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Comparison of Detrital Zircon U-Pb and Muscovite$ ^{40}Ar/^{39}$Ar Ages in the Yangtze Sediment: Implications for Provenance Studies
| Content Provider | MDPI |
|---|---|
| Author | Sun, Xilin Kuiper, Klaudia F. Tian, Yuntao Li, Chang’An Zhang, Zengjie Wijbrans, Jan R. |
| Copyright Year | 2020 |
| Description | Detrital zircon U-Pb and muscovite 40Ar/39Ar dating are useful tools for investigating sediment provenance and regional tectonic histories. However, the two types of data from same sample do not necessarily give consistent results. Here, we compare published detrital muscovite 40Ar/39Ar and zircon U-Pb ages of modern sands from the Yangtze River to reveal potential factors controlling differences in their provenance age signals. Detrital muscovite 40Ar/39Ar ages of the major tributaries and main trunk suggest that the Dadu River is a dominant sediment contributor to the lower Yangtze. However, detrital zircon data suggest that the Yalong, Dadu, and Min rivers are the most important sediment suppliers. This difference could be caused by combined effects of lower reaches dilution, laser spot location on zircons and difference in closure temperature and durability between muscovite and zircon. The bias caused by sediment laser spot targeting a core or rim of zircon and zircon reworking should be considered in provenance studies. |
| Starting Page | 643 |
| e-ISSN | 2075163X |
| DOI | 10.3390/min10070643 |
| Journal | Minerals |
| Issue Number | 7 |
| Volume Number | 10 |
| Language | English |
| Publisher | MDPI |
| Publisher Date | 2020-07-20 |
| Access Restriction | Open |
| Subject Keyword | Minerals Geology Zircon U-pb Ages Muscovite 40ar/39ar Ages Sediment Provenance Yangtze River |
| Content Type | Text |
| Resource Type | Article |
