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Isotope (δ13C and δ18O) compositions of dolomites from the Permian evaporitic sequences of the Eastern Russian Plate: Evidence from the Syukeevo gypsum deposit | 112 |
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Isotope (δ13C and δ18O) compositions of dolomites from the Permian evaporitic sequences of the Eastern Russian Plate: Evidence from the Syukeevo gypsum deposit | 3 | 1 | 1 | 0 | 0 | 5 | 0 |
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SCOPUS00244902-2014-49-5-SID84906494823-a1.pdf | 12 |
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