2014
DOI: 10.1260/0144-5987.32.1.19
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Prospect of Ultra-Deep Petroleum Onshore China

Abstract: A series of breakthroughs have been achieved in the exploration of ultra-deep formations onshore China as geological understanding and technologies progress, such as Tarim Basin, Sichuan Basin, Bohai Bay Basin. Some new understandings are put forward suggesting that ultra-deep petroleum potential should be beyond expectation: hydrocarbons are controlled by rift valleys in the pre-Cambrian in China, conventional marine carbonate hydrocarbon source kitchens and scattered liquid hydrocarbons in source rocks are c… Show more

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Cited by 23 publications
(4 citation statements)
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“…Due to the increasing di culty of exploration and development of conventional oil and gas reservoirs worldwide, unconventional reservoirs have attracted increasing attention (Zou et al, 2014;He et al, 2017). The Tarim Basin, which is situated in the Xinjiang Uygur Autonomous Region of the People's Republic of China, is host to the T-Sh oil eld.…”
Section: Introductionmentioning
confidence: 99%
“…Due to the increasing di culty of exploration and development of conventional oil and gas reservoirs worldwide, unconventional reservoirs have attracted increasing attention (Zou et al, 2014;He et al, 2017). The Tarim Basin, which is situated in the Xinjiang Uygur Autonomous Region of the People's Republic of China, is host to the T-Sh oil eld.…”
Section: Introductionmentioning
confidence: 99%
“…Due to the increasing di culty of exploration and development of conventional oil and gas reservoirs worldwide, unconventional reservoirs have attracted intensive attention (Zou et al, 2014;He et al, 2017).…”
Section: Introductionmentioning
confidence: 99%
“…With the depletion of relatively shallow conventional reservoirs, ultra-deep resources will become an important target for oil and gas exploration. Carbonate reservoirs are typical examples (e.g., Zou et al, 2014), which, due to their burial depth and high degree of diagenesis, their pay zone is located in areas with secondary pores or cracks (or rift caves and karst caves) (Pang, 2010). The tectonic action, abnormal high pressure, the presence of fractures and thermal fluid activity favor the development of this secondary pore space.…”
Section: Introductionmentioning
confidence: 99%