糜棱岩及其与其它区域变质岩的区别MYLONITES AND THEIR DISTINCTION FROM OTHER REGIONAL METAMORPHIC ROCKS
徐树桐
摘要(Abstract)：
糜棱岩形成于深部,以柔性变形为主或多或少保留脆性变形残迹,这是由于物性的不同,也是由于变形的塑性阶段的应变硬化造成的,一些高应变率的产物也可以生成于蠕变造成的糜棱岩中,因为积累于强烈变形带中的能量都有缓慢释放和突然释放过程的交替。在所提出的糜棱岩定义中,作者将变形行为作为糜棱岩的主要标志。按照这个定义,可以从区域变质岩和混合岩中分出一些新的糜棱岩类型。文中提出了一个便于野外应用的包括糜棱岩在内的断层岩分类表。在此分类中,形成于深部和浅部的断层岩有完全对应的结构。
关键词(KeyWords)：
基金项目(Foundation):
作者(Author): 徐树桐
参考文献(References)：
- 〔1〕Bates, R.L.and Jackson, J.A., Glossary of Geology, Amer.Geol.Inst., Fall Church,Virginia, 1980, p.400
- 〔2〕Bell, T.H.and Etheridge, MA., Microstructure of mylonites and their descriptive terminology,Lithos, 1974, Vol.6, pp.337-348
- 〔3〕Berthe, D and Jegouzo, P., Orthogneiss, mylonite and coaxial deformation of granites:the Example of the South American Shear Zone, J.of Str. Geol., 1979, Vol.1, pp.31-42
- 〔4〕Bobyarchicn, A.R., Deformation and metamorphism in the Hylas zone and adjacent parts of the Eastern Piedmont in Virginia, Geol.Soc.of Amer. Bull., 1979, Vol.90, No.8,pp.739-751
- 〔5〕Christie, J.M., Mylonitic rocks of Moine Thrust Zone in the Assynt region, Northwest Scotlaud, Trans.Edingburgh Geol.Soc.,1960, Vol.8, Pt.1, pp.79-93
- 〔6〕Dietrich. R.V., Banded gneiss of eight localities, Norsk.Geol.Tidsskr, 1963, Vol.43, No.1,pp.89-119
- 〔7〕Griggs, D.T., Hydrolic weakening of quartz and other silicates, Geophs.Jour.R.astr.Soc.,1967, Vol.14, pp.19-23
- 〔8〕Hurker, A., Metamorphism, Methuen, London, 1939, pp.3oo-320
- 〔9〕Higgings, M.W., Cataclasite rocks, US.Geol. Surv. Prof.Paper, 1971, No.687, pp.16-63
- 〔10〕Hobbs, B.E., Means, W.D., Williams, P.F., An Outline of Structural Geology, John Wiley & Sons Inc., 1970, pp.213-276, 416-428
- 〔11〕Hutton, D.H.W.,Tectonic Guide in the Caledonides, Thtrust and Nappe Tectonics, Blackwell Scientific Publications, 1961, pp.261-266
- 〔12〕Hopgood, A.M., Bowes, D.R.and Adison, J., Structural development of migmatites near Skado, South Finland, Bull. Geol.Finland, 1976, Vol.48, pp.43-62
- 〔13〕Hsu, K.J.,Thin skinned plate tectonics during nco-alpine orogenesis, Amer.J.Sci.,1979,Vol.279, pp.353-366
- 〔14〕Hyndman, D. W., Petrology of Igneous and Metamorphic Rocks, McGraw-Hill Inc., in USA.,1972, pp.240-255, 278-291
- 〔15〕Lister, G.S.and Snoke, A.W., 5-C mylonite, J.of Str.Geol.,1984, Vol.6.No.6.pp.617-638
- 〔16〕Myers,J.S.,Archean tectonics in the Fiskenaesset region of Southwest Greenland,PrecambrianTectonics Illustrated, E.Schwc-zerbart, sche Verlagsbuchhandlung (Nagele U .Obermiller),Stuttgart,1984, pp.95-112
- 〔17〕 Nicolas, A.and Poirier, J.P.,Crystalline Plasticity and Solid State Flow in Metamorphic Rocks, John Wiley & Sons Inc.,1976, pp.132-145, 176-187
- 〔18〕 Ramsay, J.G.,Folding and Fracturing of Rocks, McGraw-Hill Inc., New York, 1967, pp.256-258
- 〔19〕 Ramsay, J.G.,Shear zone geometry. a review. J.of Str. Goel., 1980,Vol.2, No.1/2, pp.83-99
- 〔20〕 Ramsay, J.G., The crack-seal mechanism of rock deformation , Nature, 1980 , Vol.284, No.5752, pp. 133-139
- 〔21〕 Sharma, R.S., On Banded Gneiss and Migmatites from Lavertezzo, and Rozzera,Schweizerische Mineralogische Petrographische Mitteilungen, 1969, Vol.49/2, pp.199-276
- 〔22〕 Sibson, R.H., Generation of pseudotachylite by ancient seismic faulting, Geophs.J.R.astr.Soc., 1975, Vol.43, pp.775-794
- 〔23〕 Sibson, R.H.,Fault rocks and fault mechanisms, J.Geol. Soc. London,1977,Vol.133,pp.191-213
- 〔24〕 Spry, A., Metamorphic Texture, Pergamon Press, Oxford, 1969, pp.224-240
- 〔25〕 White,J.G.and Mawer, C.K., Extreme ductility of feldspars from a mylonite, Parry Sound,Canada, J.of.Str. Geol., 1986, Vol.8, No.2, pp.133-143
- 〔26〕 Winkler, H.G.F., Petrogenesis of Metamorphic Rock, Springer-Verlag, 1979, pp. 82-83,248-251
- 〔27〕 徐树桐等:大别山东段(安徽)大别杂岩中的断层构造岩和推覆构造,《科学通报》,1984年,第4期,298-301页
- 〔28〕 除树桐,季寿元:天然变形岩石中黑云母的击象,《地质学报》,1985年,第59卷第4期,279-285页
- 〔29〕 徐树桐等:皖东元古代未之构造滑动,《国际交流地质学术论文集——为27届地质大会而作》,地质出版社,1985年,193-200页
- 〔30〕 徐树桐:安徽东部元古代变质岩中的糜棱岩带及其地质意义,《构造地质论丛》,1985年,第5期,97-110页