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10.1371/journal.pone.0144727

http://scihub22266oqcxt.onion/10.1371/journal.pone.0144727
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C4682852!4682852!26658165
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pmid26658165      PLoS+One 2015 ; 10 (12): ä
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  • 1 8 Billion Years of Detrital Zircon Recycling Calibrates a Refractory Part of Earth?s Sedimentary Cycle #MMPMID26658165
  • Hadlari T; Swindles GT; Galloway JM; Bell KM; Sulphur KC; Heaman LM; Beranek LP; Fallas KM
  • PLoS One 2015[]; 10 (12): ä PMID26658165show ga
  • Detrital zircon studies are providing new insights on the evolution of sedimentary basins but the role of sedimentary recycling remains largely undefined. In a broad region of northwestern North America, this contribution traces the pathway of detrital zircon sand grains from Proterozoic sandstones through Phanerozoic strata and argues for multi-stage sedimentary recycling over more than a billion years. As a test of our hypothesis, integrated palynology and detrital zircon provenance provides clear evidence for erosion of Carboniferous strata in the northern Cordillera as a sediment source for Upper Cretaceous strata. Our results help to calibrate Earth's sedimentary cycle by showing that recycling dominates sedimentary provenance for the refractory mineral zircon.
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