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  • 1
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(1044-L)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: IV, L-86 S. + 2 pl.
    Series Statement: U.S. Geological Survey professional paper 1044-L
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
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    In:  Geology, Amsterdam, Schweizerbart'sche Verlagsbuchhandlung, vol. 27, no. 12, pp. 1107-1110, pp. L12S09, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 1999
    Description: The decrease in permeability (k) of the continental crust with depth (z), as constrained by geothermal data and calculated fluid flux during metamorphism, is given by log k = -14 - 3.2 log z, where k is in meters squared and z is in kilometers. At moderate to great crustal depths (〉~5 km), this curve is defined mainly by data from prograde metamorphic systems, and is thus applicable to orogenic belts where the crust is being thickened and/or heated; lower permeabilities may occur in stable cratonic regions. This k-z relation implies that typical metamorphic fluid flux values of ~10^11 m/s are consistent with fluid pressures significantly above hydrostatic values. The k-z curve also predicts that metamorphic CO2 flux from large orogens may be sufficient to cause significant climatic effects, if retrograde carbonation reactions are minimal, and suggests a significant capacity for diffuse degassing of Earth (10^15 -- 10^16 g/yr) in tectonically active regions.
    Keywords: cracks and fractures (.NE. fracturing) ; Fluids ; porosity
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  • 3
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    In:  Reviews of Geophysics, Ottawa, 3-4, vol. 37, no. 1, pp. 127-150, pp. 1057, (ISSN: 1340-4202)
    Publication Date: 1999
    Description: Migrating fluids play a crucial role in the transport of heat and mass in the crust as well as in the mechanical strength of the crust. A synthesis and integration of evidence from diverse disciplines is used to quantify the fundamental parameter for this fluid transport, the permeability of the crust as a function of depth.
    Keywords: Geothermics ; Fluids ; Physical properties of rocks ; Review article
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  • 4
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    In:  Water Resour. Res., Warszawa, Inst. Electrical & Electronics Engineers, vol. 34, no. 10, pp. 2573-2586, pp. L11614, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1998
    Keywords: InSAR ; Fluids ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Physical properties of rocks ; 1829 ; Hydrology ; Groundwater ; hydrology ; 1894 ; Instruments ; and ; techniques ; 1803 ; Anthropogenic ; effects ; 5194 ; Physical ; properties ; of ; rocks ; JGR
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  • 5
    Publication Date: 2012-05-12
    Description: Oscillations in stress, such as those created by earthquakes, can increase permeability and fluid mobility in geologic media. In natural systems, strain amplitudes as small as 10−6 can increase discharge in streams and springs, change the water level in wells, and enhance production from petroleum reservoirs. Enhanced permeability typically recovers to prestimulated values over a period of months to years. Mechanisms that can change permeability at such small stresses include unblocking pores, either by breaking up permeability-limiting colloidal deposits or by mobilizing droplets and bubbles trapped in pores by capillary forces. The recovery time over which permeability returns to the prestimulated value is governed by the time to reblock pores, or for geochemical processes to seal pores. Monitoring permeability in geothermal systems where there is abundant seismicity, and the response of flow to local and regional earthquakes, would help test some of the proposed mechanisms and identify controls on permeability and its evolution.
    Print ISSN: 8755-1209
    Topics: Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 6
    Publication Date: 2014-10-08
    Description: Fluid circulation in the Earth's crust plays an essential role in surface, near surface, and deep crustal processes. Flow pathways are driven by hydraulic gradients but controlled by material permeability, which varies over many orders of magnitude and changes over time. Although millions of measurements of crustal properties have been made, including geophysical imaging and borehole tests, this vast amount of data and information has not been integrated into a comprehensive knowledge system. A community data infrastructure is needed to improve data access, enable large-scale synthetic analyses, and support representations of the subsurface in Earth system models. Here, we describe the motivation, vision, challenges, and an action plan for a community-governed, four-dimensional data system of the Earth's crustal structure, composition, and material properties from the surface down to the brittle–ductile transition. Such a system must not only be sufficiently flexible to support inquiries in many different domains of Earth science, but it must also be focused on characterizing the physical crustal properties of permeability and porosity, which have not yet been synthesized at a large scale. The DigitalCrust is envisioned as an interactive virtual exploration laboratory where models can be calibrated with empirical data and alternative hypotheses can be tested at a range of spatial scales. It must also support a community process for compiling and harmonizing models into regional syntheses of crustal properties. Sustained peer review from multiple disciplines will allow constant refinement in the ability of the system to inform science questions and societal challenges and to function as a dynamic library of our knowledge of Earth's crust. We describe the motivation, vision, challenges and an action plan for a community-governed, four-dimensional data system of the Earth's crustal structure, composition and material properties from the surface down to the brittle-ductile transition.
    Print ISSN: 1468-8115
    Electronic ISSN: 1468-8123
    Topics: Geosciences
    Published by Wiley
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  • 7
    Publication Date: 2014-11-08
    Print ISSN: 1468-8115
    Electronic ISSN: 1468-8123
    Topics: Geosciences
    Published by Wiley
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  • 8
    Publication Date: 2014-09-20
    Description: Heat-flow mapping of the western USA has identified an apparent low-heat-flow anomaly coincident with the Columbia Plateau Regional Aquifer System, a thick sequence of basalt aquifers within the Columbia River Basalt Group (CRBG). A heat and mass transport model (SUTRA) was used to evaluate the potential impact of groundwater flow on heat flow along two different regional groundwater flow paths. Limited  in situ permeability ( k ) data from the CRBG are compatible with a steep permeability decrease (approximately 3.5 orders of magnitude) at 600–900 m depth and approximately 40°C. Numerical simulations incorporating this permeability decrease demonstrate that regional groundwater flow can explain lower-than-expected heat flow in these highly anisotropic ( k x / k z  ~ 10 4 ) continental flood basalts. Simulation results indicate that the abrupt reduction in permeability at approximately 600 m depth results in an equivalently abrupt transition from a shallow region where heat flow is affected by groundwater flow to a deeper region of conduction-dominated heat flow. Most existing heat-flow measurements within the CRBG are from shallower than 600 m depth or near regional groundwater discharge zones, so that heat-flow maps generated using these data are likely influenced by groundwater flow. Substantial  k  decreases at similar temperatures have also been observed in the volcanic rocks of the adjacent Cascade Range volcanic arc and at Kilauea Volcano, Hawaii, where they result from low-temperature hydrothermal alteration. Regional groundwater flow can explain lower-than-expected heat flow in a thick sequence of highly anisotropic (k x /k z ~10 4 ) continental flood basalts (Columbia River Basalt Group). A steep permeability decrease (approximately 3.5 orders of magnitude) is observed at 600–900 m depth and approximately 40°C, possibly a result of low-temperature hydrothermal alteration. Substantial k decreases at similar temperatures have also been observed in the volcanic rocks of the Cascade Range and at Kilauea Volcano, Hawaii
    Print ISSN: 1468-8115
    Electronic ISSN: 1468-8123
    Topics: Geosciences
    Published by Wiley
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  • 9
    Publication Date: 2014-09-30
    Description: Nature Geoscience 7, 697 (2014). doi:10.1038/ngeo2261 Authors: S. E. Ingebritsen & M. Manga Earthquake prediction is a long-sought goal. Changes in groundwater chemistry before earthquakes in Iceland highlight a potential hydrogeochemical precursor, but such signals must be evaluated in the context of long-term, multiparametric data sets.
    Print ISSN: 1752-0894
    Electronic ISSN: 1752-0908
    Topics: Geosciences
    Published by Springer Nature
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  • 10
    Publication Date: 2014-09-24
    Description: Subsurface fluid-pressure declines caused by pumping of groundwater or hydrocarbons can lead to aquifer-system compaction and consequent land subsidence. This subsidence can be rapid, as much as 30 cm per year in some instances, and large, totaling more than 13 m in extreme examples. Thus anthropogenic subsidence may be the dominant contributor to relative sea-level rise in coastal environments where subsurface fluids are heavily exploited. Maximum observed rates of human-induced subsidence greatly exceed the rates of natural subsidence of unconsolidated sediments (∼0.1–1 cm yr −1 ) and the estimated rates of ongoing global sea-level rise (∼0.3 cm yr −1 ).
    Print ISSN: 1748-9318
    Electronic ISSN: 1748-9326
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering
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