“CB” well is located in the South Makassar Basin, where the lithological unit comprises of the Balangbaru and the Toraja Formation. The Paleogene calcareous nannofossils biostratigraphy of this area has not been studied yet and the chronostratigraphic framework is still arguable, So in this study, we discuss the detailed bio-chronostratigraphy of the South Makassar Basin, using calcareous nannofossil biostratigraphy.
Oleh :
Yarra Sutadiwira
