The reliability of textural, structural, mineralogical and geochemical diagenetic criteria in identification of sea-level changes is illustrated from five regional sequences ranging in age from Pleistocene to Holocene. -from Authors
CITATION STYLE
Coudray, J., & Montaggioni, L. (1986). The diagenetic products of marine carbonates as sea-level indicators. Sea-Level Research, 311–360. https://doi.org/10.1007/978-94-009-4215-8_11
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