δ13C and 87Sr/86Sr signatures from carbonates of the Morar Formation, Gwalior Group: Implications towards depositional setting and Paleoproterozoic seawater chemistry
Author:
Funder
Council of Scientific and Industrial Research, India
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12040-022-01970-6.pdf
Reference55 articles.
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2. Banner J L and Kaufman J 1994 The isotopic record of ocean chemistry and diagenesis preserved in non-luminescent brachiopods from Mississippian carbonate rocks, Illinois and Missouri; Geol. Soc. Am. Bull. 106(8) 1074–1082, https://doi.org/10.1130/0016-7606(1994)106%3c1074:TIROOC%3e2.3.CO;2.
3. Beeunas M A and Knauth L P 1985 Preserved stable isotopic signature of subaerial diagenesis in the 1.2-by Mescal Limestone, central Arizona: Implications for the timing and development of a terrestrial plant cover; Geol. Soc. Am. Bull. 96(6) 737–745, https://doi.org/10.1130/0016-7606(1985)96<737:PSISOS>2.0.CO;2.
4. Bekker A, Karhu J A, Eriksson K A and Kaufman A J 2003 Chemostratigraphy of Paleoproterozoic carbonate successions of the Wyoming Craton: Tectonic forcing of biogeochemical change?; Precamb. Res. 120(3–4) 279–325.
5. Bekker A, Slack J F, Planavsky N, Krapez B, Hofmann A, Konhauser K O and Rouxel O J 2010 Iron formation: The sedimentary product of a complex interplay among mantle, tectonic, oceanic, and biospheric processes; Econ. Geol. 105(3) 467–508, https://doi.org/10.2113/gsecongeo.105.3.467.
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