Evolution of the provenances of Triassic rocks in Franz Josef Land: U/Pb LA-ICP-MS dating of the detrital zircon from Well Severnaya

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• 作者：A. V. Soloviev (1) (6)
  A. V. Zaionchek (1) (2)
  O. I. Suprunenko (2)
  H. Brekke (3)
  J. I. Faleide (4)
  D. V. Rozhkova (1)
  A. I. Khisamutdinova (1)
  N. M. Stolbov (2)
  J. K. Hourigan (5)
  
  1. Geological Institute ; Russian Academy of Sciences ; Pyzhevskii per. 7 ; Moscow ; 119017 ; Russia
  6. Rosgeologiya OJSC ; ul. Khersonskaya 43/3 ; Moscow ; 117246 ; Russia
  2. All-Russia Research Institute of Geology and Mineral Resources of the World Ocean ; Angliiskii pr. 1 ; St. Petersburg ; 190121 ; Russia
  3. Norwegian Petroleum Directorate ; Stavanger ; Norway
  4. University of Oslo ; Oslo ; Norway
  5. Department of Earth and Planetary Sciences ; University of California ; Santa Cruz ; 1156 High Street ; Santa Cruz ; California ; 95064 ; USA
  
• 刊名：Lithology and Mineral Resources
• 出版年：2015
• 出版时间：March 2015
• 年：2015
• 卷：50
• 期：2
• 页码：102-116
• 全文大小：1,602 KB
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• 刊物类别：Earth and Environmental Science
• 刊物主题：Earth sciences
  Mineral Resources
  Mineralogy
  Sedimentology
  Russian Library of Science
  
• 出版者：MAIK Nauka/Interperiodica distributed exclusively by Springer Science+Business Media LLC.
• ISSN：1608-3229

文摘

Morphological analysis and U/Pb LA-ICP-MS dating were carried out for detrital zircon (400 age determinations) from four core samples of Triassic rocks recovered by Well Severnaya (Graham Bell Island, Franz Josef Land Archipelago). It is shown that source areas were mainly composed of peraluminous granites. U/Pb LA-ICP-MS zircon data were used to decipher the provenance evolution in the northern Barents Sea region. The main source of clastic material in the North Barents sedimentary basin in the Middle-Late Triassic was the Uralian fold belt, with lesser contribution from the East European Craton (Baltica), Timanides, Taimyr, and rocks related to the Siberian plume. The clastic material was mainly transported from the south and southeast. From the beginning of the Middle to the terminal Late Triassic, influence of the Neoproterozoic sources systematically decreased, whereas contribution of Caledonian sources increased.