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This study illustrates the effective utilisation and integration of sedimentology, biostratigraphy, organic petrology and petroleum geochemistry methods on outcrop samples to comprehend the evolution of a depositional basin (sec workflow as given in Figure 3). <br>The Neogene strata studied here consist of the Setap Shale, Belait and Liang formations, which are located within the Inboard Belt of the Sabah Basin, NW Borneo continental margin (see Figure 1 and Figure 2).