Difference between revisions of "Natural hydraulic fracturing example, North Sea"

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Revision as of 16:42, 31 January 2014

Exploring for Oil and Gas Traps
Series Treatise in Petroleum Geology
Part Predicting the occurrence of oil and gas traps
Chapter Evaluating top and fault seal
Author Grant M. Skerlec
Link Web page
Store AAPG Store

Trap description

A trap in the Central Graben, North Sea, appears to have been bled dry by natural hydraulic fracturing. This trap is a low-relief salt structure with a dry hole and has less-than-sufficient strain to fracture the top seal.

Evidence

Evidence for hydraulic fracturing and seal rupture include the following:

  • A fossil oil—water contact exists at the synclinal spill point of the trap. The trap was once filled with hydrocarbon, but something happened after trap fill to bleed off hydrocarbons.
  • Hydrocarbon shows exist throughout the sediment column above the reservoir. These hydrocarbons are direct evidence of a breached top seal.
  • The pore pressure is close to the theoretical fracture pressure. In adjacent fields, the pore pressure is significantly less than Pf.
  • Cores show vertical, open extension fractures rather than the more common shear fractures found in adjacent fields. These fractures are identical to fractures produced by hydraulic fracturing.

Figure 10-44 shows that the pore pressure is close to the fracture pressure at the base of the top seal (approximately depth::1300 ft). The pore pressure is inferred from mud weight and RFT measurements (solid dots). Leak-off tests (LOT) help constrain the fracture pressure. The fracture pressure is close to the lithostatic pressure or overburden pressure.

Figure 10-44 . Copyright: Esso Exploration and Production, U.K.

See also

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