2014
DOI: 10.1086/676478
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Neogene Source-to-Sink Relations between the Pamir and Tarim Basin: Insights from Stratigraphy, Detrital Zircon Geochronology, and Whole-Rock Geochemistry

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Cited by 31 publications
(55 citation statements)
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References 102 publications
(272 reference statements)
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“…Additional magnetostratigraphic dating in the southwestern depression of Tarim Basin confirms the chronostratigraphic division of these formations. By integrating the fossil assemblages, magnetostratigraphic dating, and detrital igneous zircon chronology (Cao et al 2014), the age uncertainty at the boundaries of each two formations should be within 1 Myr. The age uncertainties of events are within 0.5 to 1 Myr at different stratigraphic levels based on calculated results assuming the accumulation rate within each formation is invariable.…”
Section: Age Controlmentioning
confidence: 99%
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“…Additional magnetostratigraphic dating in the southwestern depression of Tarim Basin confirms the chronostratigraphic division of these formations. By integrating the fossil assemblages, magnetostratigraphic dating, and detrital igneous zircon chronology (Cao et al 2014), the age uncertainty at the boundaries of each two formations should be within 1 Myr. The age uncertainties of events are within 0.5 to 1 Myr at different stratigraphic levels based on calculated results assuming the accumulation rate within each formation is invariable.…”
Section: Age Controlmentioning
confidence: 99%
“…This indicates the upper part of the Keziluoyi Formation could have been deposited between ~20-16 Ma and the top of the Anjuan Formation roughly at 14 ± 0.5 Ma, which is in line with the result of correlated ostracods among the Tarim Basin, Junggar Basin, and Kuche Depression (Jiang et al 1995). A minimal U/Pb age of 18.3 ± 0.5 Ma for detrital zircon chronology from a sandstone bed at the base of the Anjuan Formation (Cao et al 2014) could point to a 17 ± 1 Ma age for the sampled layer considering that the time needed for zircon exhumation and transportation (Malusà et al 2009). With this respect, the boundary of the Keziluoyi and Anjuan Formations in the Qimugan section could be assigned to be 18 ± 1 Ma based on the accumulation rate in the Anjuan Formation, which is in line with the biostratigraphic estimates.…”
Section: Keziluoyi and Anjuan Formationsmentioning
confidence: 99%
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