Fabric development of granite mylonites in the Soonchang shear zone: 2. Fabrics

순창전단대내 화강분쇄암의 열구조 발달: 2. 열구조

Chang, Tae-Woo;Lee, Mi-Kyung
장태우;이미경

  • Published : 19961200

Abstract

Composite planar fabrics in granite mylonites in the Soonchang shear zone consist of four types of foliations: 1) S-foliation, 2) C-foliation, 3) oblique foliation, and 4) extensional crenulation foliation. Their development is closely related to the strain intensity. At low strain, S-foliations are the most conspicuous. whereas C-foliations are weak and nonpenetrative. At intermediate strain. C-foliations become penetrative and the angle between S - and C - foliations decreases with increasing strain. At high strain, S- and C-foliations are virtually parallel: oblique foliations more conspicuous. Finally, extensional crenulation foliations superimpose on the earlier-formed foliations. Quartz c-axes progressively become concentrated in orientation with increasing strain toward the center of the shear zone and the patterns of fabric diagram gradually change as follows: point maximum around z axis ${\rightarrow}$ crossed girdle ${\rightarrow}$ single girdle ${\rightarrow}$ point maximum around Y axis. Active slip system was probably basal slip at the margin of the shear zone, and rhomb slip and prism slip at the center. Mylonitization in the Soonchang shear zone probably took place in the Late Middle Jurassic with a dextral movement under a temperature condition of $400^{\circ}{\sim}500^{\circ}C$.

순창전단대 화강분쇄암에서는 혼합 면열구조 (S엽리, C엽리, 사각엽리, 신장 파랑엽리) 4가지 형태가 발견되며 이들의 발달은 변형 증가에 밀접히 상관된다. 저변형에서 S엽리는 현저하고 균질하나 C엽리는 드물고 비관통상이다. 중변형에서는 C엽리도 관통상이 되고 S와 C사이의 각은 감소한다. 고변형에서 S엽리는 C엽리와 거의 평행하게 되고 사각엽리는 중변형에서 보다 더 뚜렷하게 관찰된다. 신장 파랑엽리는 마지막으로 발달하여 이전에 생성된 엽리들을 간섭하고 있다. 전단대의 가장자리에서 중심부를 향해 석영 c축은 배향이 점차 집중되어지고 열구조 그림의 가장자리에서 중심을 향해 이동한다. 작용한 슬립계는 전단대의 가장자리에서 저면 슬립, 중심부에서 능면 슬립과 주면 슬립이 지배적으로 일어났다. 순창전단대의 분쇄암화 작용은 $400^{\circ}{\sim}500^{\circ}C$의 온도 조건하에서 우수 운동하에 (쥬라기 중기 말엽) 일어난 것으로 추정된다.

Keywords

References

  1. 담양 - 거창 지역에 분포하는 중생대 화성암류의 U-Pb 저어콘 지질 연대, 대한지질학회 제48차 정기총회 및 학술발표회 초록집 김정빈;김용준
  2. 지질학회지 v.21 전남 영광 부근 화강암질 분쇄암 미구조의 순차적 발달 장태우
  3. 지질학회지 v.32 순창전단대내 화강분쇄암의 열구조 발달: 1. 입자크기 감소 장태우;이미경
  4. 지질학회지 v.25 전주 부근 화강암의 연성 변형작용에 관하여 장태우;한영민
  5. 지질학회지 v.30 광주 전단대내 석영분쇄암의 미구조에 관한 연구 장태우
  6. 영남육괴 Rb-Sr 연대 측정(2): 지리산 남서부 일대 편마상 화강암류 및 화강암질 편마암류, KR-86-7 주승환;김성재
  7. Lithos v.6 Microstructure of mylonite and their descriptive terminology Bell, T.H.;Etheridge, M.A.
  8. Jour. Struct. Geol. v.1 Orthogneiss, mylonite and non-coaxial deformation of granites: the example of the South Amorican shear zone Berthe, D.;Choukroune, P.;Jegouzo, P.
  9. Tectonophysics v.78 Variscan intracontinental deformation: the Coimbra-Cordoba shear zone (SW Iberian Peninsula);The Effect of Deformation on Rocks Burg, J.P.;Iglesias, M.;Laurent, Ph.;Matte, Ph.;Ribeiro, A.;Lister, G.S.(ed.);Behr, H.J.(ed.);Weber, K.(ed.);Zwart, H.J.(ed.)
  10. Tectonophysics v.47 Strain analysis of a shear zone in a granodiorite Burg, J.P.;Lawrent, Ph.
  11. Relative timing of shear zone formation and pluton emplacement in the Yechon shear zone, Korea Chang, T.W.
  12. Jour. Geol. Soc. Korea v.27 On the microstructures of mylonitic rocks with special reference to Yechon shear zone, Korea Chang, T.W.
  13. Jour. Struct. Geol. v.17 Quartz deformation in a very fine grained quartzo-felds-pathic mylonite: a lack of evidence for dominant grain boundary sliding deformation Fliervoet, T.F.;White, S.H.
  14. Geology v.17 Shear structures within deformed granites: mechanical and thermal indicators Gapais, D.
  15. Metall. Trans. v.7A Grain-boundary sliding and its accomodation during creep superplasticity Gifkins, R.C.
  16. Jour. Struct. Geol. v.17 Development of phyllonite from granodiorite: mechanisms of grain-size reduction in the Santa Rosa mylonite zone, California Goodwin, L.B.;Wenk, H.R.
  17. Shear sense indicaters: a review, 90-17 Hanmer, S.;Passchier, C.
  18. Jour. Geol. Soc. Korea v.28 Shear criteria in mylonites from the Soonchang shear zone, the Hwasoon coalfield, Korea Kee, W.S.;Kim, J.H.
  19. Jour. Struct. Geol. v.13 Quartz c-axis fabric differences between porphyroclasts and recrystallized grains Kirschner, D.;Teyssier, C.
  20. Geol. Soc. Lond. Spec. Pub. v.54 Crystallographic fabrics: a selective review of their applications to research in structural geology;Deformation Mechanisms, Rheology and Tectonics Law, R.D.;Knipe, R.J.(ed.);Rutter, E.H.(ed.)
  21. Tectonophysics v.39 Discussion: Crossed girdle c-axis fabrics in quartzites plastically deformed by plane strain and progressive simple shear Lister, G.S.
  22. Jour. Sturct. Geol. v.6 S-C mylonites Lister, G.S.;Snoke, A.W.
  23. Jour. Struct. Geol. v.8 Porphyroclast systems as kinematic indicators Passchier, C.W.;Simpson, C.
  24. Jour. Struct. Geol. v.1 Extensional crenulation cleavage Platt, J.P.
  25. Jour. Struct. Geol. v.2 Shear zones in the Iberian arc Ponce de Leon, M.J.;Choukroune, P.
  26. Can. J. Earth. Sci. v.7 Strain variation in shear belts Ramsay, J.G.;Graham, R.H.
  27. Geophys Monogr., Am. Geophys. Union v.36 Complete fabric analysis of some commonly observed quartz c-axis pattern Schmid, S.M.;Casey, M.
  28. Geology v.12 Borrego Springs-Santa Rosa mylonite zones: a Late Cretaceous west-directed thrust in southern California Simpson, C.
  29. Geol. Soc. Am. Bull. v.94 An evaluation of criteria to deduce the sense of movement in sheared rocks Simpson, C.;Schmid, S.M.
  30. Jour. Metamor. Geol. v.7 Evidence for deformation-induced K-feldspar replacement by myrmekite Simpson, C.;Wintch, R.P.
  31. Short Course Notes, 1991 Ann. GSA Mtg. Deformation and kinematics of high strain zones Simpson, C.;De Paor, D.
  32. Tectonophysics v.92 Grain-size reduction and foliation development in a deformed granitoid batholith Vernon, R.H.;Williams, V.A.;D'Arcy, W.F.
  33. Schweiz. Mineral. Petrogr. Mitt. v.56 Recrystallization of quartz, biotite and feldspar from Erstfeld to the Leventina nappe, Swiss Alps, and its geological significance Voll, G.
  34. Jour. Struct. Geol. v.2 On mylonites in ductile shear zones White, S.H.;Burrows, S.E.;Carreras, J.;Shaw, N.D.;Humphreys, F.J.