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  • Paul R. EizenhöferEmail author
Chapter
Part of the Springer Theses book series (Springer Theses)

Abstract

The 1694 U–Pb ages of detrital zircons from Permian arc basins of the accretionary collision zone between the Mongolian Arcs and the North China Craton exhibit a wide age range, from Neoarchean (ca. 2.5 Ga) to Late Permian (ca. 269 Ma), with major age populations around ca. 2.5 Ga, ca. 1.8 Ga, ca. 436 Ma, ca. 314 Ma and ca. 269 Ma (Figs. 4.1 and 4.2a).

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© Springer Nature Singapore Pte Ltd. 2020

Authors and Affiliations

  1. 1.Department of GeosciencesUniversity of TübingenTübingenGermany

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