Modelling hydrocarbon generation and migration in tertiary source rocks of deepwater, Phu Khanh Basin, offshore Vietnam
- 주제(키워드) Phu Khanh Basin , hydrocarbon generation , migration , heat flow , source rock , Vietnam
- 주제(기타) Energy & Fuels; Engineering, Chemical; Engineering, Petroleum
- 설명문(일반) [Nguyen Xuan Huy; Ta Quoc Dung; Nguyen Thi Thu Trang; Kieu Nguyen Binh] Ho Chi Minh Univ Technol HCMUT, Fac Geol & Petr Engn, 268 Ly Thuong Kiet St,Dist 10, Ho Chi Minh City 700000, Vietnam; [Nguyen Xuan Huy; Ta Quoc Dung; Nguyen Thi Thu Trang; Kieu Nguyen Binh] Vietnam Natl Univ Ho Chi Minh City, Linh Trung Ward, Ho Chi Minh City 700000, Vietnam; [Cu Minh Hoang] Petrovietnam Explorat & Prod Corp, Hanoi 100000, Vietnam; [Baehyun, Min] Ewha Woman Univ, Dept Climate & Energy Syst Engn, Seoul 03760, South Korea; [Androne, Delia Anne-Marie] Alexandra Ioan Cuza Univ Iasi, Dept Geog, Iasi 700506, Romania
- 관리정보기술 faculty
- 등재 SCIE, SCOPUS
- 발행기관 INDERSCIENCE ENTERPRISES LTD
- 발행년도 2021
- URI http://www.dcollection.net/handler/ewha/000000183527
- 본문언어 영어
- Published As http://dx.doi.org/10.1504/IJOGCT.2021.117452
초록/요약
This study modelled a petroleum system to analyse the history of basin evolution, maturity, and hydrocarbon generation in the deepwater of the Phu Khanh Basin, offshore Vietnam. The paleo-heat flow, surface-water interface temperatures, and paleo water-depth were modelled using existing wells occurring in shallow to deep marine environments. Based on the geochemical analysis, the Oligocene and Lower-Middle Miocene source rocks are predominantly a mixture of type II and type III kerogens, with differences in distribution and maturation level. In the Phu Khanh Basin, hydrocarbon generation started during the Early Miocene. Petroleum migrated to a trap and accumulated in an uplift structure in the sandstone and carbonate reservoirs of the Lower Miocene formation. The results of this study can assist in defining the distribution of reservoir locations for future field development planning in the Phu Khanh Basin. [Received: March 28, 2020; Accepted: August 7, 2020]
more