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Volumn 106, Issue 4, 1997, Pages 225-236

Development of quartz ribbons in quartzofeldspathic granulites

Author keywords

Deformation; Dislocations; Quartz ribbons; Recrystallization

Indexed keywords

GRANULITES; QUARTZ RIBBONS;

EID: 0031397438     PISSN: 02534126     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article
Times cited : (6)

References (22)
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    • Bouchez, J.L.1    Mainprice, D.H.2    Trepied, L.3    Doukhan, J.C.4
  • 3
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    • Quartz shape fabric variations and c axis fabric in a ribbon-mylonite: Arguments for an oscillating foliation
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  • 4
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    • The Moine thrust zone in assynt region, northwest Scotland
    • Christie J M 1963 The Moine thrust zone in assynt region, northwest Scotland; Univ. Calif. Pubis. Geol. Sci. 40 345-439
    • (1963) Univ. Calif. Pubis. Geol. Sci. , vol.40 , pp. 345-439
    • Christie, J.M.1
  • 5
    • 0021283825 scopus 로고
    • Quartz ribbons in high grade granite gneiss: Modifications of dynamically formed quartz c-axis preferred orientation by oriented grain growth
    • Culshaw N G and Fyson W K 1984 Quartz ribbons in high grade granite gneiss: Modifications of dynamically formed quartz c-axis preferred orientation by oriented grain growth; J. Struct. Geol. 6 663-668
    • (1984) J. Struct. Geol. , vol.6 , pp. 663-668
    • Culshaw, N.G.1    Fyson, W.K.2
  • 8
    • 0026614655 scopus 로고
    • Phase boundary mobility in naturally deformed, high-grade quartzofeldspathic rocks: Evidence of diffusional creep
    • Gower R J W and Simpson C 1992 Phase boundary mobility in naturally deformed, high-grade quartzofeldspathic rocks: Evidence of diffusional creep; J. Struct. Geol. 14 301-313
    • (1992) J. Struct. Geol. , vol.14 , pp. 301-313
    • Gower, R.J.W.1    Simpson, C.2
  • 9
    • 0026614487 scopus 로고
    • Dislocation creep regimes in quartz aggregates
    • Hirth G and Tullis J 1992 Dislocation creep regimes in quartz aggregates; J. Struct. Geol. 14 145-159
    • (1992) J. Struct. Geol. , vol.14 , pp. 145-159
    • Hirth, G.1    Tullis, J.2
  • 11
    • 0024200125 scopus 로고
    • Simulation of fabric development in recrystallizing aggregates-II. Example from model runs
    • Jessell M W 1988 Simulation of fabric development in recrystallizing aggregates-II. Example from model runs; J. Struct. Geol. 10 779-793
    • (1988) J. Struct. Geol. , vol.10 , pp. 779-793
    • Jessell, M.W.1
  • 13
    • 33745997496 scopus 로고
    • Strain path partitioning within thrust sheets: Microstructural and petrofabric evidence from the Moine Thrust zone at Loch Eriboll, northwest Scotland
    • Law R D, Knipe R J and Dayan H 1984 Strain path partitioning within thrust sheets: Microstructural and petrofabric evidence from the Moine Thrust zone at Loch Eriboll, northwest Scotland; J. Struct. Geol. 12 29-45
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    • Law, R.D.1    Knipe, R.J.2    Dayan, H.3
  • 14
    • 0021284067 scopus 로고
    • The origin of ribbon lineation within the southern Adrirondacks
    • McLelland J 1984 The origin of ribbon lineation within the southern Adrirondacks. U.S.A.; J. Struct. Geol. 6 147-157
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    • McLelland, J.1
  • 15
    • 0000761853 scopus 로고
    • Microscopic deformation mechanisms and flow laws in quartzites within South Mountain anticline
    • Mitra S 1978 Microscopic deformation mechanisms and flow laws in quartzites within South Mountain anticline; J. Geol. 86 129-152
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  • 18
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    • Origin of leptynites, an orthopyroxenefrce granite gneiss, in two granulite terrains of India
    • Hindusthan Publishing Corporation
    • Sen S K 1987 Origin of leptynites, an orthopyroxenefrce granite gneiss, in two granulite terrains of India; Geological Evolution of Peninsular India. Petrological and Structural aspects, Hindusthan Publishing Corporation, 13, 117-124
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  • 19
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    • Microstructures and preferred orientations of experimentally deformed quartzites
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  • 21
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    • Compositional changes of minerals associated with dynamic recrystallization
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    • Yund, R.A.1    Tullis, J.2
  • 22
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    • Preferred orientation in quartz ribbon mylonites
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    • Wilson, C.J.L.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.