Journal
JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING
Volume 196, Issue -, Pages -Publisher
ELSEVIER
DOI: 10.1016/j.petrol.2020.107621
Keywords
Yinggehai basin; Overpressure; Caprock; Natural hydraulic fracturing; Leakage potential; Mud diapir
Categories
Funding
- National Science and Technology Major Projects of China [2016ZX05024-005-006]
- National Natural Science Foundation of China [41702156]
- Natural Science Foundation of Heilongjiang Province [TD2019D001]
- Youth Foundation of Northeast Petroleum University [2019QNL-01]
- Open Fund of Heilongjiang Province Key Laboratory of oil and gas reservoir formation and resource evaluation [KL20190106]
- Northeast Petroleum University [KYCXTD201803]
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The Yinggehai Basin is a highly overpressured basin, where the seal capacity of caprocks is crucial for controlling the vertical distribution of oil and gas. The study found that both C1 and C2 caprocks in the diapir zone and only C2 caprock far from the diapir zone experienced hydraulic leakage, suggesting that diapirism played a role in promoting natural hydraulic fracturing.
The Yinggehai Basin is a strongly overpressured basin without large-scale faults in the Central Depression Zone. The hydraulic seal capacity of the caprocks over geological history has been the key factor controlling the vertical distribution characteristics of oil and gas. Based on leak-off data, rock mechanics tests and measured pore pressure data, this paper analyses the potential of natural hydraulic fracturing with the fault analysis seal technology (FAST) methodology for caprocks C1 (caprock of the Huangliu Formation) and C2 (caprock of the Meishan Formation) of the diapir belt in the north Central Depression Zone and determines the failure mode and gas sealing capacity of the two caprocks. The results show that gas leakage occurred continuously in both C1 and C2 in the diapir zone (DZ) throughout geological time. However, far from the diapir zone (FDZ), hydraulic leakage occurred only in caprock C2 while no leakage occurred in caprock Cl over geological time. These results are consistent with the gas accumulation that occurred in both the Yinggehai Formation and Huangliu Formation in the DZ but only in the Huangliu Formation in the FDZ. A relatively reasonable explanation is that diapirism promoted natural hydraulic fracture development via the following effects: (i) Diapirism transfers deep overpressure to shallow layers and increases the pressure gradient; (ii) The high-angle fractures associated with diapirism reduce the critical stress condition for the occurrence of natural hydraulic fracturing; and (iii) Diapirism results in the formation of dome structures in shallow layers, causing more shallow burial of caprock in the DZ than the FDZ. Shallowly buried caprocks, which have a relatively lower hydraulic fracture pressure, facilitate gas migration. These effects promoted natural hydraulic fracturing in the DZ, which is the main reason for the difference in the vertical distribution of gas reservoirs between the DZ and FDZ.
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