Changes
On October 22, 2024, 5:27:35 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 5 (previously 4)
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| 2 | "author": null, | 2 | "author": null, | ||
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| 8 | ntink\",\"orcid\":\"0000-0001-5702-3658\",\"affiliation\":\"University | 8 | ntink\",\"orcid\":\"0000-0001-5702-3658\",\"affiliation\":\"University | ||
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| 10 | ":true,\"contactemailaddress\":\"lantink@wisc.edu\",\"formatted\":\"M. | 10 | ":true,\"contactemailaddress\":\"lantink@wisc.edu\",\"formatted\":\"M. | ||
| 11 | L. Lantink - University of Wisconsin Madison - ORCID: | 11 | L. Lantink - University of Wisconsin Madison - ORCID: | ||
| 12 | 0000-0001-5702-3658 - Corresponding Author - | 12 | 0000-0001-5702-3658 - Corresponding Author - | ||
| 13 | lantink@wisc.edu\"},{\"firstname\":\"W. | 13 | lantink@wisc.edu\"},{\"firstname\":\"W. | ||
| 14 | pondingauthor\":null,\"contactemailaddress\":null},{\"firstname\":\"J. | 14 | pondingauthor\":null,\"contactemailaddress\":null},{\"firstname\":\"J. | ||
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| 16 | du Qu\u00e9bec \u00e0 | 16 | du Qu\u00e9bec \u00e0 | ||
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| 18 | H. Davies - Universit\u00e9 du Qu\u00e9bec \u00e0 Montr\u00e9al - | 18 | H. Davies - Universit\u00e9 du Qu\u00e9bec \u00e0 Montr\u00e9al - | ||
| 19 | ORCID: | 19 | ORCID: | ||
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| 21 | Netherlands Institute for Sea | 21 | Netherlands Institute for Sea | ||
| 22 | espondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"R. | 22 | espondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"R. | ||
| 23 | Hennekam - Royal Netherlands Institute for Sea Research - ORCID: | 23 | Hennekam - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 24 | 0000-0002-8823-4519\"},{\"firstname\":\"D. | 24 | 0000-0002-8823-4519\"},{\"firstname\":\"D. | ||
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| 29 | \"Reichart\",\"orcid\":\"0000-0002-7256-2243\",\"affiliation\":\"Royal | 29 | \"Reichart\",\"orcid\":\"0000-0002-7256-2243\",\"affiliation\":\"Royal | ||
| 30 | Netherlands Institute for Sea | 30 | Netherlands Institute for Sea | ||
| 31 | espondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"G. | 31 | espondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"G. | ||
| 32 | J. Reichart - Royal Netherlands Institute for Sea Research - ORCID: | 32 | J. Reichart - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 33 | 0000-0002-7256-2243\"},{\"firstname\":\"C. | 33 | 0000-0002-7256-2243\"},{\"firstname\":\"C. | ||
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| 35 | Netherlands Institute for Sea | 35 | Netherlands Institute for Sea | ||
| 36 | espondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"C. | 36 | espondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"C. | ||
| 37 | P. Slomp - Royal Netherlands Institute for Sea Research - ORCID: | 37 | P. Slomp - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 38 | 0000-0002-7272-0109\"},{\"firstname\":\"F. | 38 | 0000-0002-7272-0109\"},{\"firstname\":\"F. | ||
| 39 | espondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"F. | 39 | espondingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"F. | ||
| 40 | J. Hilgen - ORCID: 0000-0002-5683-259X\"}]", | 40 | J. Hilgen - ORCID: 0000-0002-5683-259X\"}]", | ||
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| 42 | "deposit_date": "2023-03-22", | 42 | "deposit_date": "2023-03-22", | ||
| 43 | "depositor": "Eric Epping", | 43 | "depositor": "Eric Epping", | ||
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| 45 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 45 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 46 | Institute for Sea Research)", | 46 | Institute for Sea Research)", | ||
| 47 | "doi_date_published": "2023-03-22", | 47 | "doi_date_published": "2023-03-22", | ||
| 48 | "geographic_coverage": "[{\"place\":\"Hamersley Range, W. | 48 | "geographic_coverage": "[{\"place\":\"Hamersley Range, W. | ||
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| 56 | "metadata_created": "2024-10-22T11:51:57.991207", | 56 | "metadata_created": "2024-10-22T11:51:57.991207", | ||
| n | 57 | "metadata_modified": "2024-10-22T17:27:35.214279", | n | 57 | "metadata_modified": "2024-10-22T17:27:35.511956", |
| 58 | "name": "7bbbf", | 58 | "name": "7bbbf", | ||
| 59 | "notes": "This file contains raw X-ray fluorescence and line scan | 59 | "notes": "This file contains raw X-ray fluorescence and line scan | ||
| 60 | data of regular 'Knox cyclothem' alternations in two short intervals | 60 | data of regular 'Knox cyclothem' alternations in two short intervals | ||
| 61 | (J45de and J60d) of drill-core DD98SGP001. Core DD98SGP001 contains | 61 | (J45de and J60d) of drill-core DD98SGP001. Core DD98SGP001 contains | ||
| 62 | banded iron formation of the lower Paleoproterozoic Joffre Member of | 62 | banded iron formation of the lower Paleoproterozoic Joffre Member of | ||
| 63 | the Brockman Iron Formation and was drilled in 1998 at Silvergrass | 63 | the Brockman Iron Formation and was drilled in 1998 at Silvergrass | ||
| 64 | Peak (22 03'29.9''S, 116 50' 06.0''E) in the Hamersley Range, Western | 64 | Peak (22 03'29.9''S, 116 50' 06.0''E) in the Hamersley Range, Western | ||
| 65 | Australia; the core is currently stored at the Perth Core Library of | 65 | Australia; the core is currently stored at the Perth Core Library of | ||
| 66 | the Geological Survey of Western Australia. The scanned interval J45de | 66 | the Geological Survey of Western Australia. The scanned interval J45de | ||
| n | 67 | is from 289.05\u2013290.26 m depth in the core (box 45, rows d and e) | n | 67 | is from 289.05 - 290.26 m depth in the core (box 45, rows d and e) and |
| 68 | and contains cherty iron formation-type cyclothems. The scanned | 68 | contains cherty iron formation-type cyclothems. The scanned interval | ||
| 69 | interval 60d is from 358.34\u2013358.73 m depth in the core (box 60, | 69 | 60d is from 358.34 - 358.73 m depth in the core (box 60, row d) and | ||
| 70 | row d) and contains shaley carbonate-type cyclothems.", | 70 | contains shaley carbonate-type cyclothems.", | ||
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| 137 | "state": "active", | 137 | "state": "active", | ||
| 138 | "subject": "Earth and Environmental Sciences", | 138 | "subject": "Earth and Environmental Sciences", | ||
| 139 | "tags": [ | 139 | "tags": [ | ||
| 140 | { | 140 | { | ||
| 141 | "display_name": "Precambrian", | 141 | "display_name": "Precambrian", | ||
| 142 | "id": "887a6d9b-1db8-43ef-ab73-c89efd0ed233", | 142 | "id": "887a6d9b-1db8-43ef-ab73-c89efd0ed233", | ||
| 143 | "name": "Precambrian", | 143 | "name": "Precambrian", | ||
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| 145 | "vocabulary_id": null | 145 | "vocabulary_id": null | ||
| 146 | }, | 146 | }, | ||
| 147 | { | 147 | { | ||
| 148 | "display_name": "XRF core scanning", | 148 | "display_name": "XRF core scanning", | ||
| 149 | "id": "5915e58a-7589-4999-a1b5-79a33113d043", | 149 | "id": "5915e58a-7589-4999-a1b5-79a33113d043", | ||
| 150 | "name": "XRF core scanning", | 150 | "name": "XRF core scanning", | ||
| 151 | "state": "active", | 151 | "state": "active", | ||
| 152 | "vocabulary_id": null | 152 | "vocabulary_id": null | ||
| 153 | }, | 153 | }, | ||
| 154 | { | 154 | { | ||
| 155 | "display_name": "banded iron formations", | 155 | "display_name": "banded iron formations", | ||
| 156 | "id": "846efd42-fb48-405b-a9dd-67f59b72fade", | 156 | "id": "846efd42-fb48-405b-a9dd-67f59b72fade", | ||
| 157 | "name": "banded iron formations", | 157 | "name": "banded iron formations", | ||
| 158 | "state": "active", | 158 | "state": "active", | ||
| 159 | "vocabulary_id": null | 159 | "vocabulary_id": null | ||
| 160 | }, | 160 | }, | ||
| 161 | { | 161 | { | ||
| 162 | "display_name": "cyclostratigraphy", | 162 | "display_name": "cyclostratigraphy", | ||
| 163 | "id": "0adc125e-dd15-4741-978c-32c1be336ce1", | 163 | "id": "0adc125e-dd15-4741-978c-32c1be336ce1", | ||
| 164 | "name": "cyclostratigraphy", | 164 | "name": "cyclostratigraphy", | ||
| 165 | "state": "active", | 165 | "state": "active", | ||
| 166 | "vocabulary_id": null | 166 | "vocabulary_id": null | ||
| 167 | } | 167 | } | ||
| 168 | ], | 168 | ], | ||
| 169 | "title": "Milankovitch cycles in banded iron formations constrain | 169 | "title": "Milankovitch cycles in banded iron formations constrain | ||
| 170 | the Earth - Moon system 2.46 billion years ago. - Data", | 170 | the Earth - Moon system 2.46 billion years ago. - Data", | ||
| 171 | "type": "dataset", | 171 | "type": "dataset", | ||
| 172 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.bf", | 172 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.bf", | ||
| t | 173 | "version": "4" | t | 173 | "version": "5" |
| 174 | } | 174 | } |