剪切带运动学涡度研究进展
摘要
剪切带是调节相对刚性围岩之间相对运动而形成的高应变带。对剪切带应变方式的分析,可利用各种对称或者不对称的构造来直接判断。然而,这些方法定量化程度较低。运动学涡度的研究能定量的表征纯剪切和简单剪应变方式所占比例。通过不同方法测量大量单个样品的运动学涡度值,建立运动学涡度时空演化轨迹,能为剪切带非均匀、非稳态变形历史的研究提供更多信息。总结前人对剪切带运动学涡度的研究,并结合当前研究前沿,综述剪切带运动学涡度的理论及其应用。
引文
[1]Ramsay J G.Shear zone geometry:a review[J].Journal of Structural Geology,1980,2:83～99.
[2]Passchier C W,Trouw R A J.Microtectonics[M].Berlin:Springer-Verlag,2005,111～112.
[3]Marques F O,Bose S.Influence of a permanent low-friction boundary on rotation and flow in rigid inclusion/viscous matrix systems from an analogue perspective[J].Tectonophysics,2004,382(3/4):229～245.
[4]Mancktelow N S.How ductile are ductile shear zones[J].Geology,2006,34(5):345～348.
[5]Simpson C,De Paor D G.Strain and kinematic analysis in general shear zones[J].Journal of Structural Geology,1993,15:1～20.
[6]张进江,郑亚东.运动学涡度、极摩尔圆及其在一般剪切带定量分析中的应用[J].地质力学学报.1995,1(3):55～64.
[7]张进江,郑亚东.运动学涡度和极摩尔圆的基本原理与应用[J].地质科技情报.1997,16(3):33～39.
[8]郑亚东.亚干变质核杂岩的运动学涡度与剪切作用类型[J].地质科学.1999,34(3):273～280.
[9]Zhang J J,Zheng Y D,Liu S W.Application of general shear theory to the study of formation mechanism of the metamorphic core complex:a case study of Xiao qin ling in central China[J].Acta Geol.Sin.,2000,74:19～28.
[10]王勇生,朱光.运动学涡度及其测量方法[J].合肥工业大学学报(自然科学版).2004,27(11):1480～1484.
[11]王新社,郑亚东,王涛.内蒙赤峰南部楼子店韧性剪切带应变与剪切作用类型[J].中国科学D辑.地球科学.2007,37:160～166.
[12]郑亚东,王涛,张进江.运动学涡度的理论与实践[J].地学前缘.2008,15(3):209～220.
[13]Xypolias P.Vorticity analysis in shear zones:A review of methods and applications[J].Journal of Structural Geology,2010:1～21.
[14]李建波,王涛,郭磊,等.韧性剪切带的剪切作用类型和韧性减薄量[J].地质通报.2012,31(1):26～37.
[15]Ramberg H.Particle paths,displacement and progressive strain applicable to rocks[J].Tectonophysics 1975,28:1～37.
[16]Weijermars R.The role of stress in ductile deformation.Journal of Structural Geology[J].1991,13:1061～1078.
[17]Means W D et al.Vorticity and non-coaxiality in progressive deformations[J].Journal of Structural Geology,1980,2:371～378.
[18]Lin S,Jiang D,Williams P F.Transpression(or transtension)zones of triclinic symmetry:natural example and theoretical modeling[C].//Holdsworth R E,Strachran R A,Dewey J F.Continental Transpressional and Transtensional Tectonics.Geological Society Special Publications,1998,135:41～57.
[19]Jiang D,Williams P F.High-strain zones:A unified model[J].Journal of Structural Geology,1998,20:1105～1120.
[20]Robin P-Y F,Cruden A R.Strain and vorticity patterns in ideally ductile transpressional zones[J].Journal of Structural Geology,1994,16:447～466.
[21]Jiang D.Vorticity decomposition and its application to sectional flow characterization[J].Tectonophysics,1999,301:243～259.
[22]Truesdell C.Two measures of vorticity[J].Journal of Rational Mechanics Analysis,1953,2:173～217.
[23]Passchier C W.The fabric attractor[J].Journal of Structural Geology,1997,19:113～127.
[24]Passchier C W.Flow in natural shear zones-the consequences of spinning flow regimes[J].Earth and Planetary Science Letters,1986,77:70～80.
[25]Passchier C W.The fabric attractor[J].Journal of StructuralGeology,1997,19(1):113～127.
[26]Bobyarchick A R.The eigenvalues of steady state flow in Mohr space[J].Teetonophysics,1986,122:35～51.
[27]Law R D,Searle M P,Simpson R L.Strain,deformation temperatures and vorticity of flow at the top of the Greater Himalayan Slab,Everest Massif,Tibet[J].Journal of the Geological Society,2004,161:305～320.
[28]Passchier C W.Analysis of deformation paths in shear zones[J].International Journal of Earth Sciences,1988,77:309～318.
[33]Knipe R J,White S H.Deformation in low grade shear zones in the Old Red Sandstone,S.W.Wales[J].Journal of Structural Geology,1979,1:53～66.
[34]Grasemann B,Fritz H,Vannay J C.Quantitative kinematic flow analysis from the main central thrust zone(NW-Himalaya,India):implications for a decelerating strain path and the extrusion of orogenic wedges[J].Journal of Structural Geology,1999,21:837～853.
[35]Wallis S R,Platt J P,Knott S D.Recognition of sunconvergence extension in accretionary wedges with examples from the Calabrian Arc and the Eastern Alps[J].American Journal of Science,1993,293:463～495.
[36]李建波.华北克拉通北缘变质核杂岩韧性拆离带的应变、运动学涡度分析与韧性减薄量[D].北京市:中国地质科学院.2010.
[37]Fossen H.Structural geology[M].Cambridge university press,2010.39～41.
[2]Passchier C W,Trouw R A J.Microtectonics[M].Berlin:Springer-Verlag,2005,111～112.
[3]Marques F O,Bose S.Influence of a permanent low-friction boundary on rotation and flow in rigid inclusion/viscous matrix systems from an analogue perspective[J].Tectonophysics,2004,382(3/4):229～245.
[4]Mancktelow N S.How ductile are ductile shear zones[J].Geology,2006,34(5):345～348.
[5]Simpson C,De Paor D G.Strain and kinematic analysis in general shear zones[J].Journal of Structural Geology,1993,15:1～20.
[6]张进江,郑亚东.运动学涡度、极摩尔圆及其在一般剪切带定量分析中的应用[J].地质力学学报.1995,1(3):55～64.
[7]张进江,郑亚东.运动学涡度和极摩尔圆的基本原理与应用[J].地质科技情报.1997,16(3):33～39.
[8]郑亚东.亚干变质核杂岩的运动学涡度与剪切作用类型[J].地质科学.1999,34(3):273～280.
[9]Zhang J J,Zheng Y D,Liu S W.Application of general shear theory to the study of formation mechanism of the metamorphic core complex:a case study of Xiao qin ling in central China[J].Acta Geol.Sin.,2000,74:19～28.
[10]王勇生,朱光.运动学涡度及其测量方法[J].合肥工业大学学报(自然科学版).2004,27(11):1480～1484.
[11]王新社,郑亚东,王涛.内蒙赤峰南部楼子店韧性剪切带应变与剪切作用类型[J].中国科学D辑.地球科学.2007,37:160～166.
[12]郑亚东,王涛,张进江.运动学涡度的理论与实践[J].地学前缘.2008,15(3):209～220.
[13]Xypolias P.Vorticity analysis in shear zones:A review of methods and applications[J].Journal of Structural Geology,2010:1～21.
[14]李建波,王涛,郭磊,等.韧性剪切带的剪切作用类型和韧性减薄量[J].地质通报.2012,31(1):26～37.
[15]Ramberg H.Particle paths,displacement and progressive strain applicable to rocks[J].Tectonophysics 1975,28:1～37.
[16]Weijermars R.The role of stress in ductile deformation.Journal of Structural Geology[J].1991,13:1061～1078.
[17]Means W D et al.Vorticity and non-coaxiality in progressive deformations[J].Journal of Structural Geology,1980,2:371～378.
[18]Lin S,Jiang D,Williams P F.Transpression(or transtension)zones of triclinic symmetry:natural example and theoretical modeling[C].//Holdsworth R E,Strachran R A,Dewey J F.Continental Transpressional and Transtensional Tectonics.Geological Society Special Publications,1998,135:41～57.
[19]Jiang D,Williams P F.High-strain zones:A unified model[J].Journal of Structural Geology,1998,20:1105～1120.
[20]Robin P-Y F,Cruden A R.Strain and vorticity patterns in ideally ductile transpressional zones[J].Journal of Structural Geology,1994,16:447～466.
[21]Jiang D.Vorticity decomposition and its application to sectional flow characterization[J].Tectonophysics,1999,301:243～259.
[22]Truesdell C.Two measures of vorticity[J].Journal of Rational Mechanics Analysis,1953,2:173～217.
[23]Passchier C W.The fabric attractor[J].Journal of Structural Geology,1997,19:113～127.
[24]Passchier C W.Flow in natural shear zones-the consequences of spinning flow regimes[J].Earth and Planetary Science Letters,1986,77:70～80.
[25]Passchier C W.The fabric attractor[J].Journal of StructuralGeology,1997,19(1):113～127.
[26]Bobyarchick A R.The eigenvalues of steady state flow in Mohr space[J].Teetonophysics,1986,122:35～51.
[27]Law R D,Searle M P,Simpson R L.Strain,deformation temperatures and vorticity of flow at the top of the Greater Himalayan Slab,Everest Massif,Tibet[J].Journal of the Geological Society,2004,161:305～320.
[28]Passchier C W.Analysis of deformation paths in shear zones[J].International Journal of Earth Sciences,1988,77:309～318.
[33]Knipe R J,White S H.Deformation in low grade shear zones in the Old Red Sandstone,S.W.Wales[J].Journal of Structural Geology,1979,1:53～66.
[34]Grasemann B,Fritz H,Vannay J C.Quantitative kinematic flow analysis from the main central thrust zone(NW-Himalaya,India):implications for a decelerating strain path and the extrusion of orogenic wedges[J].Journal of Structural Geology,1999,21:837～853.
[35]Wallis S R,Platt J P,Knott S D.Recognition of sunconvergence extension in accretionary wedges with examples from the Calabrian Arc and the Eastern Alps[J].American Journal of Science,1993,293:463～495.
[36]李建波.华北克拉通北缘变质核杂岩韧性拆离带的应变、运动学涡度分析与韧性减薄量[D].北京市:中国地质科学院.2010.
[37]Fossen H.Structural geology[M].Cambridge university press,2010.39～41.