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- W1995053358 endingPage "481" @default.
- W1995053358 startingPage "471" @default.
- W1995053358 abstract "The 2.33–2.06 Ga positive δ13Ccarb excursion, associated with environmental change and the breakup of the Kenorland or Superia supercontinent, is called the Lomagundi or Jatulian Event or Great Oxidation Event, and has been reported in many Early Precambrian cratons, but not yet in the Sino-Korean craton. The Guanmenshan Formation of the Liaohe Group occurs in the northeastern part of the Sino-Korean craton. δ13Ccarb and δ18O values in 42 samples from this formation range from 3.5–5.9‰ (V-PDB), and 15.4–24.8‰ (V-SMOW), respectively, showing a clear positive δ13Ccarb excursion that characterizes the Lomagundi Event. Thirty-five of the 42 samples with less hydrothermal alteration have higher δ13Ccarb and δ18Ocarb values than the other 7 samples obviously affected by fluid flow, confirming that it was fluid flow that reduced the δ13Ccarb and δ18Ocarb values. This positive δ13Ccarb excursion places deposition of the Guanmenshan Formation within the age range of 2.33–2.06 Ga." @default.
- W1995053358 created "2016-06-24" @default.
- W1995053358 creator A5017901513 @default.
- W1995053358 creator A5047273213 @default.
- W1995053358 creator A5048842584 @default.
- W1995053358 creator A5088793158 @default.
- W1995053358 date "2011-03-01" @default.
- W1995053358 modified "2023-10-12" @default.
- W1995053358 title "Paleoproterozoic positive δ13Ccarb excursion in the northeastern Sino-Korean craton: Evidence of the Lomagundi Event" @default.
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- W1995053358 doi "https://doi.org/10.1016/j.gr.2010.07.002" @default.
- W1995053358 hasPublicationYear "2011" @default.
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