Tectonic Evolution of the North Qilian Orogenic Belt from the Late Ordovician to Devonian:Evidence from Detrital Zircon Geochronology
Abstract
The Upper Ordovician-Devonian strata are distributed asymmetrically in the North Qilian orogenic belt(NQOB)and are record of the collision process between Central Qilian block and North China plate.Age spectra of detrital zircons from the Upper Ordovician strata in the eastern of belt suggest that sediments in the basement of Upper Ordovician originate from the North Qilian arc and detritus in the upper part of Ordovician come from Central...
Paper Details
Title
Tectonic Evolution of the North Qilian Orogenic Belt from the Late Ordovician to Devonian:Evidence from Detrital Zircon Geochronology
Published Date
Jan 1, 2013
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