Hydrothermal diagenesis during the Zagros Orogeny produced three phases of saddle dolomites (SD1. SD2. and SD3) and two phases of blocky calcites (CI and CII) in the studied sections of Bekhme Formation (Fm) (Campanian−Maastrichtian). Field observations. https://parisnaturalfoodes.shop/product-category/ginkgoforce/