PALEOTECTONIC AND PALEOGEOGRAPHIC CONDITIONS FOR THE ACCUMULATION OF THE LOWER RIPHEAN AI FORMATION IN THE BASHKIR UPLIFT (SOUTHERN URALS): THE TERRANECHRONE® DETRITAL ZIRCON STUDY

PALEOTECTONIC AND PALEOGEOGRAPHIC CONDITIONS FOR THE ACCUMULATION OF THE LOWER RIPHEAN AI FORMATION IN THE BASHKIR UPLIFT (SOUTHERN URALS): THE TERRANECHRONE® DETRITAL ZIRCON STUDY

The TerraneChrone® (LA-ICP-MS) technique has been applied to carry out an integrated study of detrital zircons in sandstones sampled from the basal horizons of the stratotypical Riphean sequence in the Southern Urals, specifically the Navysh and Chudin suites of the Ai Formation of the Burzyan Group...

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Bibliographic Details
Main Authors: T. V. Romanyuk, N. B. Kuznetsov, E. A. Belousova, V. M. Gorozhanin, E. N. Gorozhanina
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2018-03-01
Series:Геодинамика и тектонофизика
Subjects:
bashkir uplift
lower riphean
detrital zircons
terranechrone® technique
navysh graben
kama-belaya aulacogen
carbonatites
supercontinent columbia
Online Access:https://www.gt-crust.ru/jour/article/view/518
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