U-Pb geochronology and geochemistry of the Torud igneous rocks: Implications for post-collision Eocene magmatism in northeast Iran
文献类型:期刊论文
作者 | Jafari, Morteza Khalatbari3; Babaie, Hassan A.2; Ao, Songjian1; Xiao, Wenjiao1,4 |
刊名 | JOURNAL OF GEODYNAMICS |
出版日期 | 2022-11-01 |
卷号 | 153-154页码:21 |
ISSN号 | 0264-3707 |
关键词 | Iran Subduction Tethys Post-collision volcanism Subvolcanic Inherited zircon |
DOI | 10.1016/j.jog.2022.101942 |
英文摘要 | New geochemical and U-Pb isotopic data from the Torud volcanic and subvolcanic rocks and their associated dikes exposed along the southern margin of the Sabzevar-Torud zone provide new evidence for Early-Middle Eocene, post-collision magmatism in northeast Iran. The 52-46 Ma (late Ypresian-Lutetian) U-Pb age interval of zircons separated from these rocks confirm the paleontological age of nummulite-bearing limestone in-terlayers. Inherited zircons separated from these igneous rocks have a much wider range of U-Pb ages that include Archean, Paleoproterozoic, Mesoproterozoic, Carboniferous, Permian, Triassic, Middle Jurassic, and Late Cretaceous. Most volcanics and subvolcanic rocks display high-K calcalkaline and shoshonitic trends. Distinct crystal fractionation patterns of the volcanic and subvolcanic rocks suggest magmatic differentiation in separate magma chambers. The studied rocks, depleted in the HFSE and enriched in the LILE, display nearly homogeneous isotopic Sr (0.7039-0.7055) and Nd (0.5126-0.5129) ratios and positive epsilon Nd values (0.08-0.56) indicating partial melting from an enriched lithospheric mantle source that was slightly contaminated with crustal material. Fluids, especially those released from the subducted slab, affected the composition of the source for the studied rocks. The magmatism occurred in the Torud area after the Late Cretaceous-Paleocene collision of the Central Iran microcontinent and Binalud-Kopeh-Dagh blocks and the Early-Middle Eocene break-off of the subducted slab. |
WOS关键词 | VOLCANIC-ROCKS ; TRACE-ELEMENT ; GEODYNAMIC EVOLUTION ; NE TURKEY ; LU-HF ; ISOTOPIC CONSTRAINTS ; LITHOSPHERIC MANTLE ; TECTONIC EVOLUTION ; MASS-SPECTROMETRY ; EASTERN PONTIDES |
资助项目 | National Natural Science Foundation of China[41822204] ; National Natural Science Foundation of China[41888101] |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
WOS记录号 | WOS:000892613000001 |
资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/107636] |
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 | Jafari, Morteza Khalatbari |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Georgia State Univ, Dept Geosci, Atlanta, GA USA 3.Res Inst Earth Sci, Azadi Sq,Meraj Ave, Tehran, Iran 4.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Jafari, Morteza Khalatbari,Babaie, Hassan A.,Ao, Songjian,et al. U-Pb geochronology and geochemistry of the Torud igneous rocks: Implications for post-collision Eocene magmatism in northeast Iran[J]. JOURNAL OF GEODYNAMICS,2022,153-154:21. |
APA | Jafari, Morteza Khalatbari,Babaie, Hassan A.,Ao, Songjian,&Xiao, Wenjiao.(2022).U-Pb geochronology and geochemistry of the Torud igneous rocks: Implications for post-collision Eocene magmatism in northeast Iran.JOURNAL OF GEODYNAMICS,153-154,21. |
MLA | Jafari, Morteza Khalatbari,et al."U-Pb geochronology and geochemistry of the Torud igneous rocks: Implications for post-collision Eocene magmatism in northeast Iran".JOURNAL OF GEODYNAMICS 153-154(2022):21. |
入库方式: OAI收割
来源:地质与地球物理研究所
浏览0
下载0
收藏0
其他版本
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。