Hydrocarbon Generation History of Tertiary Source Rocks in Phu Khanh Basin, Offshore Vietnam
The source rock maturity and the hydrocarbon generation history are evaluated in the deepwater Phu Khanh Basin. The average values of heat flow, paleo water depth, and surface-water interface temperatures range from 50.80–61.69 mW/m2, 150-3,500 m, and 2.30-250C, respectively. The Oligocene and Lower...
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doaj-1fbaf8fcdb0d4fa59679eeb7189de5762020-11-25T03:05:29ZengUniversitas Islam Riau (UIR) PressJournal of Earth Energy Engineering2301-80972540-93522020-10-0192596510.25299/jeee.2020.55295529Hydrocarbon Generation History of Tertiary Source Rocks in Phu Khanh Basin, Offshore VietnamHuy Xuan Nguyen0Trang Thi Thu Nguyen1Van Nguyen Nguyen2Thi Hong Quyen Vo3Faculty of Geology and Petroleum Engineering, Ho Chi Minh University of Technology (HCMUT)Faculty of Geology and Petroleum Engineering, Ho Chi Minh University of Technology (HCMUT); Vietnam National University Ho Chi Minh CityGeneral Department of Geology and Minerals of VietnamHo Chi Minh City Institute of Resources GeographyThe source rock maturity and the hydrocarbon generation history are evaluated in the deepwater Phu Khanh Basin. The average values of heat flow, paleo water depth, and surface-water interface temperatures range from 50.80–61.69 mW/m2, 150-3,500 m, and 2.30-250C, respectively. The Oligocene and Lower–Middle Miocene source rocks are presented. The Oligocene source rock is derived from the lacustrine environment; it is mature to overmature in the Southwest part of the Phu Yen Depression. The main oil phase started in the Early Miocene, and the amount of wet gas occurred only at the bottom part. The Lower-Middle Miocene source rock has been immature in both the Southwest and Northeast part of the Phu Yen Depression. Based on the geochemical analysis, these source rocks were predominantly a mixture of type II and type III kerogens. The total organic carbon and the hydrogen index values range from 1.8-2.5 % and 250-320 mg/g, respectively. The results can help define reservoir locations for future field development planning in the Phu Khanh Basin.https://journal.uir.ac.id/index.php/JEEE/article/view/5529phu khanh basinhydrocarbon generationpaleo heat flowsource rock |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Huy Xuan Nguyen Trang Thi Thu Nguyen Van Nguyen Nguyen Thi Hong Quyen Vo |
spellingShingle |
Huy Xuan Nguyen Trang Thi Thu Nguyen Van Nguyen Nguyen Thi Hong Quyen Vo Hydrocarbon Generation History of Tertiary Source Rocks in Phu Khanh Basin, Offshore Vietnam Journal of Earth Energy Engineering phu khanh basin hydrocarbon generation paleo heat flow source rock |
author_facet |
Huy Xuan Nguyen Trang Thi Thu Nguyen Van Nguyen Nguyen Thi Hong Quyen Vo |
author_sort |
Huy Xuan Nguyen |
title |
Hydrocarbon Generation History of Tertiary Source Rocks in Phu Khanh Basin, Offshore Vietnam |
title_short |
Hydrocarbon Generation History of Tertiary Source Rocks in Phu Khanh Basin, Offshore Vietnam |
title_full |
Hydrocarbon Generation History of Tertiary Source Rocks in Phu Khanh Basin, Offshore Vietnam |
title_fullStr |
Hydrocarbon Generation History of Tertiary Source Rocks in Phu Khanh Basin, Offshore Vietnam |
title_full_unstemmed |
Hydrocarbon Generation History of Tertiary Source Rocks in Phu Khanh Basin, Offshore Vietnam |
title_sort |
hydrocarbon generation history of tertiary source rocks in phu khanh basin, offshore vietnam |
publisher |
Universitas Islam Riau (UIR) Press |
series |
Journal of Earth Energy Engineering |
issn |
2301-8097 2540-9352 |
publishDate |
2020-10-01 |
description |
The source rock maturity and the hydrocarbon generation history are evaluated in the deepwater Phu Khanh Basin. The average values of heat flow, paleo water depth, and surface-water interface temperatures range from 50.80–61.69 mW/m2, 150-3,500 m, and 2.30-250C, respectively. The Oligocene and Lower–Middle Miocene source rocks are presented. The Oligocene source rock is derived from the lacustrine environment; it is mature to overmature in the Southwest part of the Phu Yen Depression. The main oil phase started in the Early Miocene, and the amount of wet gas occurred only at the bottom part. The Lower-Middle Miocene source rock has been immature in both the Southwest and Northeast part of the Phu Yen Depression. Based on the geochemical analysis, these source rocks were predominantly a mixture of type II and type III kerogens. The total organic carbon and the hydrogen index values range from 1.8-2.5 % and 250-320 mg/g, respectively. The results can help define reservoir locations for future field development planning in the Phu Khanh Basin. |
topic |
phu khanh basin hydrocarbon generation paleo heat flow source rock |
url |
https://journal.uir.ac.id/index.php/JEEE/article/view/5529 |
work_keys_str_mv |
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