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Wednesday, April 29, 2020 | History

3 edition of Fluid-rock interaction and fracture development in "crystalline" rock types found in the catalog.

Fluid-rock interaction and fracture development in "crystalline" rock types

Fluid-rock interaction and fracture development in "crystalline" rock types

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  • 37 Currently reading

Published by [Books and Open-File Reports Section, distributor in [Denver, Colo.? : Dept. of the Interior, U.S. Geological Survey .
Written in English

    Subjects:
  • Groundwater flow -- Nevada -- Nevada Test Site.

  • Edition Notes

    Includes bibliographical references (p. 51-53).

    Statementby D.E. Moore, C.A. Morrow, and J. Byerlee.
    SeriesOpen-file report -- no. 87-279., U.S. Geological Survey open-file report -- 87-279.
    ContributionsMorrow, C. A., Byerlee, J. D., Geological Survey (U.S.)
    The Physical Object
    FormatMicroform
    Pagination1 microfiche
    ID Numbers
    Open LibraryOL14661298M


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Fluid-rock interaction and fracture development in "crystalline" rock types Download PDF EPUB FB2

Get this from a library. Fluid-rock interaction and fracture development in 'crystalline' rock types. [D E Moore; C A Morrow; J D Byerlee; Geological Survey (U.S.)]. The control of precursor brittle fracture and fluid–rock interaction on the development of single and paired ductile shear zones Article in Journal of Structural Geology 27(4) April.

Clay mineral formation and fluid-rock interaction in fractured crystalline rocks of the Rhine rift system [Elektronische Ressource]: case studies from the.

The permeability (κ[m 2]) of fractured crystalline basement of the upper continental crust is an intrinsic property of a complex system of rocks and fractures that characterizes the flow properties of a representative volume of that bility decreases with depth.

Permeability can be derived from hydraulic well test data in deep by: Physical Properties and Fundamental Processes in Fractures T o build predictive models and understand the behavior of complex fracture systems it is necessary to understand the behavior of a single fracture under the same in situ conditions imposed on the whole system.

@article{osti_, title = {Low-temperature water-rock interactions in bedrock aquifers of southern Rhode Island: Results of laboratory simulations}, author = {Veeger, A.I. and Moulton, K.L.}, abstractNote = {The nature of low-temperature chemical reactions occurring in bedrock aquifers of southern Rhode Island was investigated in the laboratory using flow-through columns.

Especially during flow along macroscopic fractures, fluid migrating along the flow backbone has limited interaction with the fracture walls. However, where flow is controlled by grain-scale dilatancy, such as in cataclasite or ductile shear zone materials, fluid-rock reaction can occur along the flow path.

The following are a few of the theoretically identified factors that affect fracture propagation: (1) variations of in situ stresses existing in different layers of rock, (2) the relative bed thickness of formations in the vicinity of the fracture, (3) bonding between formations, (4) variations in mechanical rock properties, (5) fluid pressure.

Fluid-rock interaction: A reactive transport approach Journal Article Steefel, C ; Maher, K - Reviews in Mineralogy and Geochemistry Fluid-rock interaction (or water-rock interaction, as it was more commonly known) is a subject that has evolved considerably in. With the growing demands for sustainable and environmentally effective development of the subsurface, the petrophysics of crystalline rocks is becoming an increasingly important available: Applications of X-ray Computed Tomography in the Geosciences - ISBN Hydrocarbons in Crystalline Rocks - ISBN Fracture And In.