Changes

Measurements of fluid inclusions, however, suggest pressure transients along faults of as much as 126 MPa [[pressure::(1,825 psi]]).<ref name=ch10r61>Parry, W., T., Bruhn, R., L., 1990, Fluid pressure transients on seismogenic normal faults: Tectonophysics, vol. 179, no. 3–4, p. 335–344., 10., 1016/0040-1951(90)90299-N</ref> Similar episodic fluid flow events are inferred from sandstone cements in the North Sea.<ref name=ch10r64>Robinson, A., Gluyas, J., 1992, Duration of quartz cementation in sandstones, North Sea and Haltenbanken basins: Marine and Petroleum Geology, vol. 9, no. 3, p. 324–327., 10., 1016/0264-8172(92)90081-O</ref>

Measurements of fluid inclusions, however, suggest pressure transients along faults of as much as 126 MPa [[pressure::(1,825 psi]]).<ref name=ch10r61>Parry, W., T., Bruhn, R., L., 1990, Fluid pressure transients on seismogenic normal faults: Tectonophysics, vol. 179, no. 3–4, p. 335–344., 10., 1016/0040-1951(90)90299-N</ref> Similar episodic fluid flow events are inferred from sandstone cements in the North Sea.<ref name=ch10r64>Robinson, A., Gluyas, J., 1992, Duration of quartz cementation in sandstones, North Sea and Haltenbanken basins: Marine and Petroleum Geology, vol. 9, no. 3, p. 324–327., 10., 1016/0264-8172(92)90081-O</ref>

Leakage through seals and seal capacity may be as episodic as hydrocarbon generation, migration, and pressure transients.

Leakage through seals and seal capacity may be as episodic as [[Petroleum generation|hydrocarbon generation]], [[migration]], and pressure transients.

==See also==

==See also==