 | "name": "Precambrian", | ||
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| 148 | "vocabulary_id": null | 147 | "vocabulary_id": null | ||
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| 150 | { | 149 | { | ||
| 151 | "display_name": "XRF core scanning", | 150 | "display_name": "XRF core scanning", | ||
| 152 | "id": "5915e58a-7589-4999-a1b5-79a33113d043", | 151 | "id": "5915e58a-7589-4999-a1b5-79a33113d043", | ||
| 153 | "name": "XRF core scanning", | 152 | "name": "XRF core scanning", | ||
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| 155 | "vocabulary_id": null | 154 | "vocabulary_id": null | ||
| 156 | }, | 155 | }, | ||
| 157 | { | 156 | { | ||
| 158 | "display_name": "banded iron formations", | 157 | "display_name": "banded iron formations", | ||
| 159 | "id": "846efd42-fb48-405b-a9dd-67f59b72fade", | 158 | "id": "846efd42-fb48-405b-a9dd-67f59b72fade", | ||
| 160 | "name": "banded iron formations", | 159 | "name": "banded iron formations", | ||
| 161 | "state": "active", | 160 | "state": "active", | ||
| 162 | "vocabulary_id": null | 161 | "vocabulary_id": null | ||
| 163 | }, | 162 | }, | ||
| 164 | { | 163 | { | ||
| 165 | "display_name": "cyclostratigraphy", | 164 | "display_name": "cyclostratigraphy", | ||
| 166 | "id": "0adc125e-dd15-4741-978c-32c1be336ce1", | 165 | "id": "0adc125e-dd15-4741-978c-32c1be336ce1", | ||
| 167 | "name": "cyclostratigraphy", | 166 | "name": "cyclostratigraphy", | ||
| 168 | "state": "active", | 167 | "state": "active", | ||
| 169 | "vocabulary_id": null | 168 | "vocabulary_id": null | ||
| 170 | } | 169 | } | ||
| 171 | ], | 170 | ], | ||
| 172 | "title": "Milankovitch cycles in banded iron formations constrain | 171 | "title": "Milankovitch cycles in banded iron formations constrain | ||
| 173 | the Earth\u2013Moon system 2.46 billion years ago. - Data", | 172 | the Earth\u2013Moon system 2.46 billion years ago. - Data", | ||
| 174 | "type": "dataset", | 173 | "type": "dataset", | ||
| 175 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.bf", | 174 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.bf", | ||
| t | 176 | "version": "2" | t | 175 | "version": "3" |
| 177 | } | 176 | } |