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Detrital-zircon geochronology of Paleozoic sedimentary rocks in the Hangay–Hentey basin, north-central Mongolia: Implications for the tectonic evolution of the Mongol–Okhotsk Ocean in central Asia

Tectonophysics, no. 1 (2008): 290-311

Cited: 111|Views29

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Mongol–Okhotsk OceanHangay–Hentey basinDetrital-zircon geochronologyCentral Asian Orogenic SystemCentral Asian Orogenic Belt

Abstract

Understanding the development of the Central Asian Orogenic System (CAOS), which is the largest Phanerozoic accretionary orogen in the world, is critical to the determination of continental growth mechanisms and geological history of central Asia. A key to unraveling its geological history is to ascertain the origin and tectonic setting o...More

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