TY - JOUR
T1 - Modelling hydrocarbon generation and migration in tertiary source rocks of deepwater, Phu Khanh Basin, offshore Vietnam
AU - Huy, Nguyen Xuan
AU - Dung, Ta Quoc
AU - Trang, Nguyen Thi Thu
AU - Hoang, Cu Minh
AU - Baehyun, Min
AU - Androne, Delia Anne Marie
AU - Binh, Kieu Nguyen
N1 - Funding Information:
This research is funded by Vietnam National University Ho Chi Minh City (VNU-HCM) under Grant Number C2018-20-24. Dr. Baehyun Min was supported by the National Research Foundation of Korea (NRF) Grants (No. 2017K1A3A1A05069660, No. 2018R1A6A1A08025520, and No. 2019R1C1C1002574). We would like to thank Ho Chi Minh City University of Technology (HCMUT), VNU-HCM for the support of time and facilities for this study. In addition, we are grateful for the support from Petrovietnam Exploration and Production Corporation (PVEP). We appreciate Schlumberger for providing the reservoir simulation software.
Funding Information:
This research is funded by Vietnam National University Ho Chi Minh City (VNU-HCM) under Grant Number C2018-20-24. Dr. Baehyun Min was supported by the National Research Foundation of Korea (NRF) Grants (No. 2017K1A3A1A05069660, No. 2018R1A6A1A08025520, and No. 2019R1C1C1002574).
Publisher Copyright:
Copyright © 2021 Inderscience Enterprises Ltd.
PY - 2021
Y1 - 2021
N2 - 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]
AB - 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]
KW - Heat flow
KW - Hydrocarbon generation
KW - Migration
KW - Phu Khanh Basin
KW - Source rock
KW - Vietnam
UR - http://www.scopus.com/inward/record.url?scp=85114899127&partnerID=8YFLogxK
U2 - 10.1504/IJOGCT.2021.117452
DO - 10.1504/IJOGCT.2021.117452
M3 - Article
AN - SCOPUS:85114899127
SN - 1753-3317
VL - 28
SP - 137
EP - 159
JO - International Journal of Oil, Gas and Coal Technology
JF - International Journal of Oil, Gas and Coal Technology
IS - 2
ER -