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Volumn , Issue 30, 2004, Pages 129-134

Validity of the "rubbing" method for the field determination of the shear sense of a fault surface;Arazide bir fay yüzeyinin kayma yönünü saptamada kullanilan "elle dokunma" yönteminin geçerliliǧli

Author keywords

Fault kinematics; Minor structures; Shear sense

Indexed keywords

FAULT SLIP; SHEAR; SLICKENSIDE; STRUCTURAL GEOLOGY;

EID: 14844290886     PISSN: 13012894     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article
Times cited : (1)

References (11)
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  • 2
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    • Koçyiǧit, A., 1991. An example of an accretionary fore-arc basin from northern Central Anatolia and its implications for the history of subduction of Neo-Tethys in Turkey. Geological Society of America Bulletin, 103, 22-36.
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    • Koçyiǧit, A.1
  • 6
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    • Petit, J.-P.1
  • 7
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    • The techniques of modern structural geology, (2): Folds and fractures
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    • Ramsay, J.G., and Huber, M.I., 1987. The techniques of modern structural geology, (2): Folds and fractures. London, Academic Press, 392 pp.
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  • 8
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    • (1929) , pp. 354-368
    • Riedel, W.1
  • 9
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    • Similarities between shear zones of different magnitudes
    • Tchalenko, J.S., 1970. Similarities between shear zones of different magnitudes. Geological Society of America Bulletin, 81, 1625-1640.
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  • 10
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    • Structural analysis of the Dasht-e Bayaz (Iran) earthquake fractures, Geological Society of America Bulletin
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  • 11
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.