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A biostratigraphic reinvestigation of 108 SSPC and competitor wells was undertaken in order to review the palaeoenvironments of the Lower Miocene to Pliocene deposits in the offshore NW Sabah area. The study was integrated with seismostratigraphic data, which defined the positions of the palaeoshelf edgeipalaeocoastline, and allowed for more detailed palaeoenvironmental reconstructions. For each stratigraphic interval, palaeoenvironment maps showing the areal distribution of depositional environments were constructed. In addition, detailed biostratigraphie/seismostratigraphic correlation enabled the recognition of four "seismic facies" (base of slope, slope, shelf and coastal plain). Integration with sand distribution data allows the characterisation of the palaeoenvironments/seismic facies in terms of their reservoir potential. The stratigraphic framework and depositional model on which this study was based on are shown in figures 2 and 3, respectively. Biostratigraphic revision was carried out on all 108 wells. An additional check for consistency of the palaeoenvironmental interpretation was provided by BULKMAT, a computer programme designed for the probabilistic interpretation of depositional environments based on foraminiferal content. Chronostratigraphic control was derived mainly from palynological data. Seismic data of superior quality acquired over the past decade add to the refinement of the palaeoenvironmental maps and demarcate the extent of the palaeoshelf edge and palaeocoastline. The integration of biostratigraphic and seismostratigraphic data enabled the construction of 19 palaeoenvironmental maps. These maps, which show the lateral distribution of palaeoenvironments, are based on the dominant palaeoenvironment (i.e., thickest) penetrated within well sections for each time interval. The stratigraphic intervals were defined primarily on

Palaeoenvironments of the Lower Miocene to Pliocene sediments in offshore NW Sabah area