Musumeci G. 2002. Sillimanite-bearing shear zones in syntectonic leucogranite: Fluid assisted brittle ductile deformation under amphibolites facies conditions. Journal of Structural Geology, 24(9): 1491-1505.
[16]
Oliver N H S. 2001. Linking of regional and local hydrothermal systems in the mid-crust by shearing and faulting. Tectonophysics, 335: 147- 161.
[17]
Pfiffner O A and Ramsay J G. 1982. Constraints on geological strain rates: Arguments from finite strain states of naturally deformed rocks. Journal of Geophysical Research, 87: 311-321.
[18]
Pryer L L. 1993. Microstructures in feldspars from a major crustal thrust zone: The Grenville Front, Ontario, Canada. Journal of Structural Geology, 15(1): 21-36.
[19]
Stipp M S H and Heilbronner R. 2002. The eastern Tonale fault zone: a "natural laboratory" for crystal plastic deformation of quartz over a temperature range from 250 to 700℃. Journal of Sructural Geology, 24: 1861-1884.
Bonnemaison M and Marcoux E. 1990. Auriferous mineralization in some shear zones: A three-stage model of metallogenesis. Mineralium Deposita, 25(2): 96-104.
[40]
Cai J X and Zhang K J. 2009. A new model for the Indochina and South China collision during the Late Permian to the Middle Triassic. Tectonophysics, 467: 35-43.
[41]
Frederico M F, Ginaldo A C, Rosa M S B and Kazuo F. 2010. Quartz recrystallization regimes, c-axis texture transitions and fluid inclusion reequilibration in a prograde greenschist to amphibolite facies mylonite zone( Ribeira Shear Zone, SE Brazil). Tectonophysics, 485: 193-214.
[42]
Liu L M and Peng S L. 2003. Prediction of hidden ore bodies by synthesis of geological, geophysical and geochemical information based on dynamic model in Fenghuangshan ore field, Tongling district, China. Journal of Geochemical Exploration, 81(1-3): 81-98.
[43]
Liu L M, Zhao Y L and Zhao C B. 2010. Coupled geodynamics in the formation of Cu skarn deposits in the Tongling-Anqing district, China: Computational modeling and implications for exploration. Journal of Geochemical of Exploration, 106: 146-155.
[44]
Massonne H J and Schreyer W. 1987. Phengite geobarometry based on the limiting assemblage with K-feldspar, phlogopite, and quartz. Contrib Mineral Petrol, 96: 212-224.
[45]
Mercier R J. 1977. Stress in the lithosphere: inferences from steadystate flow of rocks. Pure and Applied Geophysics, 115: 199-226.
[46]
Twiss R J. 1977. Theory and applicability of a recrystallized grain size paleopiezometer. Pure and Applied Geophysics, 115: 337-340.
[47]
Zhang G L, Boulter C A and Liang J C. 2001. Brittle origins for disseminated gold mineralization in mylonite: Gaocun gold deposit, Hetai goldfield, Guangdong Province, South China. Economic Geology, 96: 49-59.
[48]
Zhang K J and Cai J X. 2009. NE-trending Hepu-Hetai dextral shear zone in southern China: Penetration of the Yunkai promontory of South China into Indochina. Journal of Structural Geology, 31: 737-748.
[49]
Zhang Y H, Lin G, Roberts P and Ord A. 2007. Numerical modelling of deformation and fluid flow in the Shuikoushan district, Hunan Province, South China. Ore Geology Reviews, 31: 261-278.
[50]
Zhao C B, Hobbs B E, Mühlhaus H B and Ord A. 2001. Finite element modeling of rock alteration and metamorphic process in hydrothermal systems. Communications in Numerical Methods of Engineering, 17: 833-843.