C, O, and Sr Isotope Geochemistry of the Vendian Shuram–Wonoka Anomaly and Associated Metasedimentary Rocks in the Inner Part of the Patom Upland (Central Siberia)-Reference-Cited by-同舟云学术

C, O, and Sr Isotope Geochemistry of the Vendian Shuram–Wonoka Anomaly and Associated Metasedimentary Rocks in the Inner Part of the Patom Upland (Central Siberia)

Published:2021-09 Issue:5 Volume:56 Page:390-417
ISSN:0024-4902
Container-title:Lithology and Mineral Resources
language:en
Short-container-title:Lithol Miner Resour

Author:

Pokrovsky B. G.,Bujakaite M. I.,Kolesnikova A. A.,Petrov O. L.,Khlebnikov M. S.

Publisher

Pleiades Publishing Ltd

Subject

Economic Geology,Geochemistry and Petrology

Link

https://link.springer.com/content/pdf/10.1134/S0024490221050047.pdf

Reference111 articles.

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3. Bartley, J.K., Pope, M., Knoll, A.H., et al., Vendian-Cambrian boundary succession from the northwestern margin of the Siberian Platform: stratigraphy, palaeontology, chemostratigraphy and correlation, Geol. Mag., 1998, vol. 135, no. 4, pp. 473–494.

4. Bergmann, K.D., Zentmyer, R.A., and Fischer, W.W., The stratigraphic expression of a large negative carbon isotope excursion from the Ediacaran Johnnie Formation, Death Valley, Precambrian Res., 2011, vol. 188, pp. 45–56.

5. Blättler, C.L., Claire, M.W., Prave, A.R., et al., Two-billion-year-old evaporites capture Earth’s great oxidation, Science, 2018, vol. 360, no. 6386, pp. 320–323.

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