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The Kalambaina Formation is a significant Paleocene stratigraphic unit characterized by fossiliferous, thinly bedded limestones, indicating stable marine conditions and serving as a key resource for the cement industry. It transitions into the Gamba Formation, an Eocene unit marked by a shift to clastic-dominated sedimentation and a regional marine regression, featuring dark gray shales and clays with limited fossil content. The Gamba Formation reflects a change to a shallow transitional marine environment,

Author

yhalirusani

Language

EN