Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1144/jgs2018-125 |
Unravelling the Neoproterozoic accretionary history of Oman, using an array of isotopic systems in zircon | |
Blades, M. L.1; Alessio, B. L.1; Collins, A. S.1; Foden, J.1; Payne, J. L.2; Glorie, S.1; Holden, P.4; Thorpe, B.1; Al-Khirbash, S.3 | |
通讯作者 | Blades, M. L. |
来源期刊 | JOURNAL OF THE GEOLOGICAL SOCIETY
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ISSN | 0016-7649 |
EISSN | 2041-479X |
出版年 | 2020 |
卷号 | 177期号:2页码:357-378 |
英文摘要 | The Omani basement is a critical window into the Neoproterozoic tectonic geography of the Mozambique Ocean and the amalgamation of Gondwana. It is located east of the juvenile arc terranes of the Arabian-Nubian Shield, yet the relationship between the two is not well understood. Magmatic and detrital zircon samples were analysed from four main basement terranes: Mirbat, the Huqf, Jebel Ja'alan and Al Jobah. The U-Pb (zircon) ages from igneous samples give ages between 838 and 765 Ma. The Lu-Hf and oxygen isotopes show that the zircons are juvenile (epsilon(Hf)(t) values 10.5-8.7), with low delta O-18 values (c. 2-6 parts per thousand). Detritus from sediments in Mirbat, the southernmost basement outcrop, preserves a main age peak at c. 786 Ma, with Lu-Hf between +6.05 and +12.64. Lu-Hf isotopic data for Proterozoic detrital zircons from Jebel Ja'alan suggest that this region was depositionally connected to a source yielding both evolved Tonian and Neoarchean to Paleoproterozoic detritus. These sources could correlate to the terranes in India and South China, which record similarly low delta O-18 values. These data support a model in which Oman formed in its own tectonic domain, accreting onto the Neoproterozoic active margin of a continent. |
类型 | Article |
语种 | 英语 |
国家 | Australia ; Oman |
收录类别 | SCI-E |
WOS记录号 | WOS:000537276100009 |
WOS关键词 | U-PB ZIRCON ; ARABIAN-NUBIAN SHIELD ; HUQF SUPERGROUP ; CRUSTAL EVOLUTION ; EASTERN DESERT ; FIQ GLACIATION ; SINGLE ZIRCONS ; KHIDA TERRANE ; BILLION YEARS ; MIRBAT AREA |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/318855 |
作者单位 | 1.Univ Adelaide, Ctr Tecton Resources & Explorat TRaX, Dept Earth Sci, Adelaide, SA 5005, Australia; 2.Univ South Australia, Ctr Tecton Resources & Explorat TRaX, Sch Built & Nat Environm, Adelaide, SA 5001, Australia; 3.Sultan Qaboos Univ, Muscat, Oman; 4.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia |
推荐引用方式 GB/T 7714 | Blades, M. L.,Alessio, B. L.,Collins, A. S.,et al. Unravelling the Neoproterozoic accretionary history of Oman, using an array of isotopic systems in zircon[J],2020,177(2):357-378. |
APA | Blades, M. L..,Alessio, B. L..,Collins, A. S..,Foden, J..,Payne, J. L..,...&Al-Khirbash, S..(2020).Unravelling the Neoproterozoic accretionary history of Oman, using an array of isotopic systems in zircon.JOURNAL OF THE GEOLOGICAL SOCIETY,177(2),357-378. |
MLA | Blades, M. L.,et al."Unravelling the Neoproterozoic accretionary history of Oman, using an array of isotopic systems in zircon".JOURNAL OF THE GEOLOGICAL SOCIETY 177.2(2020):357-378. |
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