Complex magmatic and impact history prior to 4.1Ga recorded in zircon from Apollo 17 South Massif aphanitic breccia 73235
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| Title: | Complex magmatic and impact history prior to 4.1Ga recorded in zircon from Apollo 17 South Massif aphanitic breccia 73235 |
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| Authors: | Grange, M.L.1 m.grange@curtin.edu.au, Nemchin, A.A.1,2, Timms, N.1, Pidgeon, R.T.1, Meyer, C.3 |
| Source: | Geochimica et Cosmochimica Acta. Apr2011, Vol. 75 Issue 8, p2213-2232. 20p. |
| Subjects: | Magmatism, Zircon, Crystallization, Breccia, Lunar geology, Lunar volcanism, Lunar exploration, Space vehicles |
| Abstract: | Abstract: Sample 73235 is one of several aphanitic impact melt breccias collected by the Apollo 17 mission at stations 2 and 3 on the slopes of the South Massif. This study presents a detailed investigation of internal structures and U-Pb ages of large zircon grains from this breccia sample. New data combined with the results of previous studies of zircon grains from the same location indicate that most zircon clasts in breccias from stations 2 and 3 formed during multiple magmatic events between 4.37 and 4.31Ga, although the oldest zircon crystallized at about 4.42Ga and the youngest at 4.21Ga. In addition, zircons from the aphanitic breccias record several impact events prior to the ∼3.9Ga Late Heavy Bombardment. The results indicate that the zircons probably crystallized at different locations within the Procellarum KREEEP Terrane and were later excavated and modified by several impacts and delivered to the same locality within separate ejecta blankets. This locality became a source of material that formed the aphanitic impact melt breccias of the South Massif during a ∼3.9Ga impact. However, the zircons, showing old impact features, are not modified by this ∼3.9Ga impact event suggesting that (i) this common source area was located at the periphery of excavation cavity, and (ii) the > 3.9Ga ages recorded by the zircon grains could date large (basin-forming) events as significant as major later (∼3.9Ga) collisions such as Imbrium and Serenitatis. [Copyright &y& Elsevier] |
| Copyright of Geochimica et Cosmochimica Acta is the property of Pergamon Press - An Imprint of Elsevier Science and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.) | |
| Database: | Engineering Source |
| FullText | Text: Availability: 0 |
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| Header | DbId: egs DbLabel: Engineering Source An: 59456634 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: Complex magmatic and impact history prior to 4.1Ga recorded in zircon from Apollo 17 South Massif aphanitic breccia 73235 – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Grange%2C+M%2EL%2E%22">Grange, M.L.</searchLink><relatesTo>1</relatesTo><i> m.grange@curtin.edu.au</i><br /><searchLink fieldCode="AR" term="%22Nemchin%2C+A%2EA%2E%22">Nemchin, A.A.</searchLink><relatesTo>1,2</relatesTo><br /><searchLink fieldCode="AR" term="%22Timms%2C+N%2E%22">Timms, N.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Pidgeon%2C+R%2ET%2E%22">Pidgeon, R.T.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Meyer%2C+C%2E%22">Meyer, C.</searchLink><relatesTo>3</relatesTo> – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Geochimica+et+Cosmochimica+Acta%22">Geochimica et Cosmochimica Acta</searchLink>. Apr2011, Vol. 75 Issue 8, p2213-2232. 20p. – Name: Subject Label: Subjects Group: Su Data: <searchLink fieldCode="DE" term="%22Magmatism%22">Magmatism</searchLink><br /><searchLink fieldCode="DE" term="%22Zircon%22">Zircon</searchLink><br /><searchLink fieldCode="DE" term="%22Crystallization%22">Crystallization</searchLink><br /><searchLink fieldCode="DE" term="%22Breccia%22">Breccia</searchLink><br /><searchLink fieldCode="DE" term="%22Lunar+geology%22">Lunar geology</searchLink><br /><searchLink fieldCode="DE" term="%22Lunar+volcanism%22">Lunar volcanism</searchLink><br /><searchLink fieldCode="DE" term="%22Lunar+exploration%22">Lunar exploration</searchLink><br /><searchLink fieldCode="DE" term="%22Space+vehicles%22">Space vehicles</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Abstract: Sample 73235 is one of several aphanitic impact melt breccias collected by the Apollo 17 mission at stations 2 and 3 on the slopes of the South Massif. This study presents a detailed investigation of internal structures and U-Pb ages of large zircon grains from this breccia sample. New data combined with the results of previous studies of zircon grains from the same location indicate that most zircon clasts in breccias from stations 2 and 3 formed during multiple magmatic events between 4.37 and 4.31Ga, although the oldest zircon crystallized at about 4.42Ga and the youngest at 4.21Ga. In addition, zircons from the aphanitic breccias record several impact events prior to the ∼3.9Ga Late Heavy Bombardment. The results indicate that the zircons probably crystallized at different locations within the Procellarum KREEEP Terrane and were later excavated and modified by several impacts and delivered to the same locality within separate ejecta blankets. This locality became a source of material that formed the aphanitic impact melt breccias of the South Massif during a ∼3.9Ga impact. However, the zircons, showing old impact features, are not modified by this ∼3.9Ga impact event suggesting that (i) this common source area was located at the periphery of excavation cavity, and (ii) the > 3.9Ga ages recorded by the zircon grains could date large (basin-forming) events as significant as major later (∼3.9Ga) collisions such as Imbrium and Serenitatis. [Copyright &y& Elsevier] – Name: AbstractSuppliedCopyright Label: Group: Ab Data: <i>Copyright of Geochimica et Cosmochimica Acta is the property of Pergamon Press - An Imprint of Elsevier Science and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.) |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1016/j.gca.2011.01.036 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 20 StartPage: 2213 Subjects: – SubjectFull: Magmatism Type: general – SubjectFull: Zircon Type: general – SubjectFull: Crystallization Type: general – SubjectFull: Breccia Type: general – SubjectFull: Lunar geology Type: general – SubjectFull: Lunar volcanism Type: general – SubjectFull: Lunar exploration Type: general – SubjectFull: Space vehicles Type: general Titles: – TitleFull: Complex magmatic and impact history prior to 4.1Ga recorded in zircon from Apollo 17 South Massif aphanitic breccia 73235 Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Grange, M.L. – PersonEntity: Name: NameFull: Nemchin, A.A. – PersonEntity: Name: NameFull: Timms, N. – PersonEntity: Name: NameFull: Pidgeon, R.T. – PersonEntity: Name: NameFull: Meyer, C. IsPartOfRelationships: – BibEntity: Dates: – D: 15 M: 04 Text: Apr2011 Type: published Y: 2011 Identifiers: – Type: issn-print Value: 00167037 Numbering: – Type: volume Value: 75 – Type: issue Value: 8 Titles: – TitleFull: Geochimica et Cosmochimica Acta Type: main |
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