中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
U-Pb ages of detrital zircon and monazite from beach placers in Sri Lanka: Implications for configuration of the Columbia supercontinent

文献类型:期刊论文

作者Athira, Pendanath Gopinathan4,5; Sajeev, Krishnan5; Malaviarachchi, Sanjeewa P. K.6; George, Paul Mathews7,8; Zhai, Mingguo2; Zhou, Ligang2; Wijeratne, Gayathri K.6; Dharmapriya, Prasanna Lakshitha6; Windley, Brian F.3; Ayisha, Valiyaveettil Abdu1
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2023-08-01
卷号251页码:10
关键词Beach placers Southern Sri Lanka Zircon Monazite Provenance
ISSN号1367-9120
DOI10.1016/j.jseaes.2023.105668
英文摘要We report new U-Pb ages of zircons and monazites, and trace element chemistry combined with Hf isotopes of the zircons from beach placers on the southwest coast of Sri Lanka, in order to understand the provenance and history of crustal evolution. The zircon ages record major concentrations that range from 650-450 Ma, 1000-650 Ma to 2300-1600 Ma, and a few grains are > 2500 Ma. The primary source signature occurs at ca. 2300-1600 Ma, with significant amounts of ca. 1800 Ma ages. The Rare Earth Element patterns of older zircons support their magmatic origin. The higher percentage of Ediacaran - Late Cambrian ages are interpreted to be metamorphic, which is further supported by the monazite ages that range from 580-481 Ma. These ages provide information on the entire multiple thermal history of Sri Lanka. The monazite trace element chemistry points towards their possible derivation from garnet bearing metasedimentary rocks. The higher percentage of Paleoproterozoic ages indicate the uplifted Highland Complex of Sri Lanka was the primary source provenance. Zircon ages and Hf isotopic compositions indicate that Paleoproterozoic was the major period of crustal growth, and Neoproterozoic was the period of prominent crustal reworking in Sri Lanka. The similarity between the Paleoproterozoic age peaks of zircons with comparable Hf isotopic signatures of beach sands from Sri Lanka and southwest India suggests derivation from a similar provenance. Moreover, the ages of metasediments and magmatic rocks from Sri Lanka are comparable to those from granulite terranes in Madagascar and East Africa. The remarkably similar age distributions and Hf isotopic signatures indicate that East Africa and central Madagascar were juxtaposed from the Paleoproterozoic to the early Mesoproterozoic, when southern India and Sri Lanka were contiguous with Madagascar. Hence, the comparable Paleoproterozoic age peaks of beach sands from four contiguous terranes provide evidence on the distribution and configuration of the Columbia Supercontinent.
WOS关键词ULTRAHIGH-TEMPERATURE METAMORPHISM ; HIGHLAND COMPLEX ; VIJAYAN COMPLEX ; SOUTHERN INDIA ; HIGH-PRESSURE ; GONDWANA ; GEOCHRONOLOGY ; GRANULITES ; EVOLUTION ; PROVENANCE
资助项目Indo-Sri Lankan bilateral Research project of the Department of Science and Technology, India[DSTO/CEAS/SJK/1802] ; Ministry of Science, Technology and Research in Sri Lanka[MTR/TRD/AGR/3/2/20] ; Chinese Academy of Sciences[XDB 18030205]
WOS研究方向Geology
语种英语
WOS记录号WOS:000988643700001
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构Indo-Sri Lankan bilateral Research project of the Department of Science and Technology, India ; Indo-Sri Lankan bilateral Research project of the Department of Science and Technology, India ; Ministry of Science, Technology and Research in Sri Lanka ; Ministry of Science, Technology and Research in Sri Lanka ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Indo-Sri Lankan bilateral Research project of the Department of Science and Technology, India ; Indo-Sri Lankan bilateral Research project of the Department of Science and Technology, India ; Ministry of Science, Technology and Research in Sri Lanka ; Ministry of Science, Technology and Research in Sri Lanka ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Indo-Sri Lankan bilateral Research project of the Department of Science and Technology, India ; Indo-Sri Lankan bilateral Research project of the Department of Science and Technology, India ; Ministry of Science, Technology and Research in Sri Lanka ; Ministry of Science, Technology and Research in Sri Lanka ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Indo-Sri Lankan bilateral Research project of the Department of Science and Technology, India ; Indo-Sri Lankan bilateral Research project of the Department of Science and Technology, India ; Ministry of Science, Technology and Research in Sri Lanka ; Ministry of Science, Technology and Research in Sri Lanka ; Chinese Academy of Sciences ; Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/110925]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Athira, Pendanath Gopinathan
作者单位1.MES Ponnani Coll, Dept PG Studies & Res Geol, Ponnani, India
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
3.Univ Leicester, Sch Geog Geol & Environm, Leicester LE1 7RH, England
4.Niigata Univ, Fac Sci, Dept Geol, Ikarashi 9502181, Japan
5.Indian Inst Sci, Ctr Earth Sci, Bengaluru, India
6.Univ Peradeniya, Fac Sci, Dept Geol, Peradeniya, Sri Lanka
7.Nazarbayev Univ, Sch Min & Geosci, Astana, Kazakhstan
8.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian, Peoples R China
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Athira, Pendanath Gopinathan,Sajeev, Krishnan,Malaviarachchi, Sanjeewa P. K.,et al. U-Pb ages of detrital zircon and monazite from beach placers in Sri Lanka: Implications for configuration of the Columbia supercontinent[J]. JOURNAL OF ASIAN EARTH SCIENCES,2023,251:10.
APA Athira, Pendanath Gopinathan.,Sajeev, Krishnan.,Malaviarachchi, Sanjeewa P. K..,George, Paul Mathews.,Zhai, Mingguo.,...&Ayisha, Valiyaveettil Abdu.(2023).U-Pb ages of detrital zircon and monazite from beach placers in Sri Lanka: Implications for configuration of the Columbia supercontinent.JOURNAL OF ASIAN EARTH SCIENCES,251,10.
MLA Athira, Pendanath Gopinathan,et al."U-Pb ages of detrital zircon and monazite from beach placers in Sri Lanka: Implications for configuration of the Columbia supercontinent".JOURNAL OF ASIAN EARTH SCIENCES 251(2023):10.

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来源:地质与地球物理研究所

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