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Evidence from Late Cretaceous-Paleogene volcanic rocks of the Kyrenia Range, northern Cyprus for the northern, active continental margin of the Southern Neotethys

文献类型:期刊论文

作者Chen, Guohui1,2; Robertson, Alastair H. F.1
刊名LITHOS
出版日期2021
卷号380页码:20
关键词Late Cretaceous-Paleogene Volcanic rocks Kyrenia Range Arc magmatism Marginal basin formation Southern Neotethys
ISSN号0024-4937
DOI10.1016/j.lithos.2020.105835
英文摘要Late Cretaceous felsic and latest Cretaceous-Paleogene basaltic volcanic rocks are exposed throughout the Kyrenia Range, N Cyprus. Field mapping of the key, well-exposed western range indicates that the felsic volcanics mainly crop out in the southerly, frontal part of the range, separated from the latest Cretaceous-Paleogene basaltic volcanics farther north by a thrust. New U-Pb zircon dating of the felsic volcanics indicates a primary age of c. 74.0 Ma (Late Campanian). The felsic volcanics are characterised by evolved compositions that were probably generated in an extensional subduction-related setting. Their relatively low Nb and Y but high Rb concentrations, together with characteristic Th/Ta ratios (6-20), suggest a mature continental arc setting. The latest Cretaceous Paleogene basaltic volcanics have mainly within-plate chemical characteristics (in the east), although some have a subordinate subduction influence; e.g. negative Nb (in the west). Sr-Nd-Hf isotopic signatures (i.e. high positive epsilon Nd(t) and epsilon Hf(t) values) suggest derivation of the basalts from several OIB-like mantle sources, with probable involvement of a crustal (recycled) component (i.e. elevated Nb/Y ratios). Comparisons with SE Turkey, where Late Cretaceous arc-related granitic rocks are widely developed, suggest that the Kyrenia Range igneous rocks may have originated to the south of the Alanya metamorphic massif (N of Cyprus) and correlative continental units in SE Turkey. The latest Cretaceous-Paleogene basaltic volcanics in N Cyprus and SE Turkey (Maden Complex) are interpreted to represent incipient marginal basin formation, possibly in an oblique-convergent setting, prior to Miocene suturing with Arabia. In the light of alternatives, we infer genesis of the N Cyprus Late Cretaceous and Paleogene volcanic rocks related to stages in the development of the northerly active continental margin of the Southern Neotethys. (C) 2020 Elsevier B.V. All rights reserved.
WOS关键词ANATOLIAN OROGENIC BELT ; TRACE-ELEMENT ; U-PB ; TECTONIC EVOLUTION ; CLINOPYROXENE COMPOSITION ; GEOCHRONOGICAL EVIDENCE ; GEOLOGICAL EVOLUTION ; KANNAVIOU FORMATION ; TROODOS MICROPLATE ; OPHIOLITIC ROCKS
资助项目Principal's Career Development PhD Scholarship ; Edinburgh Global Research Scholarship ; Natural Environment Research Council Ion Microprobe Facility ; International Association of Sedimentologists ; Mineralogical Society of Great Britain and Ireland ; Edinburgh Geological Society ; John Dixon Memorial Fund
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
WOS记录号WOS:000612245000002
出版者ELSEVIER
资助机构Principal's Career Development PhD Scholarship ; Principal's Career Development PhD Scholarship ; Edinburgh Global Research Scholarship ; Edinburgh Global Research Scholarship ; Natural Environment Research Council Ion Microprobe Facility ; Natural Environment Research Council Ion Microprobe Facility ; International Association of Sedimentologists ; International Association of Sedimentologists ; Mineralogical Society of Great Britain and Ireland ; Mineralogical Society of Great Britain and Ireland ; Edinburgh Geological Society ; Edinburgh Geological Society ; John Dixon Memorial Fund ; John Dixon Memorial Fund ; Principal's Career Development PhD Scholarship ; Principal's Career Development PhD Scholarship ; Edinburgh Global Research Scholarship ; Edinburgh Global Research Scholarship ; Natural Environment Research Council Ion Microprobe Facility ; Natural Environment Research Council Ion Microprobe Facility ; International Association of Sedimentologists ; International Association of Sedimentologists ; Mineralogical Society of Great Britain and Ireland ; Mineralogical Society of Great Britain and Ireland ; Edinburgh Geological Society ; Edinburgh Geological Society ; John Dixon Memorial Fund ; John Dixon Memorial Fund ; Principal's Career Development PhD Scholarship ; Principal's Career Development PhD Scholarship ; Edinburgh Global Research Scholarship ; Edinburgh Global Research Scholarship ; Natural Environment Research Council Ion Microprobe Facility ; Natural Environment Research Council Ion Microprobe Facility ; International Association of Sedimentologists ; International Association of Sedimentologists ; Mineralogical Society of Great Britain and Ireland ; Mineralogical Society of Great Britain and Ireland ; Edinburgh Geological Society ; Edinburgh Geological Society ; John Dixon Memorial Fund ; John Dixon Memorial Fund ; Principal's Career Development PhD Scholarship ; Principal's Career Development PhD Scholarship ; Edinburgh Global Research Scholarship ; Edinburgh Global Research Scholarship ; Natural Environment Research Council Ion Microprobe Facility ; Natural Environment Research Council Ion Microprobe Facility ; International Association of Sedimentologists ; International Association of Sedimentologists ; Mineralogical Society of Great Britain and Ireland ; Mineralogical Society of Great Britain and Ireland ; Edinburgh Geological Society ; Edinburgh Geological Society ; John Dixon Memorial Fund ; John Dixon Memorial Fund
源URL[http://ir.iggcas.ac.cn/handle/132A11/100111]  
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Chen, Guohui
作者单位1.Univ Edinburgh, Sch GeoSci, West Mains Rd, Edinburgh EH9 3JW, Midlothian, Scotland
2.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, POB 9825, Beijing 100029, Peoples R China
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GB/T 7714
Chen, Guohui,Robertson, Alastair H. F.. Evidence from Late Cretaceous-Paleogene volcanic rocks of the Kyrenia Range, northern Cyprus for the northern, active continental margin of the Southern Neotethys[J]. LITHOS,2021,380:20.
APA Chen, Guohui,&Robertson, Alastair H. F..(2021).Evidence from Late Cretaceous-Paleogene volcanic rocks of the Kyrenia Range, northern Cyprus for the northern, active continental margin of the Southern Neotethys.LITHOS,380,20.
MLA Chen, Guohui,et al."Evidence from Late Cretaceous-Paleogene volcanic rocks of the Kyrenia Range, northern Cyprus for the northern, active continental margin of the Southern Neotethys".LITHOS 380(2021):20.

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来源:地质与地球物理研究所

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