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- W4239497689 abstract "This chapter deals with static permeability which include contributions related to sediments and sedimentary rocks and igneous and metamorphic rocks. In contrast to the near-surface crust, the bulk of the continental crust is dominated by metamorphic rocks rather than sedimentary rock. In contrast to the near-surface crust, the bulk of the continental crust is dominated by metamorphic rocks rather than sedimentary rock. The chapter explores porosity-permeability relations for clastic sediments to a depth of 2 km, a depth restriction that largely avoids complications such as pressure solution and hydrothermal alteration. Circulation of meteoric fluids to these depths may occur through “hydrologic windows” in overlying lower permeability units. Geochemical analyses and numerical modeling by Pepin et al. suggest that the Truth or Consequences, New Mexico, hot-spring system is supported by deep (2-8 km) circulation in permeable crystalline basement rocks." @default.
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- W4239497689 date "2012-01-17" @default.
- W4239497689 modified "2023-10-14" @default.
- W4239497689 title "Static permeability" @default.
- W4239497689 doi "https://doi.org/10.1002/9781119166573.ch9" @default.
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