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Volumn 23, Issue 8, 2001, Pages 1187-1202

Experimental investigation into the microstructural and mechanical evolution of phyllosilicate-bearing fault rock under conditions favouring pressure solution

Author keywords

Halite; Microstructure; Mylonites; Phyllosilicates; Pressure solution

Indexed keywords

CRUSTAL FAULT ZONES;

EID: 0035427447     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0191-8141(00)00184-X     Document Type: Article
Times cited : (148)

References (44)
  • 5
    • 0024251778 scopus 로고
    • The brittle-ductile transition in a deformation-mechanism map for halite
    • (1988) Tectonophysics , vol.154 , pp. 125-136
    • Chester, F.M.1
  • 11
  • 14
    • 0023468825 scopus 로고
    • The deformational behaviour of bimineralic limestone-halite aggregates
    • (1987) Tectonophysics , vol.135 , pp. 185-197
    • Jordan, P.1
  • 15
    • 0002688573 scopus 로고    scopus 로고
    • The strength profile for bimineralic shear zones: An insight from high-temperature shearing experiments on calcite-halite mixtures
    • (1998) Tectonophysics , vol.295 , pp. 1-14
    • Kawamoto, E.1    Shimamoto, T.2
  • 23
    • 0029543425 scopus 로고
    • A theory for granular flow accommodated by material transfer via an intergranular fluid
    • (1995) Tectonophysics , vol.245 , pp. 135-151
    • Paterson, M.S.1
  • 36
    • 0022439632 scopus 로고
    • Transition between frictional slip and ductile flow for halite shear zones at room temperature
    • (1986) Science , vol.231 , pp. 711-714
    • Shimamoto, T.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.