Variations in the provenance of the late Neogene Red Clay deposits in northern China
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- 作者：Yuan Shanga ; b ; yuan.shang@helsinki.fi" class="auth_mail" title="E-mail the corresponding author ; Christiaan J. Beetsb ; c.j.beets@vu.nl" class="auth_mail" title="E-mail the corresponding author ; Hui Tanga ; 1 ; hui.tang@geo.uio.no" class="auth_mail" title="E-mail the corresponding author ; Maarten A. Prinsb ; m.a.prins@vu.nl" class="auth_mail" title="E-mail the corresponding author ; Yann Lahayec ; yann.lahaye@gtk.fi" class="auth_mail" title="E-mail the corresponding author ; Roel van Elsasb ; r.van.elsas@vu.nl" class="auth_mail" title="E-mail the corresponding author ; Leena Sukselainena ; leena.sukselainen@gmail.com" class="auth_mail" title="E-mail the corresponding author ; Anu Kaakinena ; anu.kaakinen@helsinki.fi" class="auth_mail" title="E-mail the corresponding author
- 关键词：detrital zircon ; U&ndash ; Pb geochronology ; end-member modelling ; backtrace trajectory modelling ; Winter monsoon ; Chinese Loess Plateau
- 刊名：Earth and Planetary Science Letters
- 出版年：2016
- 出版时间：1 April 2016
- 年：2016
- 卷：439
- 期：Complete
- 页码：88-100
- 全文大小：1901 K
文摘
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An integrated approach constrains the provenance of the Red Clay deposits.
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End-member modelling demonstrates spatiotemporal heterogeneity of the Red Clays.
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Late Miocene dust trajectories were modelled for the studied localities.
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U–Pb age spectra suggest differing source areas for the northeastern and southern sites.
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Zircon ages suggest increased component from western China since the middle Pliocene.