The study results indicate that there is a close relationship

An important point to note is similar facies (shoal grainstones, for example) under different sea-level situations (e.g., Late HST to Early TST vs. Late TST to Early HST) may exhibit dissimilar diagenetic overprints. As an example, while shoal grainstones under Late HST to Early TST conditions were generally subjected to dolomitization and subsequent anhydrite plugging, similar facies under Late TST to Early HST showed dissolution by meteoric waters.