The Ductile Deformation Characteristics of Caledonian Intracontinental Orogeny in the Northeastern Jiangshan-Shaoxing Tectonic Zone:Insights from Magnetic Fabric Study and Its Geodynamic Implication
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摘要
The Jiangshan-Shaoxing tectonic zone was the northeastern boundary between the Yangtze Block and the Cathaysia Block during the Neoproterozoic and was an intracontinental orogenic belt during late of the early Paleozoic.In this tectonic zone,there develops a lot of mylonite underwent strong ductile deformation and schist,gneiss,and amphibolite with medium and high grade metamorphism which was formed during the late of early Paleozoic.The research of geometry and kinematic of ductile deformation in Jiangshan-Shaoxing tectonic zone is very important to reveal the tectonic process of intracontinental orogeny.This paper uses the anisotropy of magnetic susceptibility(AMS)to determine the ductile deformation geometry and kinematic of Jiangshan-Shaoxing tectonic zone combing with the field survey.In this study,190 specimens of 19 locations and 221 specimens of23 locations from Wangjiazhai section and Lipu-Sizhai section were analyzed.The magnetic foliation over magnetic lineation in both Wangjiazhai and Lipu-Sizhai sections together with the field observations indicated a compressional deformation pattern.3 and 4 strong ductile deformation zones can be established in the Wangjiazhai section and the Lipu-Sizhai section,respectively.According to the magnetic fabric and petro-fabric studies,the Northeastern Jiangshan-Shaoxing tectonic zone suffered two kinds of deformation patterns during the late early Paleozoic,i.e.,the thrusting deformation followed by sinistral shear deformation.
The Jiangshan-Shaoxing tectonic zone was the northeastern boundary between the Yangtze Block and the Cathaysia Block during the Neoproterozoic and was an intracontinental orogenic belt during late of the early Paleozoic.In this tectonic zone,there develops a lot of mylonite underwent strong ductile deformation and schist,gneiss,and amphibolite with medium and high grade metamorphism which was formed during the late of early Paleozoic.The research of geometry and kinematic of ductile deformation in Jiangshan-Shaoxing tectonic zone is very important to reveal the tectonic process of intracontinental orogeny.This paper uses the anisotropy of magnetic susceptibility(AMS)to determine the ductile deformation geometry and kinematic of Jiangshan-Shaoxing tectonic zone combing with the field survey.In this study,190 specimens of 19 locations and 221 specimens of23 locations from Wangjiazhai section and Lipu-Sizhai section were analyzed.The magnetic foliation over magnetic lineation in both Wangjiazhai and Lipu-Sizhai sections together with the field observations indicated a compressional deformation pattern.3 and 4 strong ductile deformation zones can be established in the Wangjiazhai section and the Lipu-Sizhai section,respectively.According to the magnetic fabric and petro-fabric studies,the Northeastern Jiangshan-Shaoxing tectonic zone suffered two kinds of deformation patterns during the late early Paleozoic,i.e.,the thrusting deformation followed by sinistral shear deformation.
The Jiangshan-Shaoxing tectonic zone was the northeastern boundary between the Yangtze Block and the Cathaysia Block during the Neoproterozoic and was an intracontinental orogenic belt during late of the early Paleozoic.In this tectonic zone,there develops a lot of mylonite underwent strong ductile deformation and schist,gneiss,and amphibolite with medium and high grade metamorphism which was formed during the late of early Paleozoic.The research of geometry and kinematic of ductile deformation in Jiangshan-Shaoxing tectonic zone is very important to reveal the tectonic process of intracontinental orogeny.This paper uses the anisotropy of magnetic susceptibility(AMS)to determine the ductile deformation geometry and kinematic of Jiangshan-Shaoxing tectonic zone combing with the field survey.In this study,190 specimens of 19 locations and 221 specimens of23 locations from Wangjiazhai section and Lipu-Sizhai section were analyzed.The magnetic foliation over magnetic lineation in both Wangjiazhai and Lipu-Sizhai sections together with the field observations indicated a compressional deformation pattern.3 and 4 strong ductile deformation zones can be established in the Wangjiazhai section and the Lipu-Sizhai section,respectively.According to the magnetic fabric and petro-fabric studies,the Northeastern Jiangshan-Shaoxing tectonic zone suffered two kinds of deformation patterns during the late early Paleozoic,i.e.,the thrusting deformation followed by sinistral shear deformation.
引文
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Cheng Hai,1991.The late Proterozoic collision orogeny in northeastern Zhejiang province.Geology Review,37:203-213(in Chinese).
De Wall,H?Greiling,R.O.,and Sadek,M.F.,2001.Postcollisional shortening in the late Pan-African Hamisana high strain zone,SE Egypt:field and magnetic fabric evidence.Precambrian Research,107(3-4):179-194.
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Ferre,E.C.,Teyssier,C,Jackson,M.,Thill,J.W.,and Rainey,E.S.,2003.Magnetic susceptibility anisotropy:A new petrofabric tool in migmatites.Journal of Geophysical Research:Solid Earth,108.http://dx.doi.org/10.1029/2002 JB001790.
Goldstein,A.G.,1980.Magnetic susceptibility anisotropy of mylonites from the Lake Char mylonite zone,southeastern New England.Tectonophysics,66(1-3):197-211.
Housen,B.A.,Van Der Pluijm,B.A.,and Essene,E.J.,1995.Plastic behavior of magnetite and high strains obtained from magnetic fabrics in the Parry Sound shear zone,Ontario Grenville Province.Journal of Structural Geology,17(2):265-278.
Hrouda,F.,1982.Magnetic anisotropy of rocks and its application in geology and geophysics.Geophysical Surveys,5(1):37-82.
Hrouda,F.,and Janak,F.,1976.The changes in shape of the magnetic susceptibility ellipsoid during progressive metamorphism and deformation.Tectonophysics,34(1-2):135-148.
Hu Shiling and Cheng Hai,1992.The age and geological significance of the mylonite in the Jiangshan-Shaoxing fault.In:Li,J.L(ed.),Study on the structure and evolution of oceanic continental lithosphere in Southeast China.Beijing:Metallurgical Industry Press,106-109(in Chinese).
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Jelinek,V.,1981.Characterization of the magnetic fabric of rocks.Tectonophysics,79(3-4):T63-T67.
Kligfield,R,Lowrie,W.,and Dalziel,I.W.,1977.Magnetic susceptibility anisotropy as a strain indicator in the sudbury basin,Ontario.Tectonophysics,40(3-4):287-308.
Kligfield,R.,Owens,W.H.,and Lowrie,W.,1981.Magnetic susceptibility anisotropy,strain,and progressive deformation in Permian sediments from the Maritime Alps(France).Earth and Planetary Science Letters,55:181-189.
Kneen,S.J.,1976.The relationship between the magnetic and strain fabrics of some haematite-bearing Welsh slates.Earth and Planetary Science Letters,3:413-416.
Kong Xiangsheng,Li Zhifei,Feng Changgen,Gu Mingguang and Ma Jianping,1995.The Precambrian geology of Chencai region in Zhejiang Province.Beijing:Geological Publishing House,136(in Chinese with English summary).
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