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Weathering on some fault lines in crystalline rock massifs
Summary Within the scope of engineering geological classification of crystalline rock massifs processes of weathering and their products on fault lines and tectonic contacts have been studied with regard to the construction of large dams in the Bohemian Massif region. The fundamental factors influencing the origin and the character of residua and the morphology of mineral grains on the discontinuity surfaces have been pointed out. The fundamental factors are hydration, hydrolysis, limonitization, chloritization, epidotization with the pressure deformation of the fault clay. Examples of the character of these residua from the fault lines in paragneiss, magmatite, amphibolite and granodiorite are given.
Weathering on some fault lines in crystalline rock massifs
Summary Within the scope of engineering geological classification of crystalline rock massifs processes of weathering and their products on fault lines and tectonic contacts have been studied with regard to the construction of large dams in the Bohemian Massif region. The fundamental factors influencing the origin and the character of residua and the morphology of mineral grains on the discontinuity surfaces have been pointed out. The fundamental factors are hydration, hydrolysis, limonitization, chloritization, epidotization with the pressure deformation of the fault clay. Examples of the character of these residua from the fault lines in paragneiss, magmatite, amphibolite and granodiorite are given.
Weathering on some fault lines in crystalline rock massifs
Milena, Šamalíková (Autor:in)
1980
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
BKL:
56.00$jBauwesen: Allgemeines
/
38.58
Geomechanik
/
38.58$jGeomechanik
/
56.20
Ingenieurgeologie, Bodenmechanik
/
56.00
Bauwesen: Allgemeines
/
56.20$jIngenieurgeologie$jBodenmechanik
RVK:
ELIB18
Weathering on some fault lines in crystalline rock massifs
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