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Published in 2019 at "Chemical Geology"
DOI: 10.1016/j.chemgeo.2019.06.021
Abstract: Abstract Marine carbonate δ13C and δ18O values are commonly utilized as indicators of past climate and are thought to record primary seawater conditions. However, these minerals can be altered following deposition and burial, overprinting the…
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Keywords:
rich depositional;
13c 18o;
carbonates mud;
midland basin ... See more keywords