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On October 22, 2024, 8:55:07 PM UTC,
ckan_admin:
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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
Abstract
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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Removed tag keywords from Milankovitch cycles in banded iron formations constrain the Earth–Moon system 2.46 billion years ago. - Data
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Added the following tags to Milankovitch cycles in banded iron formations constrain the Earth–Moon system 2.46 billion years ago. - Data
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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 2 (previously 1)
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| 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. | ||
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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: | ||
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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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| 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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| 60 | "name": "7bbbf", | 60 | "name": "7bbbf", | ||
| n | 61 | "notes": "Abstract", | n | 61 | "notes": "This file contains raw X-ray fluorescence and line scan |
| 62 | data of regular \u2018Knox cyclothem\u2019 alternations in two short | ||||
| 63 | intervals (J45de and J60d) of drill-core DD98SGP001. Core DD98SGP001 | ||||
| 64 | contains banded iron formation of the lower Paleoproterozoic Joffre | ||||
| 65 | Member of the Brockman Iron Formation and was drilled in 1998 at | ||||
| 66 | Silvergrass Peak (22\u00b003'29.9''S, 116\u00b050' 06.0''E) in the | ||||
| 67 | Hamersley Range, Western Australia; the core is currently stored at | ||||
| 68 | the Perth Core Library of the Geological Survey of Western Australia. | ||||
| 69 | The scanned interval J45de is from 289.05\u2013290.26 m depth in the | ||||
| 70 | core (box 45, rows d and e) and contains cherty iron formation-type | ||||
| 71 | cyclothems. The scanned interval 60d is from 358.34\u2013358.73 m | ||||
| 72 | depth in the core (box 60, row d) and contains shaley carbonate-type | ||||
| 73 | cyclothems.", | ||||
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| 131 | { | 143 | { | ||
| n | 132 | "display_name": "keywords", | n | 144 | "display_name": "Precambrian", |
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| 154 | "state": "active", | ||||
| 155 | "vocabulary_id": null | ||||
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| 157 | { | ||||
| 158 | "display_name": "banded iron formations", | ||||
| 159 | "id": "846efd42-fb48-405b-a9dd-67f59b72fade", | ||||
| 160 | "name": "banded iron formations", | ||||
| 161 | "state": "active", | ||||
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| 165 | "display_name": "cyclostratigraphy", | ||||
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| 137 | } | 170 | } | ||
| 138 | ], | 171 | ], | ||
| 139 | "title": "Milankovitch cycles in banded iron formations constrain | 172 | "title": "Milankovitch cycles in banded iron formations constrain | ||
| 140 | the Earth\u2013Moon system 2.46 billion years ago. - Data", | 173 | the Earth\u2013Moon system 2.46 billion years ago. - Data", | ||
| 141 | "type": "dataset", | 174 | "type": "dataset", | ||
| 142 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.bf", | 175 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.bf", | ||
| t | 143 | "version": "1" | t | 176 | "version": "2" |
| 144 | } | 177 | } |