The heterogeneous orogenic lithospheric mantle: whole rock and mineral geochemical evidence from early Paleozoic mafic intrusives in the Qilian orogen, China.
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| Title: | The heterogeneous orogenic lithospheric mantle: whole rock and mineral geochemical evidence from early Paleozoic mafic intrusives in the Qilian orogen, China. |
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| Authors: | Chen, Qi1 (AUTHOR), Dai, Li-Qun1,2,3 (AUTHOR) lqdai@ustc.edu.cn, Zhao, Zi-Fu1,2,3 (AUTHOR) zfzhao@ustc.edu.cn, Zheng, Yong-Fei1,2 (AUTHOR), Zhou, Yao1 (AUTHOR) |
| Source: | Contributions to Mineralogy & Petrology. Nov2022, Vol. 177 Issue 11, p1-21. 21p. |
| Subjects: | Regolith, Mafic rocks, Subduction zones, Igneous rocks, Strontium isotopes, Minerals, Orogenic belts |
| Geographic Terms: | China |
| Abstract: | Mantle heterogeneity is caused by recycling of crustal materials into the mantle, and mafic arc magmatism provides important imformation on the nature of crust–mantle interaction. Here we undertake an integrated study of whole rock major-trace elements and Sr–Nd–Hf isotopes, in-situ zircon U–Pb ages and Hf–O isotopes as well as mineral major-trace elements and clinopyroxene Sr isotopes for mafic intrusives in the Qilian orogen. The studied Jinyuan and Jishishan mafic igneous rocks show consistent zircon U–Pb ages of ca. 448–450 Ma. They all display arc-like trace element distribution patterns, relatively depleted Sr–Nd isotope compositions, and variably high zircon O isotopes. In comparison, the Jinyuan mafic igneous rocks have less depleted Sr–Nd–Hf and higher O isotope compositions than the Jishishan mafic rocks. These geochemicial features indicate they originated from a heterogeneous orogenic lithospheric mantle source, which resulted from the incorporation of variable crustal materials into the mantle. Model calculations confirm that the heterogeneous mantle source would be generated by reaction of the mantle wedge peridotite with different proportions of the subducting Proto–Tethyan oceanic crust-derived aqueous solutions and sediment-derived hydrous melts. Partial melting of the heterogeneous mantle source would generate different batches of mafic melts, which led to magma mixing and recharge processes prior to emplacement as evidenced by mineral compositional zonings. Therefore, in addition to heterogeneous crust–mantle interaction during oceanic subduction, magmatic processes such as magma recharge and mixing may also contribute to the petrogenesis of arc igneous rocks above the oceanic subduction zone. [ABSTRACT FROM AUTHOR] |
| Copyright of Contributions to Mineralogy & Petrology is the property of Springer Nature 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 |
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| Header | DbId: egs DbLabel: Engineering Source An: 160707088 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: The heterogeneous orogenic lithospheric mantle: whole rock and mineral geochemical evidence from early Paleozoic mafic intrusives in the Qilian orogen, China. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Chen%2C+Qi%22">Chen, Qi</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Dai%2C+Li-Qun%22">Dai, Li-Qun</searchLink><relatesTo>1,2,3</relatesTo> (AUTHOR)<i> lqdai@ustc.edu.cn</i><br /><searchLink fieldCode="AR" term="%22Zhao%2C+Zi-Fu%22">Zhao, Zi-Fu</searchLink><relatesTo>1,2,3</relatesTo> (AUTHOR)<i> zfzhao@ustc.edu.cn</i><br /><searchLink fieldCode="AR" term="%22Zheng%2C+Yong-Fei%22">Zheng, Yong-Fei</searchLink><relatesTo>1,2</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Zhou%2C+Yao%22">Zhou, Yao</searchLink><relatesTo>1</relatesTo> (AUTHOR) – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Contributions+to+Mineralogy+%26+Petrology%22">Contributions to Mineralogy & Petrology</searchLink>. Nov2022, Vol. 177 Issue 11, p1-21. 21p. – Name: Subject Label: Subjects Group: Su Data: <searchLink fieldCode="DE" term="%22Regolith%22">Regolith</searchLink><br /><searchLink fieldCode="DE" term="%22Mafic+rocks%22">Mafic rocks</searchLink><br /><searchLink fieldCode="DE" term="%22Subduction+zones%22">Subduction zones</searchLink><br /><searchLink fieldCode="DE" term="%22Igneous+rocks%22">Igneous rocks</searchLink><br /><searchLink fieldCode="DE" term="%22Strontium+isotopes%22">Strontium isotopes</searchLink><br /><searchLink fieldCode="DE" term="%22Minerals%22">Minerals</searchLink><br /><searchLink fieldCode="DE" term="%22Orogenic+belts%22">Orogenic belts</searchLink> – Name: SubjectGeographic Label: Geographic Terms Group: Su Data: <searchLink fieldCode="DE" term="%22China%22">China</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Mantle heterogeneity is caused by recycling of crustal materials into the mantle, and mafic arc magmatism provides important imformation on the nature of crust–mantle interaction. Here we undertake an integrated study of whole rock major-trace elements and Sr–Nd–Hf isotopes, in-situ zircon U–Pb ages and Hf–O isotopes as well as mineral major-trace elements and clinopyroxene Sr isotopes for mafic intrusives in the Qilian orogen. The studied Jinyuan and Jishishan mafic igneous rocks show consistent zircon U–Pb ages of ca. 448–450 Ma. They all display arc-like trace element distribution patterns, relatively depleted Sr–Nd isotope compositions, and variably high zircon O isotopes. In comparison, the Jinyuan mafic igneous rocks have less depleted Sr–Nd–Hf and higher O isotope compositions than the Jishishan mafic rocks. These geochemicial features indicate they originated from a heterogeneous orogenic lithospheric mantle source, which resulted from the incorporation of variable crustal materials into the mantle. Model calculations confirm that the heterogeneous mantle source would be generated by reaction of the mantle wedge peridotite with different proportions of the subducting Proto–Tethyan oceanic crust-derived aqueous solutions and sediment-derived hydrous melts. Partial melting of the heterogeneous mantle source would generate different batches of mafic melts, which led to magma mixing and recharge processes prior to emplacement as evidenced by mineral compositional zonings. Therefore, in addition to heterogeneous crust–mantle interaction during oceanic subduction, magmatic processes such as magma recharge and mixing may also contribute to the petrogenesis of arc igneous rocks above the oceanic subduction zone. [ABSTRACT FROM AUTHOR] – Name: AbstractSuppliedCopyright Label: Group: Ab Data: <i>Copyright of Contributions to Mineralogy & Petrology is the property of Springer Nature 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: 10.1007/s00410-022-01970-1 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 21 StartPage: 1 Subjects: – SubjectFull: Regolith Type: general – SubjectFull: Mafic rocks Type: general – SubjectFull: Subduction zones Type: general – SubjectFull: Igneous rocks Type: general – SubjectFull: Strontium isotopes Type: general – SubjectFull: Minerals Type: general – SubjectFull: Orogenic belts Type: general – SubjectFull: China Type: general Titles: – TitleFull: The heterogeneous orogenic lithospheric mantle: whole rock and mineral geochemical evidence from early Paleozoic mafic intrusives in the Qilian orogen, China. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Chen, Qi – PersonEntity: Name: NameFull: Dai, Li-Qun – PersonEntity: Name: NameFull: Zhao, Zi-Fu – PersonEntity: Name: NameFull: Zheng, Yong-Fei – PersonEntity: Name: NameFull: Zhou, Yao IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 11 Text: Nov2022 Type: published Y: 2022 Identifiers: – Type: issn-print Value: 00107999 Numbering: – Type: volume Value: 177 – Type: issue Value: 11 Titles: – TitleFull: Contributions to Mineralogy & Petrology Type: main |
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