First Results of Dating Detrital Zircons from the Late Precambrian Quartzite–Schist Sequences of the Chu Block (Southern Kazakhstan)

2019 ◽  
Vol 489 (1) ◽  
pp. 1273-1276 ◽  
Author(s):  
N. A. Kanygina ◽  
A. A. Tretyakov ◽  
K. E. Degtyarev ◽  
K.-N. Pang ◽  
K. L. Wahg ◽  
...  
2018 ◽  
Vol 483 (1) ◽  
pp. 1384-1387 ◽  
Author(s):  
N. A. Kanygina ◽  
E. F. Letnikova ◽  
K. E. Degtyarev ◽  
A. A. Tretyakov ◽  
F. I. Zhimulev ◽  
...  

2018 ◽  
Vol 479 (1) ◽  
pp. 320-323 ◽  
Author(s):  
N. A. Kanygina ◽  
A. A. Tretyakov ◽  
V. P. Kovach ◽  
K. E. Degtyarev ◽  
Kuo-Lun Wang ◽  
...  

2019 ◽  
Vol 489 (1) ◽  
pp. 57-61
Author(s):  
N. A. Kanygina ◽  
A. A. Tretyakov ◽  
K. E. Degtyarev ◽  
K. N. Pang ◽  
K. L. Van ◽  
...  

U-Pb geochronological studies of detrital zircons from quartzite-schist sequences of the Akbastau Formations of the Chu block (northwest of the Chu-Kendyktas terrane, Southern Kazakhstan) have been provided. The concordant ages of detrital zircons are predominantly within the intervals of 1672-2115 Ma with peaks at 1697, 1780, 1857 and 2066 Ma. Individual zircon grains display ages of 2291-2332 Ma with peaks at 2303 and 2322 Ma. Neoarchean ages 2608-2747 with peak at 2681 Ma characterize another significant zircon population. The lower limit of deposition for the Akbastau Formations of the Chu block, corresponding to the youngest statistically significant zircon population, is estimated at 1,7 billion years.


2014 ◽  
Vol 455 (1) ◽  
pp. 259-265 ◽  
Author(s):  
N. N. Kosteva ◽  
N. B. Kuznetsov ◽  
A. M. Teben’kov ◽  
T. V. Romanyuk

2012 ◽  
Vol 445 (2) ◽  
pp. 962-968 ◽  
Author(s):  
A. A. Soboleva ◽  
N. B. Kuznetsov ◽  
E. L. Miller ◽  
O. V. Udoratina ◽  
G. Gehrels ◽  
...  

2019 ◽  
Vol 485 (4) ◽  
pp. 488-492
Author(s):  
N. S. Ulyasheva ◽  
Yu. I. Pystina ◽  
A. M. Pystin ◽  
O. V. Grakova ◽  
V. B. Hubanov

The first results of U-Pb LA-SF-ICP-MS-dating of detrital zircons from terrigenous deposits of the Miniseishor suite of the Nyarovei series of the Harbei anticlinorium of the Polar Urals are presented. The series has a presumably Middle Riphean age and lies at the base of the section of the Polar Ural Upper Precambrian. The data obtained give grounds to limit the lower age interval for the formation of sediments of the Minisejshor suite abroad 660 million years ago. Allotment the Nyarovei series as a Middle Riphean straton is erroneous. Formation of the whole cut the Nyarovei series occurred in a relatively narrow age range at the end of the late Riphean. The dominant role in the formation of deposits of the entire series belonged to the products of erosion close arrays of deeply metamorphosed rocks.


2020 ◽  
Vol 494 (1) ◽  
pp. 675-679
Author(s):  
G. N. Aleksandrova ◽  
K. G. Erofeeva ◽  
N. B. Kuznetsov ◽  
T. V. Romanyuk ◽  
V. S. Sheshukov ◽  
...  

2018 ◽  
Vol 483 (1) ◽  
pp. 74-77
Author(s):  
N. Kanygina ◽  
◽  
E. Letnikova ◽  
E. Degtyarev ◽  
A. Tretyakov ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document