U-Pb geochronology and geochemistry of the Torud igneous rocks: Implications for post-collision Eocene magmatism in northeast Iran

IF 2.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Morteza Khalatbari Jafari , Hassan A. Babaie , Songjian Ao , Wenjiao Xiao
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Abstract

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 interlayers. 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 ɛNd 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.

伊朗东北部托鲁德火成岩的U-Pb年代学和地球化学:对碰撞后始新世岩浆活动的启示
Sabzevar-Torud带南缘Torud火山岩和次火山岩及其伴生岩脉的地球化学和U-Pb同位素资料为伊朗东北部早中始新世碰撞后岩浆活动提供了新的证据。从这些岩石中分离出的锆石的52 ~ 46 Ma(晚伊普勒世—鲁特世)U-Pb年龄区间证实了含麻榴石灰岩夹层的古生物年龄。从这些火成岩中分离出来的继承锆石的U-Pb年龄范围更广,包括太古宙、古元古代、中元古代、石炭系、二叠纪、三叠纪、中侏罗世和晚白垩世。大部分火山岩和次火山岩表现出高钾碱性和高钾玄武性倾向。火山岩和次火山岩的晶体分异模式表明岩浆分异存在于不同的岩浆房中。研究的岩石表现出同位素Sr(0.7039 ~ 0.7055)和Nd(0.5126 ~ 0.5129)比值接近均匀的特征,并呈现出正的Nd值(0.08 ~ 0.56),表明其部分熔融来自富集的岩石圈地幔源,受地壳物质的轻微污染。流体,特别是从俯冲板块中释放出来的流体,影响了所研究岩石源的组成。Torud地区岩浆活动发生在伊朗中部微大陆与Binalud-Kopeh-Dagh地块晚白垩世-古新世碰撞和早中始新世俯冲板块断裂之后。
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来源期刊
Journal of Geodynamics
Journal of Geodynamics 地学-地球化学与地球物理
CiteScore
4.60
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: The Journal of Geodynamics is an international and interdisciplinary forum for the publication of results and discussions of solid earth research in geodetic, geophysical, geological and geochemical geodynamics, with special emphasis on the large scale processes involved.
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