Abstract
Ham Rong Field is located in Block 106, Song Hong basin, offshore Vietnam, 75km SE of Hai Phong City. It is a proven Pre-Tertiary carbonate play with the discovery of Hamrong-1X ST4 and Hamrong- 2X. The field is located in the SW of block 106, at the SE edge of Thuy Nguyen Half Graben, Song Hong basin. The structure was formed as the results of a number of tectonic events such as regional uplift and extension creating a series of horst and grabens and the movement of the Red River fault. The study has targeted the qualitative and quantitative evaluation pf the pre-Tertiary carbonate reservoir.
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