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Qimantage Orogen as the western part of East Kunlun Mountains is located in the northeastern margin of the Tibet Plateau. In this contribution, detrital zircon age spectra combined with heavy mineral analysis of Cenozoic sediments from Qaidam Basin were applied to reveal the uplift history of Qimantage Mountains. Our results show that the Cenozoic staged uplift of the Qimantage Mountains exhibit eastward...
There are several Precambrian microcontinents in the Central Asian Orogenic Belt (CAOB). Across these microcontinents, there are many metasedimentary rocks which were not all deposited in the Precambrian. We report on a field‐based petrological and zircon geochronological study of metasedimentary rocks from the Tianshan and Beishan orogens, southern CAOB, in order to reveal the Precambrian affinity...
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