Archaean and Proterozoic crustal evolution in the Eastern Succession of the Mt Isa district, Australia: U – Pb and Hf-isotope studies of detrital zircons *

2006 ◽  
Vol 53 (1) ◽  
pp. 125-149 ◽  
Author(s):  
W. L. Griffin ◽  
E. A. Belousova ◽  
S. G. Walters ◽  
S. Y. O'Reilly
Keyword(s):  
Detrital Zircons ◽  
Hf Isotope ◽  
Crustal Evolution ◽  
Isotope Studies ◽  
Mt Isa

scholarly journals Crustal evolution of the Paleoproterozoic Birimian terranes of the Baoulé-Mossi domain, southern West African Craton: U–Pb and Hf-isotope studies of detrital zircons

2016 ◽  
Vol 274 ◽  
pp. 25-60 ◽  
Author(s):  
Luis A. Parra-Avila ◽  
Elena Belousova ◽  
Marco L. Fiorentini ◽  
Lenka Baratoux ◽  
James Davis ◽  
...  
Keyword(s):  
West African ◽  
Detrital Zircons ◽  
Hf Isotope ◽  
Crustal Evolution ◽  
West African Craton ◽  
Isotope Studies

Archean crustal evolution in the northern Yilgarn Craton: U–Pb and Hf-isotope evidence from detrital zircons

2004 ◽  
Vol 131 (3-4) ◽  
pp. 231-282 ◽  
Author(s):  
W.L. Griffin ◽  
E.A. Belousova ◽  
S.R. Shee ◽  
N.J. Pearson ◽  
S.Y. O’Reilly
Keyword(s):  
Detrital Zircons ◽  
Hf Isotope ◽  
Crustal Evolution ◽  
Yilgarn Craton ◽  
Isotope Evidence

scholarly journals Age and sources of the metasedimrntary rocks of the Tokur terrane in the Mongol-Okhotsk fold belt: results of the U–Pb geoсhronological and Lu–Hf isotope studies

2019 ◽  
Vol 486 (4) ◽  
pp. 446-450
Author(s):  
V. A. Zaika ◽  
A. A. Sorokin ◽  
A. P. Sorokin
Keyword(s):  
Detrital Zircons ◽  
Hf Isotope ◽  
Fold Belt ◽  
Metasedimentary Rocks ◽  
The North ◽  
Icp Ms ◽  
North Asia ◽  
Southeastern Margin ◽  
Isotope Studies ◽  
Metamorphic Complexes

This paper presents the results of U–Pb (LA–ICP–MS) and Lu–Hf ­isotope studies of detrital zircons from metasedimentary rocks of the Tokur Terrane. It has been shown that metasedimentary rocks of the Tokur and Ekimchan formations are characterized by similar age peaks of detrital zircons, which indicates a close (or same) age of these formations. The lower age of the sedimentation is determined by the age of the youngest zircons of 326–323 Ma. The upper age boundary is determined of 254–251 Ma, based on the intruded of the Late Permian granitoids. The main sources of zircons in the metasedimentary rocks of the Tokur Terrane are the igneous and metamorphic complexes of the southeast framing of the North Asia Craton. The Tokur Terrane can be considered as a fragment of the Paleozoic accretionary complex, the formation in front of the southeastern margin of the North Asia Craton.

Precambrian crustal evolution of the Yangtze Craton: U–Pb and Hf-isotope evidence from detrital zircons

2006 ◽  
Vol 70 (18) ◽  
pp. A366
Author(s):  
Xiaoming Liu ◽  
Shan Gao ◽  
Jin-Hui Yang ◽  
Wenli Ling ◽  
Zhaochu Hu ◽  
...  
Keyword(s):  
Detrital Zircons ◽  
Hf Isotope ◽  
Crustal Evolution ◽  
Yangtze Craton ◽  
Isotope Evidence

Implications of discordant U–Pb ages on Hf isotope studies of detrital zircons

2014 ◽  
Vol 385 ◽  
pp. 17-25 ◽  
Author(s):  
Martin Guitreau ◽  
Janne Blichert-Toft
Keyword(s):  
Detrital Zircons ◽  
Hf Isotope ◽  
Isotope Studies

Paleozoic magmatism and metamorphism in the Central Tianshan block revealed by U–Pb and Lu–Hf isotope studies of detrital zircons from the South Tianshan belt, NW China

Lithos ◽  
2015 ◽  
Vol 233 ◽  
pp. 193-208 ◽  
Author(s):  
Xiaoran Zhang ◽  
Guochun Zhao ◽  
Paul R. Eizenhöfer ◽  
Min Sun ◽  
Yigui Han ◽  
...  
Keyword(s):  
Detrital Zircons ◽  
Hf Isotope ◽  
The South ◽  
Nw China ◽  
South Tianshan ◽  
Isotope Studies
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