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Article: Geochemistry, Geochronology, and Hf isotopic Composition of the Late Paleoproterozoic Lujiapuzi Formation, NE Yan-Liao Rift, Northern Liaoning

TitleGeochemistry, Geochronology, and Hf isotopic Composition of the Late Paleoproterozoic Lujiapuzi Formation, NE Yan-Liao Rift, Northern Liaoning
Authors
KeywordsChangcheng System
crustal growth
detrital zircon
North China Craton
Yan-Liao rift
Issue Date2018
Citation
Acta Geologica Sinica (English Edition), 2018, v. 92, n. 6, p. 2136-2156 How to Cite?
AbstractThe metasedimentary Lujiapuzi Formation crops out along the northeastern margin of the North China Craton, close to the Yan-Liao Rift. The age and tectonic setting of the formation, and its relationship with the Yan-Liao Rift are currently unclear. Here we present detrital zircon U-Pb ages, and Hf isotopic and geochemical data for the Lujiapuzi Formation to constrain the timing of deposition, the provenance of the formation, and the regional stratigraphy relationship. Zircon U-Pb dating constrains the timing of deposition of the Lujiapuzi Formation to younger than 1780 Ma, and indicates that most grains were sourced from the Longgang Block and the Paleoproterozoic Liao-Ji Belt. Detailed field investigations and a correlation of the regional stratigraphy reveal that much of the Lujiapuzi Formation is equivalent to the Tuanshanzi Formation in the Yan-Liao Rift; the lower section may represent the earliest sediments deposited within the Fanhe Basin. Based on these results and the findings of previous studies, we suggest that the base of the Changcheng System has an age of 1.80 Ga. Zircon Hf isotopic data indicate that the main period of crustal growth along the northeastern margin of the North China Craton occurred at 3.2–2.5 Ga, with a peak at 2.9–2.7 Ga.
Persistent Identifierhttp://hdl.handle.net/10722/327215
ISSN
2023 Impact Factor: 3.5
2023 SCImago Journal Rankings: 0.505
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorLiu, Jin-
dc.contributor.authorZhang, Jian-
dc.contributor.authorLiu, Zhenghong-
dc.contributor.authorYin, Changqing-
dc.contributor.authorZhao, Chen-
dc.contributor.authorPeng, Youbo-
dc.contributor.authorDou, Shiyong-
dc.contributor.authorYang, Zhongjie-
dc.date.accessioned2023-03-31T05:29:46Z-
dc.date.available2023-03-31T05:29:46Z-
dc.date.issued2018-
dc.identifier.citationActa Geologica Sinica (English Edition), 2018, v. 92, n. 6, p. 2136-2156-
dc.identifier.issn1000-9515-
dc.identifier.urihttp://hdl.handle.net/10722/327215-
dc.description.abstractThe metasedimentary Lujiapuzi Formation crops out along the northeastern margin of the North China Craton, close to the Yan-Liao Rift. The age and tectonic setting of the formation, and its relationship with the Yan-Liao Rift are currently unclear. Here we present detrital zircon U-Pb ages, and Hf isotopic and geochemical data for the Lujiapuzi Formation to constrain the timing of deposition, the provenance of the formation, and the regional stratigraphy relationship. Zircon U-Pb dating constrains the timing of deposition of the Lujiapuzi Formation to younger than 1780 Ma, and indicates that most grains were sourced from the Longgang Block and the Paleoproterozoic Liao-Ji Belt. Detailed field investigations and a correlation of the regional stratigraphy reveal that much of the Lujiapuzi Formation is equivalent to the Tuanshanzi Formation in the Yan-Liao Rift; the lower section may represent the earliest sediments deposited within the Fanhe Basin. Based on these results and the findings of previous studies, we suggest that the base of the Changcheng System has an age of 1.80 Ga. Zircon Hf isotopic data indicate that the main period of crustal growth along the northeastern margin of the North China Craton occurred at 3.2–2.5 Ga, with a peak at 2.9–2.7 Ga.-
dc.languageeng-
dc.relation.ispartofActa Geologica Sinica (English Edition)-
dc.subjectChangcheng System-
dc.subjectcrustal growth-
dc.subjectdetrital zircon-
dc.subjectNorth China Craton-
dc.subjectYan-Liao rift-
dc.titleGeochemistry, Geochronology, and Hf isotopic Composition of the Late Paleoproterozoic Lujiapuzi Formation, NE Yan-Liao Rift, Northern Liaoning-
dc.typeArticle-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1111/1755-6724.13720-
dc.identifier.scopuseid_2-s2.0-85059091887-
dc.identifier.volume92-
dc.identifier.issue6-
dc.identifier.spage2136-
dc.identifier.epage2156-
dc.identifier.eissn1755-6724-
dc.identifier.isiWOS:000454419700006-

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