在台灣的地質分區中，中央山脈的東側可以區分為太魯閣帶及玉里帶。早期研究指出這兩個變質帶之間為一條斷層所分隔，為西側高溫低壓的太魯閣帶以及東側高壓低溫的玉里帶的分界，成東北西南走向。在已有文獻中，僅知在萬榮、銅門及新武地區有逆衝斷層出露，對於此一斷層的詳細情形尚未有詳細的記載。
本研究選定池南地區台14線公路龍澗-銅門段、木瓜溪河谷、荖溪河谷以及白鮑溪河谷進行野外地質調查，並採集標本進行伊萊石結晶度與綠泥石結晶度分析、鈉雲母存在指標分析及微視構造分析瞭解其運動型式，來判斷兩變質帶之間是否有構造存在。
研究結果顯示，在太魯閣帶及玉里帶兩變質帶間之韌性剪切帶為左移兼具逆衝的運動型式。伊萊石結晶度及綠泥石結晶度顯示在韌性剪切帶處有較好的結晶度。另外，僅在玉里帶中發現五個樣品含有鈉雲母，表示玉里帶壓力相較於太魯閣帶為高。

The central range of eastern Taiwan is proposed to be divided into a high-temperature/low-pressure Tailuko belt and a high-pressure/low-temperature Yuli belt by northeastern extending Shoufeng fault. Some previous studies have recognized the fault is a reverse fault or shear zone in Wanrung, Tongmen and Xinwu areas. However, the exact location is northern Central Range and the characteristics of the fault are still ambiguous.
In this research, Chinan area in north-central Range is selected as the study area. Observation of microscopic structures is used to identify the characteristics of the fault movement. Additionally, the illite and chlorite crystallinity determined by XRD are also used to help determining the location of the fault.
The study results show that there is a mylonite shear zone characterized by reverse motion with left-lateral strike slip component near the boundary of the Tailuko belt and the Yuli belt. The illite crytallinity index and chlorite crytallinity index all indicate the rocks in the shear zones have a better crystallinity. Additionally, the paragonite can only be found in five specimens sampled in the Yuli belt which implies that strata in Yuli belt have undergone a higher pressure than that in Tailuko belt.

小笠原美津雄，大南澳圖幅說明書，台灣總督府殖產局，第六五六號，共32頁，1933。
中國地質學會地層名詞統一委員會，1960，中國地層命名原則，中國地質學會會刊，第3號，第2-5頁。
朱傚祖，台灣北部矽線石之發現，中國地質學會專刊，第四號，第491-496頁，1981。
何春蓀，台灣地質概論-台灣地質圖說明書，第二版，經濟部中央地質調查所出版，共163頁，1986。
何恭睿，中央山脈萬榮地區地質構造研究，國立成功大學地球科學研究所碩士論文，共121頁，2007。
沈正嘉，台灣變質岩區鈉雲母之研究，國立成功大學地球科學研究所碩士論文，共89頁，1996。
林能通，大禹嶺地區岩石韌性剪切變形作用及糜嶺岩化作用，台灣大學地質學研究所碩士論文，共81頁，1995。
林啟文、楊昭男，由變質岩區的製圖單位與地質圖圖型探討臺灣中央山脈中北部的地層問題，經濟部中央地質調查所彙刊，第十五號，第69-86頁，2002。
曹恕中，台灣中央山脈變質沈積岩伊萊石結晶度、鋯石核飛跡年代和鉀氬年代之地質意義，國立台灣大學地質學研究所博士論文，共256頁，1996。
陳維民，花蓮銅門地區大南澳片岩之岩相構造學研究，國立台灣大學地質學研究所碩士論文，共69頁，1985。
陳維民、楊昭男，「花蓮銅門地區大南澳片岩之地質構造」，地質，第六卷，第二期，第1-20頁，1985。
陳肇夏，變質泥岩中鉀雲母的Ｘ光射線繞射圖樣變化及其對變質度之指示，中國地質學會專刊; 第4號, 第475-490頁，1981。
陳肇夏，利用鉀雲母綠泥石結晶度推定臺灣中央山脈綠色片岩相之下部界線，中國地質學會會刊; 第27號, 第41-53頁，1984。
陳肇夏、王京新，台灣變質相圖說明，經濟部中央地質調查所特刊，第二號，第1-51頁，1995。
陳肇夏、王京新、鍾三雄，鉀雲母結晶度在台灣雪山及中央山脈地層與構造研究上之應用，經濟部中央地質調查所特刊，第八號，第261-284頁，1994。
陳肇夏，台灣的變質岩，經濟部中央地質調查所，共356頁，1998。
陳肇夏、何信昌、謝凱旋、羅偉、林偉雄、張徽正、黃鑑水、林啟文、陳政恆、楊昭男、李元希，五十萬分之一台灣地質圖，經濟部中央地質調查所，2000。
錢憲和，國際地層小組工作的回顧與臺灣的地層問題，經濟部中央地質調查所特刊，第八號，第7-25頁。
顏滄波，台灣大南澳片岩區中之變質帶，中國地質學會會刊，第六號，第72-74頁，1963。
顏滄波，台灣之藍閃石片岩，中國地質學會會刊，第九號，第70-73頁，1966。
羅清華、王執明，台灣東部花蓮和平-溪畔地區片麻岩體內之礦物化學，中國地質學會會刊，第二十四號，第40-55頁，1981a。
Aldahan, A.A., Occurrence of epidote, pumpellyite and prehnite in Proterozoic clastics, dolerites and basalt from central Sweden, Neues Jahrbuch Miner. Abh., v.155, 147-164,1986.
Arkai, P., Chlorite crystallinity: an empirical approach and correlation with illite crystallinity, coal rank and mineral facies as exemplified by Palaeozoic and Mesozoic rocks of northeast Hungary, Journal of Metamorphic Geology, v.9, 723-734,1991.
Arkai, P., Merriman, R.J., Roberts, B., Peacor, D.R. and Toth, M.,Crystallinity,
crystallite size and lattice strain of illite-muscovite and chlorite: comparison of XRD and TEM data for diagenetic to epizonal pelites, Eur. Journal Mineral., v.8,1119-1137,1996.
Bell, T.H., Etheridge, M.A., Microstructures of mylonites and their descriptive terminology, Lithos, v.6, 337-348,1973.
Berthe, D., Choukroune, P. and Jegouzo, P. Orthogneiss,mylonite and non Coaxial deformation of granites:the example of the South Armorican Shear Zone.J. Struct. Geol. 1,31-42,1979.
Blatt, H., Tracy, R. J. and Owens, B. E. Petrology: Igneous, Sedimentary, and
Metamorphic (3rd). New York: W.H. Freeman, 530 p,2006.
Chatterjee, N.D.,Synthesis and upper stability of paragonite, Contrib.Mineral.
Petrol.,v.27, 244-257,1970.
Chatterjee, N.D., Low-temperature compatibility relations of the assemblage
quartz-paragonite and the thermodynamic status of the phase rectorite, Contrib.Mineral. Petrol., v.42, 259-271,1973.
Dunoyer de Segonzac,The transformation of clay mineral during diagenesis and low grade metamorphism:a review,Sedimentology,15,281-346,1970.
Ferry, J.M., A comparative study of geothermometers and geobarometers in politic schists from south-central Maine, Amer. Mineral., v.65, 720-732,1980.
Ferry, J.M., Petrology of graphitic sulfide-rich schists from south-central Maine: an example of desulfidation during prograde regional metamorphism, Amer. Mineral.,v.66, 908-930,1981.
Ferry, J.M., A comparative geochemical study of pelitic schists and metamorphosed carbonate rocks from south-central Maine, USA, Contrib. Mineral. Petrol., v.80,59-72,1982.
Fettes, D. and Desmons, J. Metamorphic Rocks: A Classification and Glossary of Terms. Cambridge University Press, p244,2007.
Frey, M., Low temperature metamorphism, Publish in the USA, Chapman and Hall, New York, 18-22,1987a.
Henley, R.W. and Ellis, A.J., Geothermal systems ancient and modern:a geochemical review, Earth-Science Reviews,v.19,1-50,1983.
Kubler, B., Anchimetamorphisme et schistosite, Bull. Centre Rech. PauSNPA, v.1(2),259-278,1967.
Merriman, R.J., Roberts, B., Peacor, D.R. and Hirons, S.R., Strain-relate differences in the crystal growth of white mica and chlorite:a TEM amd XRD study of the development of metapelitic microfabrics in the Southern Uplands thrust terrane, Scotland, Journal of Metamorphic Geology, v.13, 559-576,1995.
Miyashiro A., Evolution of metamorphic belts: Journal of Petrology, Vol.2,277-382,1961.
Passchier, C.W. and Trouw, R.A.J, Microtectonics,Springer,111-233,2005.
Ramsay, J.G. and Huber, M.I., The techniques of modern structural geology, v.1:Strain analysis Academic Press, London,1-307,1983.
Romeo, I., Capote, R. and Lunar R., Crystallographic preferred orientations and microstructure of a Variscan marble mylonite in the Ossa-Morena Zone (SW Iberia), Journal of structural geology, v.29, 1353-1368,2007.
Sibson, R.H., Fault rocks and fault mechanisms, Journal of the Geological Society of London, v.133, 191-213, 1977.
Stanley, R.S,Hill, L.B.,Chang,H.C. and Hu, H.N. A transect through the metamorphic core of the central mountains southern Taiwan,memoir of the geological society of china, NO. 4,443-473,1981.
Yen, T.P. Structral analysis of the slate formation of Taiwan. Bull, Geol. Soc. China, 21, 1-51,1970.