The use of soils in estimating the time of last movement of faults

Site safety factors require that a nuclear reactor not be built over an active fault. Pedological principles have been used to assist in defining the minimum time since the last movement of a fault. Soil morphology may indicate if a fault associated with the soil last moved before or after the forma...

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Veröffentlicht in:Soil Sci.; (United States) 1980-01, Vol.129 (6), p.345-352
1. Verfasser: DOUGLAS, LOWELL A.
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description Site safety factors require that a nuclear reactor not be built over an active fault. Pedological principles have been used to assist in defining the minimum time since the last movement of a fault. Soil morphology may indicate if a fault associated with the soil last moved before or after the formation of the soil. Mineral or rock alteration within the soil may indicate the minimum amount of time represented by the soil.
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Pedological principles have been used to assist in defining the minimum time since the last movement of a fault. Soil morphology may indicate if a fault associated with the soil last moved before or after the formation of the soil. Mineral or rock alteration within the soil may indicate the minimum amount of time represented by the soil.</abstract><cop>Baltimore</cop><pub>Baltimore :Lippincott Williams &amp; Wilkins Co</pub><doi>10.1097/00010694-198006000-00004</doi><tpages>8</tpages></addata></record>
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identifier ISSN: 0038-075X
ispartof Soil Sci.; (United States), 1980-01, Vol.129 (6), p.345-352
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subjects 220501 - Nuclear Reactor Technology- Environmental Aspects- Siting
510500 - Environment, Terrestrial- Site Resource & Use Studies- (-1989)
580100 - Geology & Hydrology- (-1989)
ENVIRONMENTAL SCIENCES
GENERAL STUDIES OF NUCLEAR REACTORS
GEOLOGIC FAULTS
GEOLOGIC STRUCTURES
GEOLOGY
GEOMORPHOLOGY
GEOSCIENCES
GROUND MOTION
MOTION
NUCLEAR FACILITIES
NUCLEAR POWER PLANTS
POWER PLANTS
REACTOR SITES
REACTORS
SITE SELECTION
SOILS
THERMAL POWER PLANTS
TIME MEASUREMENT
title The use of soils in estimating the time of last movement of faults
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