[1] Zhai Mingguo,Liu Wenjun．The formation of granulite and its contribution to evolution of the continental crust[J].Acta Petrologica Sinica,2001,17(1):28-38.[翟明国,刘文军. 麻粒岩的形成及其对大陆地壳演化的贡献[J]. 岩石学报,2001,17(1)：28-38.]
[2]Lai Shaocong, Qin Jiangfeng. Petrology and geochemistry of the granulite xenoliths from Cenozoic Qiangtang volcanic fiels：Implication for the nature of the lower crust in the northern Tibetan Plateau and the genesis of Cenozoic volcanic rocks[J].Acta Petrologica Sinica,2008,24(2):325-336.[赖绍聪, 秦江锋. 藏北羌塘地块新生代火山岩中麻粒岩捕虏体的岩石学和地球化学研究:对青藏高原新生代火山岩成因及下地壳性质的约束[J]. 岩石学报,2008, 24(2):325-336.]
[3] Guo Jinghui, Zhai Mingguo, Zhang Yigang, et al. Early precambrian Manjinggou highpressure granulite mélange belt on the south edge of the Huaian Complex, North China Craton: Geological features, petrology and isotopic geochronology[J].Acta Petrologica Sinica,1993,9(4):329-342.[郭敬辉,翟明国,张毅刚,等. 怀安蔓菁沟早前寒武纪高压麻粒岩混杂岩带地质特征、岩石学和同位素年代学[J].岩石学报, 1993,9(4):329-342.]
[4] Galan G, Marcos A. The metamorphic evolution of the high pressure mafic granulites of the Bacariza Formation (Cabo Ortegal Complex, Hercynian belt, NW Spain)[J].Lithos,2000, 54(3/4): 139-171.
[5] Montanini A, Harlov D. Petrology and mineralogy of granulitefacies mafic xenoliths (Sardinia, Italy): Evidence for KCl metasomatism in the lower crust[J].Lithos,2006, 92(3/4): 588-608.
[6]Li Zilong, Chen Hanlin, Yang Shufeng, et al. Discovery of mafic granulites from the Altay orogenic belt:Evidence from mineralogical study[J].Acta Petrologica Sinica,2004,20(6):1 445-1 455.[厉子龙,陈汉林,杨树锋,等. 阿尔泰基性麻粒岩的发现:来自矿物学的证据[J]. 岩石学报,2004,20(6):1 445-1 455.]
[7] Gao Shan,Luo Tingchuan,Zhang Benren ,et al.Structure and propose of crust in China east[J].Science in China (Series D),1999,29(3): 203-213.[高山,骆庭川,张本仁,等. 中国东部地壳的结构和组成 [J]. 中国科学:D辑,1999,29(3): 203-213.]
[8]Okamoto A,Michibayashi K. Progressive shape evolution of a mineral inclusion under differential stress at high temperature: Example of garnet inclusions within a granulite[J].Journal of Geophysical Research,2005, 110(B11203): 1-16.
[9] Huang Xiaolong, Xu Yigang. Geochemical characteristics of the Nüshan granulite xenoliths,Anhui province:Implications for composite of lower crust and tectonic affinity[J]. Geochemistry, 2002,31(5):443-454.[黄小龙，徐义刚. 安徽女山麻粒岩包体的地球化学特征:下地壳组成及其构造属性初探[J]. 地球化学,2002,31(5):443-454.]
[10]Yu Jinhai, Xu Xisheng, Zhou Xinmin. Geochemistry of granulite xenoliths in south China coastal and the composition of lower crust[J].Science in China (Series D), 2002,32(5):383-393.[于津海,徐夕生,周新民. 华南沿海基性麻粒岩捕虏体的地球化学研究和下地壳组成[J]. 中国科学:D辑,2002,32(5):383-393.]
[11] Huang Xiaolong, Xu Yigang, Chu Xuelei, et al. Geochemical comparative studies of some granulite ferranes and granulite xenoliths from North China Craton[J].Acta Petrologica et Mineralogica, 2001,20(3):318-328.[黄小龙,徐义刚,储雪蕾,等. 华北地台部分麻粒岩地体及包体的地球化学特征对比[J]. 岩石矿物学杂志, 2001,20(3):318-328.]
[12]Rajamani V, Tripathi J K, Malviya V P. Weathering of lower crustal rocks in the Kaveri River catchment, southern India: Implications to sediment geochemistry[J].Chemical Geology,2009, 265(3/4): 410-419.
[13] Gong Songlin, Chen Nengsong, Liu Rong, et al. Excess Argon in Biotite from the Felsic Granulite in Huangtuling area,north Dabie unit:Genetic interpretation and implications to Ar isotope chronology[J]. Modern Geology,2007,21(2):226-231.[龚松林，陈能松，刘嵘，等. 北大别黄土岭麻粒岩中黑云母过剩Ar的成因解释和Ar同位素热年代学研究启示[J]. 现代地质,2007,21(2):226-231.][
[14]Zheng Jianping, Luo Zhaohua, Yu Chunmei,et al. Geochemistry and zircon geochronology of granulite xenoliths from Xinjiang Tuoyun: Petrogenesis and the property of lower crust in southwestern Tianshan[J].Chinese Science Bulletin,2005,50(8): 793-801.[郑建平，罗照华，余淳梅，等. 新疆托云麻粒岩捕虏体地球化学和锆石年代学:岩石成因及西南天山下地壳性质[J]. 科学通报,2005,50(8): 793-801.]
[15]Liu Yongsheng, Gao Shan, Zhou Lian, et al. Geochronology and geodynamic implication of the felsic granulite xenoliths from the Hannuoba basalt[J]. Geochemistry, 2001,30(1):51-56.[刘勇胜，高山，周炼，等. 汉诺坝长英质麻粒岩包体同位素年代学及其地球动力学意义[J].地球化学,2001,30(1):51-56.]
[16]Liu Shoujie, Li Jianghai, Santosh M. First application of the revised Tiinzircon geothermometer to Paleoproterozoic ultrahightemperature granulites of Tuguiwula, Inner Mongolia, North China Craton[J]. Contributions to Mineralogy and Petrology,2010, 159(2): 225-235.
[17] Taylor J, Stevens G, Armstrong R, et al. Granulite facies anatexis in the ancient gneiss complex, Swaziland, at 2.73 Ga: Midcrustal metamorphic evidence for mantle heating of the Kaapvaal craton during Ventersdorp magmatism[J]. Precambrian Research,2010, 177(1/2): 88-102.
[18]PadronNavarta J A, Garrido C J, SanchezNavas A, et al. Oriented growth of garnet by topotactic reactions and epitaxy in highpressure, mafic garnet granulite formed by dehydration melting of metastable hornblendegabbronorite (Jijal Complex, Kohistan Complex, North Pakistan)[J].Journal of Metamorphic Geology,2008, 26(8): 855-870.
[19]Chen Xiaode,Lin Chuanyong,Shi Lanbin. Deformation microstructures of lower crustal granulite xenoliths from Hannuoba Cenozoic basalts, China and their geologic implications[J]. Acta Petrologica Sinica,2007, 23(11): 2 775-2 784.[陈孝德，林传勇，史兰斌. 汉诺坝新生代玄武岩中下地壳麻粒岩包体的变形显微构造特征及其地质意义[J]. 岩石学报,2007,23(11)：2 775-2 784.][
[20] Xu Lili. Microstructure and Water Content Researcher of Granulite in Hebei Huaian[D].Wuhan:China University of Geosciences, 2008.[许丽丽. 河北怀安地体型麻粒岩显微组构特征及含水量研究[D]. 武汉: 中国地质大学, 2008.]
[21] Ma Baolin. The North China plate boundaries of the basic characteristics of the deep crustal rocks and the deformation mechanism [J].Acta Petrologica Sinica,1992, 8(1): 18-26.[马宝林. 华北板块边缘深地壳岩石的基本特征和变形机制[J].岩石学报,1992, 8(1): 18-26.]
[22] Jin Shuyan. Plagioclase fabrics and seismic anisotropy of the lower crust[J].Geological Science and Technology Information,2000, 19(3): 1-6.[金淑燕. 斜长石组构与下地壳各向异性[J]. 地质科技情报, 2000, 19(3): 1-6.]
[23]Ji Shaocheng, Mainprice D. Natural deformation fabrics of plagioclase: Implications for slip systems and seismic anisotropy[J].Tectonophysics,1988, 147: 145-163.
[24]Lund M D, Piazolo S, Harley S L. Ultrahigh temperature deformation microstructures in felsic granulites of the Napier Complex, Antarctica[J].Tectonophysics,2006, 427(1/4): 133-151.
[25]Blacic J D, Christie J M. Plasticity and hydrolytic weakening of quartz single crystals[J]. Journal of Geophysical Research,1984, 89: 4 223-4 239.
[26] Stipp M, Tullis J, Behrens H. Effect of water on the dislocation creep microstructure and flow stress of quartz and implications for the recrystallized grain size piezometer[J]. Journal of Geophysical Research,2006, 111(B04201):1-19.
[27] Puelles P, Abalos B, Gil Ibarguchi J I. Transposed highpressure granulite fabrics (Cabo Ortegal, NW Spain): Implications on the scales of deformation localization[J].Journal of Structural Geology,2009, 31(8): 776-790.
[28]Su Wen, Cong Bolin L, You Zhendong, et al. Plastic mechanism of deformation of garnetWater weakening[J].Science in China(Series D),2002, 45(10): 885-892.
[29] Kleinschrodt R, Mcgrew A. Garnet plasticity in the lower continental crust: Implications for deformation mechanisms based on microstructures and SEMelectron channeling pattern analysis[J].Journal of Structural Geology,2000, 22(6): 795-809.
[30] Kleinschrodt R,Duyster J P. HT deformation of garnet: An EBSD study on granulites from Sri Lanka, India and the Ivrea zone[J]. Journal of Structural Geology,2002, 24(11):1 829-1 844.
[31] Bestmann M, Habler G, Heidelbach F, et al. Dynamic recrystallization of garnet and related diffusion processes[J].Journal of Structural Geology,2008, 30(6): 777-790.
[32] Ji Shaocheng,Wang Qian, Xia Bin,et al.Generalized mixture rule and its applications to rheology of the earth materials[J].Acta Petrologica Sinica,2006,22(7):2 067-2 080.[嵇少丞, 王茜, 夏斌, 等.广义混合律及其在地球材料流变学中的应用[J]. 岩石学报,2006, 22(7):2 067-2 080.]
[33]Yang Zhentao,Ning Jieyuan, Zhao Yonghong. Finite element computation of rheology for multimineral rocks[J].Acta Petrologica Sinica,2004,20(6):1 469-1 476.[杨振涛, 宁杰远, 赵永红. 多矿物岩石流变性的有限元计算[J]. 岩石学报,2004, 20(6):1 469-1 476.]
[34] Jiang Yan, Zang Shaoxian.The research progressand some existing problems of rheological law for multimineral rocks[J].Progress in Geophysics,2002, 39(zl): 74-76.[江燕，臧绍先. 多矿物岩石流变规律的研究进展及存在问题[J]. 地球物理学进展,2002, 39(zl): 74-76.]
[35] Jiang Yan. Research of Experience Flow Law in MultiMineral Rocks and Investigate of the Lithosphere Rheological Structure Model[D]. Beijing:Beijing University,2002.[江燕. 多矿物岩石经验流变规律的研究及岩石圈流变结构模型的初步探讨[D]. 北京:北京大学,2002.]
[36] Ji Shaocheng,Wang Qian, Xia Bin,et al.Mechanical properties of multiphase materials and rocks: A phenomenological approach using generalized means[J].Journal of Structural Geology, 2004, 26: 1 377-1 390.
[37]Ji Shaocheng,Wang Qian, Xia Bin,et al. Flow laws of multiphase materials and rocks from endmember flow laws[J].Tectonophysics,2003, 370: 129-145.
[38]Ji Shaocheng. Generalized means as an approach for predicting Young's moduli of multiphase materials [J].Materials Science and Engineering, 2004, 366: 195-201.
[39] Holyoke C W, Tullis J. Mechanisms of weak phase interconnection and the effects of phase strength contrast on fabric development[J].Journal of Structural Geology,2006, 28(4): 621-640.
[40] Ji Shaocheng，Wang Qian，Xu Zhiqin. BreakUp of the North China Craton through Lithospheric thinning[J].Acta Geologica Sinica, 2008, 82(2): 174-193.[嵇少丞，王茜，许志琴. 华北克拉通破坏与岩石圈减薄[J]. 地质学报,2008, 82(2): 174-193.]
[41] Johnson E A. Water in nominally anhydrous crustal minerals: Speciation, concentration, and geologic significance[C]∥Reviews in Mineralogy and Geochemistry.Mineralogical Society of America,2006,62: 117-154.
[42]Yang Xiaozhi, Xia Qunke, Deloule E, et al. Water in minerals of the continental lithospheric mantle and overlying lower crust: A comparative study of peridotite and granulite xenoliths from the North China Craton[J]. Chemical Geology,2008, 256(1/2): 33-45.
[43] Cuney M, Coulibaly Y, Boiron M. Highdensity early CO₂ fluids in the ultrahigh-temperature granulites of Ihouhaouene (in Ouzzal, Algeria)[J].Lithos,2007, 96(3/4): 402-414.
[44]RegenauerLieb K. Water and geodynamics[C]∥Reviews in Mineralogy and Geochemistry.Mineralogical Society of America,2006,62: 451-473.
[45] Yang Xiaozhi, Xia Qunke,Yu Huimin, et al. The possible effect of hydrogen on the high electrical conductivity in the lower continental crust[J].Advances in Earth Science,2006 ,21(1):31-38.[杨晓志，夏群科，于慧敏，等. 大陆下地壳高电导率的起源:矿物中的结构水[J]. 地球科学进展,2006,21(1):31-38.]
[46]Kohlstedt D L. The role of water in hightemperature rock deformation[C]∥Reviews in Mineralogy and Geochemistry.Mineralogical Society of America, 2006, 62: 377-396.
[47] Gleason G C, Desisto S. A natural example of crystalplastic deformation enhancing the incorporation of water into quartz[J]. Tectonophysics,2008, 446(1/4): 16-30.
[48] Ingrin J, Blanchard M. Diffusion of hydrogen in minerals[C]∥Reviews in Mineralogy and Geochemistry. Mineralogical Society of America,2006, 62: 291-320.
[49] Chen S, Hiraga T, Kohlstedt D L. Water weakening of clinopyroxene in the dislocation creep regime[J].Journal of Geophysical ResearchSolid Earth,2006, 111(B08203): 1-14.
[50] Ni H, Behrens H, Zhang Y. Water diffusion in dacitic melt[J]. Geochimica et Cosmochimica Acta,2009, 73(12): 3 642-3 655.
[51]Dimanov A W R D G. The effect of melt distribution on the rheology of plagioclase rocks[J].Tectonophysics,2000, 328: 307-327.
[52] Li Huaqi，Liang Yihong，Ma Rui，et al. The deformation structure and component migration of middlelower crustal rocks in differential stresses state with melt[J].Journal of Jilin University (Earth Science Edition),2009, 39(2): 262-268.[李化启，梁一鸿，马瑞，等. 含熔体差应力状态下中下地壳岩石的变形结构与物质迁移[J]. 吉林大学学报:地球科学版,2009, 39(2): 262-268.]
[53] Camacho A, Yang P, Frederiksen A. Constraints from diffusion profiles on the duration of highstrain deformation in thickened crust[J].Geology,2009, 37: 755-758.
[54]Fang H, Yongsheng H. Partial melting of the dry mafic continental crust: Implications for petrogenesis of Ctype adakites[J].Chinese Science Bulletin,2010, 55: 2 428-2 439.
[55]Zhou Yongsheng, He Changrong. The status of continental lithosphere rheology and experiments on creep of rocks at high temperature and high pressure[J].Progress in Geophysics, 2004,19(2):246254.[周永胜，何昌荣. 大陆岩石圈流变研究进展与高温高压流变实验现状[J]. 地球物理学进展, 2004,19(2):246-254.]
[56]Zhou Yongsheng, He Changrong. The continental crust typical rocks under high temperature and pressure flow experiment[J].Recent Developments in World Seismology,2004, (z1): 79.[周永胜，何昌荣. 大陆下地壳典型岩石的高温高压流变实验[J]. 国际地震动态,2004, (z1): 79.]
[57]Wilks K R, Carter N L. Rheology of some continental lower crustal rocks[J].Tectonophysics,1990, 182(1/2): 57-77.
[58]Zhou Yongsheng，He Changrong. Rhelogical paraneters of crustal rocks and crustal rheology of NorthChina[J].Earthquake Geology,2003, 25(1):1-7.[周永胜，何昌荣. 地壳主要岩石流变参数及华北地壳流变性质研究[J]. 地震地质,2003, 25(1):1-7.]
[59] Zhou Yongsheng，He Changrong，Huang Xiaoge, et al. Rheological complexity of mafic rocks and the effect of mineral component to creep ofrocks[J].Earth Science Frontiers,2009,16(1):1-12.[周永胜，何昌荣，黄晓葛，等. 基性岩流变的复杂性与成分对岩石流变影响的实验研究[J]. 地学前缘,2009,16(1):1-12].
[60]Dimanov A, Jaoul O, Sautter V. Calcium selfdiffusion in natural diopside single crystals[J].Geochimica et Cosmochimica Acta,1996, 60: 4 095-4 106.
[61] Dimanov A, Jaoul O. Calcium selfdiffusion in diopside at high temperature: Implications for transport properties[J].Physics and Chemistry of Minerals,1998, 26: 116-127.
[62]Dimanov A, Sautter V. “Average” interdiffusion of (Fe,Mn)Mg in natural diopside[J].European Journal of Mineralogy,2000, 12: 749-760.
[63]Bystricky M, Mackwell S. Creep of dry clinopyroxene aggregates[J].Journal of Geophysical ResearchSolid Earth,2001, 106:13 443-13 454.
[64]Mauler A, Bystricky M, Kunze K ,et al. Microstructures and lattice preferred orientations in experimentally deformed clinopyroxene aggregates[J].Journal of Structural,2000,84(1):1 633-1 648.
[65]Hier-Majumder, Mei S, Kohlstedt D L. Water weakening of clinopyroxenite in diffusion creep[J].Journal of Geophysical Research,2005, 110 (B07406):1-12.
[66] Skemer P, Karato S. Rheology and recrystallizationof orthopyroxene at upper mantle conditions[J].EOS Trans AmGeophys Union, 2006, 87(52): R23A-R25A.
[67]Dimanov A, Dresen G, Xiao X, et al. Grain boundary diffusion creep of synthetic anorthite aggregates: The effect of water[J].Journal of Geophysical Research-Solid Earth,1999, 104: 10 483-10 497.
[68]Rybacki E, Dresen G. Dislocation and diffusion creep of synthetic anorthite aggregates[J].Journal of Geophysical Research—Solid Earth,2000, 105: 26 017-26 036.
[69]Rybacki E, Wirth R, Dresen G. Highstrain creep of feldspar rocks: Implications for cavitation and ductile failure in the lower crust[J].Geophysical Research Letters,2008, 35(4): L4304.
[70]Kronenberg A K,Tullis J. Flow strengths of aggregates: Grain size and pressure effects due to hydrolytic weakening[J].Journal of Geophysical Research, 1984,89(B6):4 281-4 297.
[71]Trepmann C A, Stöckhert B. Quartz microstructures developed during non-steady state plastic flow at rapidly decaying stress and strain rate[J].Journal of Structural Geology,2003,25(12): 2 035-2 051.[
[72] Hirth G, Teyssier C, Dunlap J W. An evaluation of quartzite flow law based on comparisons between experimentally and naturally deformed rocks[J].International Journal of Earth Sciences,2001, 90: 77-87.
[73]Dimanov A, Dresen G. Rheology of synthetic anorthitediopside aggregates: Implications for ductile shear zones[J].Journal of Geophysical Research—Solid Earth,2005,110,doi:10.1029/2004JB003431.
[74] Dimanov A, Rybacki E, Wirth R, et al. Creep and straindependent microstructures of synthetic anorthitediopside aggregates[J]. Journal of Structural Geology,2007, 29: 1 049-1 069.
[75]Kronenberg A K, Shelton G L. Deformation microstructures in experimentally deformed Maryl and diabase[J].Journal of Structural Geology,1980, 2: 341-353.
[76]Mackwell S J, Zinmermen M E, Kohlstedt D L. High temperature deformation of dry diabase with application totectonics on Venus[J].Journal of Geophysical Research,1998, 103: 975-984.
[77] Wilks K R, Carter N L. Rheology of some continental lower crustal rocks[J].Tectonophysics,1990, 180(1/2): 57-77.
[78]He Changrong, Zhou Yongsheng,Sang Zu′nan. An experimental study on semibrittle and plastic rheology of Panzhihua gabbro[J].Science in China(Series D),2002, 32(9): 717-726.[何昌荣，周永胜，桑祖南. 攀枝花辉长岩半脆性—塑性流变的实验研究[J].中国科学:D辑,2002, 32(9): 717-726.]
[79] Liu Shun，Xiao Xiaohui，Zhong Dalai. Experimental research on rheological properties of a felsic granulite[J].Journal of Chengdu University of Technology,1997,24(1):42-47.[刘顺，肖晓辉，钟大赉. 长英质麻粒岩流变性质的实验研究[J]. 成都理工学院学报,1997,24(1):42-47.]
[80]Ross J V, Wilks K R. Effects of a third phase on the mechanical and microstructural evolutionofa granulite[J]. Tectono Physics,1995, 241: 303-316.
[81] Ross J V, Wilks K R. Microstructuredevelo pmentinanex perimentall yshearedortho pyroxene granulite[J].Tectonophysics,1996,256: 83-100.
[82]Liu Shun,Sun Tianze,Zhong Dalai.Experimental study of mechanism for semibrittle ductile shear zones in mafic granulite [J].Journal of Chengdu University of Technology,1997,24(3):36-41.[刘顺,孙天泽,钟大赉. 基性麻粒岩半脆性域剪切带形成机制的实验研究[J]. 成都理工学院学报,1997,24(3):36-41.][83]Chen Xiaode,Lin Chuanyong, Shi Lanbin. Rheology of the lower crust beneath the northern part of North China: Inferences from lower crustal xenoliths from Hannuoba basalts, Hebei province, China[J].Science in China (Series D),2007, 50(8): 1 128-1 141.[陈孝德,林传勇,史兰斌. 华北北部下地壳的流变学特征——河北汉诺坝下地壳包体提供的信息[J]. 中国科学:D辑,2007, 50(8): 1 128-1 141.][84]Wang Yongfeng,Zhang Junfeng,Jin Zhenmin, et al. Experimental research on rheological intensity of a mafic granulite in the lower crust [J].Bulletin of Mineralogy Petrology and Geochemistry,2008, 27(zl): 235-236.[王永锋，章军锋，金振民，等. 下地壳基性麻粒岩流变强度实验研究[J]. 矿物岩石地球化学通报,2008, 27(zl): 235-236.]
[85]Zhao Jing,Liu Shun. Experimental research on rheological behaviors of lower crust and its significance of tectonic evolution in the juncture area of Shanxi, Hebei and Inner Mongolia provinces, China[J]. Geological Journal of Universities,1998, 4(2): 155-165.[赵靖,刘顺. 晋冀内蒙交界区下地壳流变性质的实验研究及其构造演化意义[J]. 高校地质学报, 1998, 4(2): 155-165.]
[86]Rybacki E, Dresen G. Deformation mechanism maps for feldspar rocks[J].Tectonophysic, 2004, 382(3/4): 173-187.
[87]Jackson J. Strength of the continental lithosphereTime to abandon the jelly sandwich[J].GSA Today,2002,12: 4-9.
[88]Burgmann R, Dresen G. Rheology of the lower crust and upper mantle: Evidence from rock mechanics, geodesy, and field observations[J].Annual Review of Earth and Planetary Sciences,2008, 36: 531-567.
[89]Liu Junlai, Ji Mo, Xia Haoran, et al.Crustalmantle detachment of the North China Craton in Late Mesozoic: Rheological constraints[J].Acta Petrologica Sinica,2009,25(8):1 819-1 829.[刘俊来，纪沫,夏浩然,等. 华北克拉通晚中生代壳—幔拆离作用:岩石流变学约束[J]. 岩石学报, 2009, 25(8):1 819-1 829.]
[90]Liu Jing, Zeng Lingsen, Ding Lin, et al. Tectonic geomorphology,active tectonics and lower crustal channel flow hypothesis of the southeastern Tibetan Plateau[J].Geological Science,2009, 44(4): 1 227-1 255.[刘静，曾令森，丁林，等. 青藏高原东南缘构造地貌、活动构造和下地壳流动假说[J]. 地质科学, 2009, 44(4): 1 227-1 255.]
[91]Li Dewei. Continental lower crustal flow:Channel flow or laminarflow?[J].Earth Science Frontiers,2008,15(3):130-139.[李德威. 大陆下地壳流动:渠流还是层流?[J]. 地学前缘,2008, 15(3): 130-139.]
[92]Zhang Xinyu, Ji Jianqing, Han Baofu,et al.Research advance in erosion, rheology of lower crust and orogeny[J].Advances in Earth Science,2006,21(5): 521-531.[张新钰,季建清,韩宝福,等. 地表剥蚀、下地壳流变与造山作用研究进展[J]. 地球科学进展,2006,21(5): 521-531.]
[93] Vanderhaeghe O. Migmatites, granites and orogeny: Flow modes of partiallymolten rocks and magmas associated with melt/solid segregation in orogenic belts[J].Tectonophysics,2009, 477(3/4): 119-134.
[94]Xu Zhiqin, Yang Jingsui, Ji Shaocheng, et al. On the continental tectonics and dynamics of China[J].Acta Geologica Sinica, 2010, 84(1): 1-29.[许志琴，杨经绥，嵇少丞，等. 中国大陆构造及动力学若干问题的认识[J]. 地质学报,2010, 84(1): 1-29.]
[95]Li Dewei, Ji Yunlong. Laminar flow in the lower continental crust and its significance for continental dynamics[J].Earthquake Geology，2000,22(1):89-96.[李德威，纪云龙. 大陆下地壳层流作用及其大陆动力学意义[J]. 地震地质,2000,22(1):89-96.]