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The Balkhash–West Junggar remnant ocean is a conspicuous tectonic feature that had an important effect on the Paleozoic tectonic evolution of the Central Asian Orogenic Belt. How the Carboniferous Balkhash–West Junggar remnant ocean was filled and closed is poorly understood. In this study, we focus on the integrated tectonic–sedimentary evolution of the Tacheng Basin, which is located in the eastern...
The Carboniferous to Permian period marks an important transition from accretion to collision in the East Junggar terrane, NW China. Field and Well Fuqian-1 well core data from the Zhaheba depression provide a better window for understanding the magmatic process during this period and its implications for the continental growth of Central Asia. Field investigations reveal structural features characterized...
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