中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
New detrital zircon U-Pb insights on the palaeogeographic origin of the central Sanandaj-Sirjan zone, Iran

文献类型:期刊论文

作者Shakerardakani, Farzaneh2,3,5; Neubauer, Franz3; Liu, Xiaoming6; Dong, Yunpeng6; Monfaredi, Behzad4; Li, Xian-Hua1,2,5
刊名GEOLOGICAL MAGAZINE
出版日期2021-12-01
卷号158期号:12页码:2165-2186
关键词Iranian microcontinent Sanandaj-Sirjan metamorphic zone U-Pb geochronology detrital zircon North Gondwana palaeobiogeography
ISSN号0016-7568
DOI10.1017/S0016756821000728
英文摘要New detrital U-Pb zircon ages from the Sanandaj-Sirjan metamorphic zone in the Zagros orogenic belt allow discussion of models of the late Neoproterozoic to early Palaeozoic plate tectonic evolution and position of the Iranian microcontinent within a global framework. A total of 194 valid age values from 362 zircon grains were obtained from three garnet-micaschist samples. The most abundant detrital zircon population included Ediacaran ages, with the main age peak at 0.60 Ga. Other significant age peaks are at c. 0.64-0.78 Ga, 0.80-0.91 Ga, 0.94-1.1 Ga, 1.8-2.0 Ga and 2.1-2.5 Ga. The various Palaeozoic zircon age peaks could be explained by sediment supply from sources within the Iranian microcontinent. However, Precambrian ages were found, implying a non-Iranian provenance or recycling of upper Ediacaran-Palaeozoic clastic rocks. Trace-element geochemical fingerprints show that most detrital zircons were sourced from continental magmatic settings. In this study, the late Grenvillian age population at c. 0.94-1.1 Ga is used to unravel the palaeogeographic origin of the Sanandaj-Sirjan metamorphic zone. This Grenvillian detrital age population relates to the 'Gondwana superfan' sediments, as found in many Gondwana-derived terranes within the European Variscides and Turkish terranes, but also to units further east, e.g. in the South China block. Biogeographic evidence proves that the Iranian microcontinent developed on the same North Gondwana margin extending from the South China block via Iran further to the west.
WOS关键词ARABIAN-NUBIAN SHIELD ; EDIACARAN-CAMBRIAN TRANSITION ; SOUTH CHINA CONSTRAINTS ; ZAGROS OROGENIC BELT ; TRACE-ELEMENT ; NW IRAN ; TECTONIC EVOLUTION ; EASTERN DESERT ; YANGTZE BLOCK ; HF ISOTOPES
资助项目Afro-Asiatisches Institut Salzburg at the Salzburg University ; Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences[XDB18030300]
WOS研究方向Geology
语种英语
WOS记录号WOS:000717139300007
出版者CAMBRIDGE UNIV PRESS
资助机构Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Afro-Asiatisches Institut Salzburg at the Salzburg University ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences ; Strategic Priority Research Programme (B) of the Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/103809]  
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Shakerardakani, Farzaneh
作者单位1.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Paris Lodron Univ Salzburg, Dept Geog & Geol, Hellbrunner Str 34, A-5020 Salzburg, Austria
4.Karl Franzens Univ Graz, NAWI Graz Geoctr, Inst Earth Sci, Univ Pl 2, A-8010 Graz, Austria
5.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
6.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Northern Taibai Str 229, Xian 710069, Peoples R China
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Shakerardakani, Farzaneh,Neubauer, Franz,Liu, Xiaoming,et al. New detrital zircon U-Pb insights on the palaeogeographic origin of the central Sanandaj-Sirjan zone, Iran[J]. GEOLOGICAL MAGAZINE,2021,158(12):2165-2186.
APA Shakerardakani, Farzaneh,Neubauer, Franz,Liu, Xiaoming,Dong, Yunpeng,Monfaredi, Behzad,&Li, Xian-Hua.(2021).New detrital zircon U-Pb insights on the palaeogeographic origin of the central Sanandaj-Sirjan zone, Iran.GEOLOGICAL MAGAZINE,158(12),2165-2186.
MLA Shakerardakani, Farzaneh,et al."New detrital zircon U-Pb insights on the palaeogeographic origin of the central Sanandaj-Sirjan zone, Iran".GEOLOGICAL MAGAZINE 158.12(2021):2165-2186.

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来源:地质与地球物理研究所

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