Geology of Kampung Pak Kancil, Permaisuri, Terengganu and seismic interpretation of Abu Field, Terengganu offshore

Kampung Pak Kancil situated at Permaisuri, Terengganu where it has been long acknowledged as meta-sediment area. The purpose of this project is to update a geological map with a size of 5 x 5 km². Several analyses, including petrography, stratigraphy, geomorphology, and structural geology, were conducted for this study. Geological mapping was performed to obtain relevant data, and a sample was collected for petrography examination. The analysis was backed by an old research article and scholarly publication. The research region has four different types of rock: phyllite, slate, schist, and mudrock. In the Charu/Sungai Perlis Bed, phyllite and schist make up the lithology. The structural geology discovered consists of significant syncline and anticline folds. It is proposed that structural geology be the subject of a comprehensive study of the region. The Abu Field is part of the Malay Basin and is located offshore Terengganu, Malaysia. It has been identified as a sedimentary region containing a hydrocarbon resource. The seismic series has been the primary focus of substantial hydrocarbon exploration in this region. Abu field has not yet been subjected to a full stratigraphic and structural analysis, and it is suggested that this be the focus of future research. Using three-dimensional data, six seismic sections spanning the research region have been identified. Four principal reflectors have been identified as sequence boundaries, with each sequence including a seismic facies unit based on seismic characteristics. On the basis of the structural features discovered within the research region, such as faults and anticlines, it may be claimed that this area has probable hydrocarbon deposits.