大别造山带后造山隆升过程研究
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摘要
为更全面了解东大别山及北淮阳地区大地构造完整的演化，并为之提供研究实例积累，本研究主要从热年代学及造山后流体特点角度对东大别山及北淮阳构造区碰撞造山后中生代未-新生代初构造隆升活动进行了初步探讨。工作主要涉及磷灰石裂变径迹热年代学及造山后流体包裹体的热力学参数、物质组分及氢氧同位素等特征的研究，采用地质综合分析法探讨了热年代学、流体热力学参数及组分特征可能的构造意义；并用(U-Th)／He低温年代学方法进行了更低温(封闭温度为70℃)热构造年代学及构造意义的初步探讨，获得了对研究区中生代未-新生代初的构造隆升及演化的新认识，主要有以下新收获：
1) 研究区造山后构造隆升主要发生在晚侏罗世-早白垩世和晚白垩世-老第三系期间，隆升样式主要为穹隆隆升和断裂隆升，具有时间、空间格局上的不均一，且缓慢特点；研究区对青藏高原快速隆升没有明显的反应，暗示青藏高原快速隆升时中国东、西部的构造活动分别受不同动力学机制控制；
2) 中生代晚期到新生代早期研究区地壳处于以拉张应力作用控制为主的背景，地壳伸展拉伸，但涉深不大；
3) 晓天-磨子潭断裂在造山后演变为大陆内区域性断裂；
4) 通过实例比较研究，强调利用流体测温数据探讨流体捕获温度、压力和流体~(18)O同位素时应该按照其基本理论要求注重压力校正；
5) 在裂变径迹测定方法改进、磷灰石T-t演化轨迹计算机模拟、近地质时期模拟T-t轨迹“吸热谷”产生原因的初步分析、自发裂变径迹对定年准确度影响的分析、磷灰石U-Th／He年龄的构造意义、系统利用流体信息探讨构造演化等方面的工作开展了有创新或改进性的工作，且效果良好。
This preliminary research focus on the tectonic uplift in late Mesozoic-early
Cenozoic after the main collision oregeny to understand more and detail on the total process of tectonics evolvement in east Dabie Mountain and Beihuaiyuan area. The research works that have been done are: apatite fission track dating, apatite thermal-evolvement patterns; the fluid characteristics including fluid inclusions' microthermometer, the compositions, 5 D - 8 18O, and their geochemistry , thermodynamics parameters. And also analyzed apatite's U-Th/He ages to understand more about the last uplift. The research integrated the all information of apatite thermol-chronology, the thermodynamics parameters and compositions of fluid inclusions and discussed their tectonics implies. We get some improvements understanding in post collision orogeny in researched area which include:
1) There were two main tectonic uplifts in the late of Mesozoic to early Cenozoic. One was in late Jurassic-early Cretaceous and another was in late Cretaceous-early Tertiary. The dome uplift and fault uplift with the heterogeneous evolution in time and space were main two uplift patterns. The uplift of post-orogency of this area was very slow and the amount of exhumation is about 3-4km since Cretaceous and it does not show sharp response for the uplifting of Tibet. It should imply the effect from the subduction and collision of Indian and Asian blocks was very limited in this area. During that the tectonic process in eastern and western of China were controlled by different dynamics mechanisms
2) The researched area was controlled by stretch and extended during late Mesozoic-early Cenozoic;
3) The Xiaotian-Mozitan fault acted just as a main fault in intro-continent. The uplift in Cenozoic was more effected by the stress adjusting in the crust.
4) We tried and did some innovation work and got unproved results which include: dating fission track by a new method, modeling apatite T-t plot of below 120 , analyzing the impact of spontaneous track on dating and fluid inclusion's tectonic implies. And the comparing research on fluid inclusions shows the pressure correction is very important to get fluid inclusions' trapped temperature, pressure and 18O isotopic composition.
1) 研究区造山后构造隆升主要发生在晚侏罗世-早白垩世和晚白垩世-老第三系期间，隆升样式主要为穹隆隆升和断裂隆升，具有时间、空间格局上的不均一，且缓慢特点；研究区对青藏高原快速隆升没有明显的反应，暗示青藏高原快速隆升时中国东、西部的构造活动分别受不同动力学机制控制；
2) 中生代晚期到新生代早期研究区地壳处于以拉张应力作用控制为主的背景，地壳伸展拉伸，但涉深不大；
3) 晓天-磨子潭断裂在造山后演变为大陆内区域性断裂；
4) 通过实例比较研究，强调利用流体测温数据探讨流体捕获温度、压力和流体~(18)O同位素时应该按照其基本理论要求注重压力校正；
5) 在裂变径迹测定方法改进、磷灰石T-t演化轨迹计算机模拟、近地质时期模拟T-t轨迹“吸热谷”产生原因的初步分析、自发裂变径迹对定年准确度影响的分析、磷灰石U-Th／He年龄的构造意义、系统利用流体信息探讨构造演化等方面的工作开展了有创新或改进性的工作，且效果良好。
This preliminary research focus on the tectonic uplift in late Mesozoic-early
Cenozoic after the main collision oregeny to understand more and detail on the total process of tectonics evolvement in east Dabie Mountain and Beihuaiyuan area. The research works that have been done are: apatite fission track dating, apatite thermal-evolvement patterns; the fluid characteristics including fluid inclusions' microthermometer, the compositions, 5 D - 8 18O, and their geochemistry , thermodynamics parameters. And also analyzed apatite's U-Th/He ages to understand more about the last uplift. The research integrated the all information of apatite thermol-chronology, the thermodynamics parameters and compositions of fluid inclusions and discussed their tectonics implies. We get some improvements understanding in post collision orogeny in researched area which include:
1) There were two main tectonic uplifts in the late of Mesozoic to early Cenozoic. One was in late Jurassic-early Cretaceous and another was in late Cretaceous-early Tertiary. The dome uplift and fault uplift with the heterogeneous evolution in time and space were main two uplift patterns. The uplift of post-orogency of this area was very slow and the amount of exhumation is about 3-4km since Cretaceous and it does not show sharp response for the uplifting of Tibet. It should imply the effect from the subduction and collision of Indian and Asian blocks was very limited in this area. During that the tectonic process in eastern and western of China were controlled by different dynamics mechanisms
2) The researched area was controlled by stretch and extended during late Mesozoic-early Cenozoic;
3) The Xiaotian-Mozitan fault acted just as a main fault in intro-continent. The uplift in Cenozoic was more effected by the stress adjusting in the crust.
4) We tried and did some innovation work and got unproved results which include: dating fission track by a new method, modeling apatite T-t plot of below 120 , analyzing the impact of spontaneous track on dating and fluid inclusion's tectonic implies. And the comparing research on fluid inclusions shows the pressure correction is very important to get fluid inclusions' trapped temperature, pressure and 18O isotopic composition.
引文
.Bakker, R.J, Jansen, J.B.,H., Experimental post-entrapment water loss from synthetic CO2-H2O inclusions in natural quartz, Geochim. Cosmochim. Acta, 1991,55:2215-2230
.Buck, W.R, Modes of continental lithospheric extension, Journal Geophysics Research, 1991, 96: 20161-20178
A.J. Hurford and P. F. Green, The zeta age calibration of fission track dating, Isotope geosciences, 1983, 1:285-317
Allerton, S., Escartin,J. R., Searle,C, Extremely asymmetric magmatic accretion of oceanic crust at the ends of slow-spreading ridge segments, Geology, 2000, 28(2): 179-182
Ames, L, Tilton,G.R., Zhou, G., Timing of collision of the Sino-Korean and Yangtze Cratons: U-Pb zircon dating of coesite-bearing eclogites, Geology, 1993,21:239-342
Anonymous, post-collisional magmatic, Lithos, Special edit, 1998,45.
B.Cong Ultrahigh-pressure metamorphic rocks in the Dabieshan-Sulu region of China, Science Press, 1995, Beijing.
Batt, G. E., Brandon, M.T., Farley, K.A., Tectonic synthesis of the Olympic Mountains segment of the Cascadia wedge, using two-dimensional thermal and kinematic modeling of thermochronological ages, J. Geophys. Res. 2001,106 (B11):26,731 26,742
Bird, P., Toksoz, M.N., Sleep,N.H., Thermal and mechanical models of continent-continent convergent zones; Journal of Geophysical Research, 1975, 80:4405-4416
Bodnar, R.J., Revised equation and table for determining the freezing point depression of H2O-NaCl solutions, Geochim. Cosmochim. Acta, 1993,57:683-684
Bonini,M., Sokoutis, D., Mulugeta,G., Boccaletti,M., Corti,G., Dynamics of magma emplacement in centrifuge models of continental extension with implications for flank volcanism, Tectonics, 2001,20(6): 1053-65
Boulier, A.M., Fluid inclusions:tectonic indicators, Journal of Structural Geology, 1999,1229-1235
Chen,B., Jahn,B., Wei, C., Petrogenesis of Mesozoic granitoids in the Dabie UHP complex, central China; trace element and Nd-Sr isotope evidence,Lithos, 2002, 60(1-2): 67-88
Christeson, G. L, Nakamura, Y., .Buffler, R.T, Morgan, J., Wamer, M., Deep crustal structure of the Chicxulub impact crater, J. Geophys. Res. 2001, 106 (B10): 21,751-21,765
Coward,M.P., Dewey, J.F., Hancock,P.L., Continental Extensional Tectonics, Blackwell,Oxford, 1987
Crowley, K.D., Thermal significance of fission track lenth distributions, Nuclear Tracks, 1985,10:311-322
Davies, J.H., Vonblanckenburg,F., Slab breakoff: a mondel of lithosphere detachment and its test in the magmatism and deformation of collisional orogens, Earth & Planet Science Letter, 1955, 129:85-102
Davies, G.F., Thermomechanical erosion of the lithosphere by mantle plumes, Journal Geophysics Research, 1995,99:15709-15722
DeCelles, P.G., Robinson, D. M., Quade,J., Ojha,.T.P., Stratigraphy, structure, and tectonic evolution of the Himalayan fold-thrust belt in western Nepal Tectonics, 2001, 20(4): 487-509
DiPietro,J.A., Isachsen,C. E., U-Pb zircon ages from the Indian plate in northwest Pakistan and their significance to Himalayan and pre-Himalayan geologic history, Tectonics 2001, 20(4): 510-518
Dobrzhinetskaya, L.F., Microdiamond in high-grade metamorphic rocks of the Western Gneiss region, Norwqy, Gology, 1995, 23:597-600
Donelick, R.A., Ketcham R. A., Carlson, W. D., Variability of apatite fission-track annealing kinetics
Ⅱ:crystalograpic orientation effects, American Mineralogist, 1999, 84:1224-1234
Eide,E.A., McWilliams, M.O., Liou,J.G., ~(40)Ar/~(39)Ar geochronology and exhumation of high-pressure to ultrahigh-pressure metamorphic rocks in east-central China, Geology, 1994,22:601-604
Ernst, W.G., Zhou, J., Liou, J.G, Eide, E., Wang, X., High-pressure and superhigh-pressure metamorphic terrances in the Qinling-Dabie Mountain belt, central China, Early-to Mid- Phamerozoic accretion of the western paleo-pacific rim, Pacific science association information bulletin 1991, 43: 6-15
Ernst, W.G., Liou,J.G, Hacker, B.R. Petrotectonic significance of high and ultrhigh-pressure metamorphic belts: inferences for subduction zone histories, International Geology Review: 1994,36:213-237
Fitzgerald,P.G.., Munoz.,J.A., Coney, P.J., Baldwin, S.L., Asymmetric exhumation across the Pyrenean orogen: implications for the tectonic evolution of a collisional orogen, Earth and planetary Science Letters, 1999, 173:157-170
Gleadow, A.J.W., Duddy, I. R., Green P. F., Lovering,J.F., Confined fission track lengths in apatite: a diagnostic tool for thermal history analysis, Contrib. Mineral Petrol. 1986, 94:405-415
Godin,L., Parrish, R., Brown,R.L., Hodges, K.V., Crustal thickening leading to exhumation of the Himalayan Metamorphic core of central Nepal: Insight from U-Pb Geochronology and ~(40)Ar/~(39)Ar Thermochronology, Tectonics 2001, 20(5): 729-741
Green, P.F., Statistics in fission-track dating [J]. Nuclear Tracks, 1981, 5(1/2):77～86
Green, P.F., Duddy, I. R., Laslett, G. M., Can fission trak annealing in apatite be described by first order kinetics? Earth planet sciences letter, 1988,87:216-228
Hacker,B.R, Ratschbacher, L., Webb, L., Ireland, T.R., alker, D.W, Dong,S., U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie Orogen, China Earth and Planetary Science Letters, 1998,161(1-4):215-230
Hacker,B.R., Ratschbacher, L, Webb, L, McWilliams, M.O., Exhumation of ultrahigh-pressure continental crust in east central China: late Triassic-early Jurassic tectonic unroofing, Journal of Geophysical Research, 2000, 105(B6): 13339-13364
Hall, D.L., Freezing point depression of NaCl-KCl-H_2O solution, Economic Geology, 1988, 83:197-202
Hall, D.L., Stemer, S.M., Preferential waterloss from synthetic fluid inclusions. Contribution Mineral Petrology, 1993,114: 489-504
Hardebeck, J.L, Hauksson,E., Crustal stress field in southern California and its implications for fault mechanics, J. Geophys. Res. 2001,106 (B10): 21,859-21,875
Hodges, K.V., Hurtado, J.M., Whipple, K.,Southward extrusion of Tibetan crust and its effect on Himalayan tectonics, Tectonics, 2001, 20(6):799-809
Hofmann ,A., Dirks, H. G.,Paul., M H., Jelsma,A., Horizontal tectonic deformation geometries in a late Archaean sedimentary sequence, Belingwe greenstone belt, Zimbabwe,Tectonics 2001, 20(6): 909-932
Hollistar, L.S., Enrichment of CO2 in fluid inclusions in quartz by removal of H_2O during crystal-plastic deformation. Journal Structural Geology, 1990,7:895-901
House,M.A., Wemicke,B. P., .Farley, K. A., Dating topography of the Sierra Nevada, California, using apatite (U-Th)/He ages, Nature, 1998, 396(5): 66-69
Hsu,K. J., Wang, Q., Li,J., Tectonic evolution of Qinling Mountains, China, Eclogae Geologicae Helvetiae. 1991, 80(3): 735-752
Huismans R.S., Podladchikov, Y. Y., Cloetingh, S., Dynamic modeling of the transition from passive to active rifting, application to the Pannonian basin, Tectonics, 2001,. 20 (6): 1021-1039
Hurford A.J., Green,P. F., A users'guide to fission track dating calibration, Earth Planet Science Letter, 1982, 59:343-354
Isacks, B., Molnar, P., Mantel earthquake mechanisms and sinking of the lithosphere, Nature, 1969, 223:1121-1124
Isacks, B.L., Oliver, J, Sykes, L.R., Seismology and the new global tectonics, Journal of Geophysical Research, 1968,73:5855-5900
Jahn, B., Wu,F., .Lo,C,Tsai, C., Crust-mantle interaction induced by deep subduction of the continental crust; geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie Complex, central China, Chemical Geology, 1999,157(1-2): 119-146
Johnson,E.L., Hollister, L. S., Syndeformational fluid trapping in quartz:determining the p-T conditions of deformation from fluid inclusions and the formation of pure CO_2 fluid inclusions during grain-boundary migration, Journal Metamorphic Geology, 1995,13:239-249
Jonckheere,R., Van den haute., P., De Corte,F., Wagner.,G.A, Fission track Age Calibration]-the next generation Abstracts of the Ninth International Conference on Fission Track Dating and Thermochronology, Lorne, Australia. Geological society of Australia abstracts series, 2000, 58, 187～188
Kohn,B.P, Gleadow, A.J.W, Cox, S.J.D., Denudation history of the Snowy Mountains: constraints from apatite fission track thermochronology, Earth and planetary science letters, 1998, 164:451-465
Laslett, G.M., Green,P.F., Duddy I.R, Thermaal annealing of fission tracks in apatite. 2. A quantitative analysis, Chemical Geology, Isotope Geoscience Section, 1987,65:1-13
Laslett, G.M., Kendall, W. S., Gleadow A. J. W., Duddy, I. R., Bias in measurement of fission-track length distributions Nucl. Tracks, 1982, 6:79-85
Lewis, J. C., Byrne,T. B., Fault kinematics and past plate motions at a convergent plate boundary: Tertiary Shimanto Belt, southwest Japan, Tectonics, 2001, 20(4), 548-565
Li, F., Huang,Y., Geochemical and geochronological constraints on the suture location between the North and South China Blocks in the Dabie orogen, Central China, Physics and Chemistry of the Earth, 2001,26:655-672
Li, S., Liou,D., Chen,Y, The Sm-Nd isotopic age of coesite-bearing eclogite from the southern Dabie Mountains, Chinese Science Bulletin, 1992,37(190):1638-1641
Li, S., Chen,Y, Cong,B., Collision of the North China and Yangtze Blocks and formation of ecoesite-bearing eclogites: timeing and processes, Chemical Geology, 1993,109:70-89
Liou,Y., Lo,C., Tsai,C., Chung, S., Qiu, J., Li,X., ~(40)Ar/~(39)Ar geochronology of volcanic and intrusive rocks in the Dabie and Sulu terranes, eastern China, and their tectonic implications,Journal of the Geological Society of China, 1999,42(4):493-520
Maruyama,S., Liou, J.G., Zhang,R., Tectonic evolution of the ultrhigh-pressure (UHP) and high-pressure (HP) metamophic belts from central China, The Island Arc, 1994, (3): 112-121
Matsuhisa, Y., Goldsmith,J.R.,Clayton, R.N.,Oxygen isotopic fractionation in the system quartz-albite-anorthite-water, Geochimica et Cosmochimica Acta, 1979, 43(7): 1131-1140
Minear, J.W., Toksoz, M.N., Thermal regime of a downgoing and new global tectonics, Journal of Geophysical Research, 1970, 1397-1419
P. Philippot, P. Chevallier, C. Chopin, J. Duhessy, fluid comosition and evolution in coesite-bearing rocks Dora Maira massif, Western Alps: implications for element rechycling during subduction, Contributions to Mineralogy Petrology, 1995,121:29-44
Rahn,M.K., Grasemann,B., Fission track and numerical thermal modeling of differential exhumation of the Glarus thrust plane (Switzerland), Earth and Planetary Science Letters, 1999, 169:245-259
Ratschbacher, L., Hacker, B. R., Webb,L. E., Dong,S., exhumation of the ultrahigh-pressure continental crustin East-Central China: Cretaceous and Cenozoic unroofing and the Tan-Lu fault, Journal of
Geophysical Research, 2000, 105 (B6): 13321-13338
Raza.,A., Mesozoic thermo-tectonic evolution of central eastern Australia and the Waltemata Basin, North Island, New Zealand: A fission track study, International Geology Review, 1997, 39: 107-124
Reiners, P.W., Farley, K.A., Helium diffusion and (U-Th)/He thermochronometry of titanite: Geochimica et Cosmochimica Acta, 1999, 63: 3845-3859
Reiners, P.W., Ehlers, T.A, Garver, J. I., Late Miocene exhumation and uplift of the Washington Cascade Range, Geology(Boulder),2002, 30 (9): 767-770
Roedder, E., Liquid CO_2 inclusion in olivine bearing and phenocrysts from basalts, America Mineral. 1965, 50:1746-1786
Roedder, E., Fluid inclusions. Res.Mineralogy, 1984.12:337-359
Roselle, G. T., Engi,M., Ultra high pressure (UHP) terrains; lessons from thermal modeling,American Journal of Science, 2002,302(5):410-441
Sack, P.E., Secor Jr, S.T., Delamination in collisional orogens, Geology, 1990, 18:999-1002
Santosh,M., Nature and evolution of metamorphic fluid in the precambrian khondalites of Kerala, South India, Precambrian Research, 1986,33:283-302
Sterner, S.M., Bodnar, R.J., Synthetic fluid inclusions: Re-equilibration of fluid inclusions in quartz during laboratory-simulated metamorphic burial and uplift, Journal Metamorphic Geology, 1989,7:243-260
Suo,S., Zhong,Z, You,Z., Extensional deformation of post ultrahigh-pressure metamorphism and exhumation process of ultrahigh-pressure metamorphic rocks in the Dabie Massif, China, Science in China. Series D, 2000,43(3):225-236
Tagami,T., Nishimura S., Determination of zeta calibration constant for fisson track dating, Nuclear Tracks Radiation Measurement, 1987, 13:127～130
Tsai, C.H., Lo,C.H., Liou, J.G., Jahn, B., Evidence against subduction-related magmatism for the Jiaoziyan Gabbro, northern Dabie Shan, China, Geology (Boulder), 2000,28(10):943-946
Turner, S., Sandiford,M., Foden, J., Some geodynamic and compositional constraints on 'postorogenic' magmatism, Geoloy, 1992,931-934
Wagner, G.A., Haute. P. V., Fission-track dating, The Netherlands. Ferdinand Enke Verlag Stuttgart, Dordrecht, 1992, 285
Wang, X., Liou,G., Mao,H.K. Coesite-bearing eclogite from the Dabie Mountains in central China,Geology, 1989,17:1085-1088
Warnock,A.C., Zeitler, P.K., Wolf, R.A., S Bergman,.C., An evaluation of low-temperature apatite U-Th/He thermochronometry: Geochimica et Cosmochimica Acta, 1997, 61: 5371-5377
Wessel,P., Global distribution of seamounts inferred from gridded Geosat/ERS-1 altimetry, J. Geophys. Res. 2001. 106(B9): 19,431-19,442
Whitehead,Jr.,J.A., Dick, H.J.B., Schouten, H., A mechanism for magmatic accretion under spreading centers, Nature, 1984,312:146-147
Wickham, S.M., Oxburgh, E.R., Continental rifts as a setting for regional metamorphism, Nature, 1985, 318:330-333
Xiao,Y., Hoefs,J., van den Kerkhof, A. M., Fiebig, J., Zheng, Y., Fluid history of UHP metamorphism in Dabie Shall, China:a fluid inclusion and oxygen isotope study,2000
Xu,S., Okay, A, I, Ji, S. et al, Diamond from metamorphic rocks and its implication for tetonic setting, Science, 1992,256:80-82
Zhang,R.Y., Liou,J.G., Cong,B.L., Talc-,magnesite-and Ti-clinohumite-bearing ultrahigh-pressure
meta - mafic and ultramafic complex in the Dabie Mountains, China, Journal of Petrology, 1995,36:1011-1037
Zheng,Y. F., Fu, B., Cong,B., Extreme ~(18)O depletion in eclogite from the Su-Lu terane in east China, Europen Journal of Mineral, 1996,317-323
安徽省地质局，中华人民共和国区域地质调查报告，六安、岳西幅(1：20万)，1974；
安徽省地质矿产局，安徽省区域地质志，地质出版社，1987，北京
陈道公，Etienne Deloule，夏群科，程昊，北大别片麻岩中锆石U-Pb年龄离子探针初步测定，岩石学报 2000，(2)
陈道公，李彬贤，夏群科，吴元保，程昊，大别超高压碰撞造山带岩石锆石U-Pb同位素框架年代学，矿物岩石地球化学通报，2001，20(4)：253-255
从柏林，王清晨，大别山-苏鲁超高压变质带研究的最新进展，科学通报，1999，44(11)：1127-1132
杜建国，顾连兴，孙先如，岳书仓，大别山带的流体系统与成矿作用，地质学报，2001，75(4)：507-517
杜建国，徐晓春，孙先如，戴圣潜，大别造山带核部罗田陈林沟金矿成矿时代，贵金属地质，2000，9(2)：91-96
杜建国，张鹏，大别造山带北部的中生代火山岩，现代地质，1999，13(1)：57-65
方中，徐士进，王汝成，大别山超高压变质带花岗岩两期变质作用和造山带抬升的年代学证据，矿物岩石地球化学通报，2001，20(2)：256-258．
傅斌，肖益林，J. L. R. Touret, A. M. Van den Kerkhof, J. Hoefs，郑永飞，大别山双河和碧溪岭超高压变质岩流体包裹体研究，岩石学报，2000，16(1)：119-126
郭锋，吴有林，范蔚茗，林舸，湖南省宁远——道县中生代玄武岩中辉长岩包体的岩石学初步研究，大地构造与成矿学，1996，1：38-45
郭震宇，董火根，郭令智，大别造山带变质岩地层年龄及其构造意义，地层学杂志，1998，22(3)：185-195
郭正府，邓晋福，许志琴，莫宣学，罗照华，青藏东昆仑晚古生代末—中生代中酸性火成岩与陆内造山过程，现代地质，1998，12(3)：344-352
韩喜球，马维林，金翔龙，杨树锋，冲绳海槽南部玄武岩中的流体包裹体成分及其意义，海洋与湖沼，2002，(01): 42-46
韩郁菁，张泽明，高压超高压变质作用中的流体，地学前缘，1996，3(3-4)：222-229
郝杰，刘小汉，桐柏大别碰撞造山带大型推覆—滑脱构造及其演化，地质科学，1988，(1)：1-10
季克俭，王立本，热液源研究的重要进展和“三源”交待成矿学说，地学前缘，1994，1(4)：126～131
简平，杨巍然，造山带构造年代学基本问题——论同位素体系与变质作用的关系，地球科学进展，1998，13(5)：452-456
江万，莫宣学，赵崇贺，郭铁鹰，张双全，矿物裂变径迹年龄与青藏高原隆升速率研究，地质力学学报，1998，4(1)：13-18
金成伟，郑祥身，大别岳西地区花岗岩类岩石学及其成因，岩石学报，1998，14(4)：493-502
李曙光，黄方，李晖，大别-苏鲁造山带碰撞后的岩石圈拆离，科学通报，2001，46(17)：1487-1491
李曙光，肖益林，刘德良，大别山石马地区石榴黑云片麻岩的Sm-Nd、K-Ar年龄及冷却速率，地质科学1995，30(2)：174-182
李一良，郑永飞，傅斌，大别山榴辉岩中石英脉的氧同位素研究，中国科学(D辑)，2001，31(4)：305-314
李勇，孙爱珍，龙门山造山带构造地层学研究，地层学杂志，2000，03：201-206
李忠，李任伟，孙枢，张雯华，大别地块北缘侏罗系花岗岩类砾石的Rb-Sr年代学特征，科学通报 2001(7)
刘斌，沈昆，流体包裹体热力学，地质出版社，1999，北京
刘凤山，石准立，太行山—燕山地区中生代花岗岩生成动力学机制与陆内造山作用，地球学报1998，19(1)：13-18
刘和甫，盆山耦合类型，地学前缘2000，7(4)：469-475
刘景波，叶凯，从柏林，范宏瑞，大别山超高压变质带片麻岩锆石中重晶石和硬石膏包裹体及其意义，岩石学报，2000，16(4)：482-484
刘文灿，王果胜，北淮阳地区中生代逆冲推覆构造，现代地质，1998，13(2)：143-149
卢焕章，李秉伦，沈昆等，包裹体地球化学，地质出版社，1990，北京
路玉林，钱存超，周存亭，安徽岳西脉状英安质角砾熔岩的发现、特征及意义，安徽地质，1996，6(4)：41-46
毛建仁，陶奎元，杨祝良，朱云鹤，薛怀民，Geodynamic Background of the Mesozoic Intracontinental Magmatism in Southeast China, Chinese Journal of Geochemistry 1997, 16(3):230-239
潘国强,钱存超 贾十军，安徽大别山腹地中生代火山岩的发现及其地质意义，安徽地质，1998，8(1)：27-31
桑隆康，王人镜，张泽明等，九资河-天堂寨地区燕山晚期花岗岩与大别山带核部隆升，地质学报，2000，74(3)：234-246
索书田，钟增球，游振东，大别地块超高压变质期后伸展变形及超高压变质岩石折返过程，中国科学(D辑)，2000，30(1)：9-17
陶士振，卫延召，刘德良，杨晓勇，造山带超高压变质流体中气体组成及成藏条件初探，地质科学，2001，36(1)：91-100
王成善，丁学林，喜马拉雅的隆升及其沉积反应研究新进展，地质科技情报，1998，17(1)：1-7(3)：338-344
王椿镛，张先康，陈步云，大别造山带的地壳结构研究，中国科学(D辑)，1997，27(3)：221-226
王光杰，滕吉文，张中杰，中国华南大陆及陆缘地带的大地构造基本格局，地球物理学进展，2000，15(03)：25-44
王国灿，杨巍然，大别造山带中新生代隆升作用的时空格局—构造年代学证据，地球科学，1998，23(5)：461-466
王强，邱家骧，王人镜，大别造山带核部典型燕山期花岗岩岩浆演化的p-T轨迹，矿物岩石，1999，19(4)：15-20
王强，赵振华，熊小林，桐柏—大别造山带燕山晚期A型花岗岩的厘定，岩石矿物学杂志，2000，19(4)：297-315
王清晨，从柏林，大别山超高压变质带的大地构造框架，岩石学报，1998，14(4)：481-492
王人镜，王强，何勇，大别山造山带核部九资河—天堂寨花岗岩的成因和时代，矿物岩石地球化学通报，1998，17(4)：224-228
王岳军，北淮阳晚中生代火山岩定年及火山砾石地球化学：对大别灰色片麻岩隆升和中生代地层格架的约束，科学通报，2002，47(20)：1528-1534
魏春景，单振刚，张立飞等，北大别榴辉岩的确定及其地质意义，科学通报，1996，42(17)：1832-1835
魏春景，张立飞，王式洗，安徽省大别山东段中生代高钾花岗质岩石及其地质意义，中国科学(D辑)，2000，30(4)：355-363
吴堑虹，刘厚昌，(U-Th)/He定年—低温热年代学研究的一种新技术，地球科学进展，2002，(1)：126-131
吴珍汉，崔盛芹，吴淦国等，燕山山脉隆升过程的热年代学分析，地质论评，2000，(1)：49-57
夏新宇，王先彬，陈江峰，葛宁洁，大别山双河地区超高压变质岩流体包裹体成分及二氧化碳碳同位
素研究，中国科学D辑，1999，29(4)：314-320
徐启东，张本仁，单光祥，蒋敬业，马振东，大别造山带中生代花岗岩类成分的时空分布与造山带演化的关系，地球科学，1997，22(6)：595-598
徐启东，钟增球，索书田，齐先茂，桐柏——大别地区中温热液金矿床成矿流体性质与沉淀机理，矿床地质，1995，1：59-72
徐树桐，江来利，刘贻灿等．大别山区(安徽部分)的构造格局和演化过程．地质学报，1992，66(1)：1～13
徐树桐，刘贻灿，吴维平，江来利，大别山造山带研究的主要进展及存在问题，自然科学进展796-803
杨坤光，马昌前，许长海，杨巍然，北淮阳构造带与大别造山带的差异性隆升，中国科学，1999，29(2)：97-103
杨坤光，马昌前，杨巍然，北淮阳马畈加里东岩体的研究及其地质意义，地球科学，1998，23，(3)：236-241
杨巍然，王国灿，简平，大别造山带构造年代学，中国地质大学出版社，2000，武汉
杨文采，余长青，根据地球物理资料分析大别—苏鲁超高压变质带演化的运动学与动力学，地球物理学报，2001，44(3)：346-359
杨晓勇，郑永飞，刘德良，陶士振，中国东部橄榄岩包体和榴辉岩中CO_2流体包裹体的碳同位素组成，岩石学报，2000，16(4)：473-481
杨志华，苏生瑞，李勇，张传林，周美夫，赵太平，中国大地构造几个重大问题的探讨，地学前缘，2001，8(2)：395-406
杨志华，苏生瑞，李勇，张传林，周美夫，赵太平，中国大地构造几个重大问题的探讨，地学前缘2001，(2)
张鸿翔，徐志方，黄智龙，刘从强，地幔流体基本特征及成因，地质地球化学，2000，28(2)：1-7
张泽明，韦必则，韩郁菁，游振东，鄂北高压榴辉岩相变质带的变质、变形和流体演化，岩石学报1999，15(1)：48-56
郑度，林振耀，张雪芹，青藏高原与全球环境变化研究进展，地学前缘，2002，9(1)：95-102
郑建平，路凤香，华北地台深部地幔流体的组成——来自金刚石不纯净组分的报道，地质科学，1998，33(1)：52-60
郑永飞，魏春生，王峥嵘等，大龙山岩体冷却史及其成矿关系的同位素研究，地质科学，1997，32(4)：465-477
郑永飞，陈江峰，稳定同位素地球化学，科学出版社，2000，北京
郑永飞，傅斌，李一良，肖益林，龚冰，大别山超高压变质作用期前和期后水岩相互作用的氢氧同位素证据，1999，29(2)：113-121
周泰禧，陈江峰，张巽，等，北淮阳花岗岩—正长岩带地质地球化学特征及其大地构造意义，地质论评，1995，2：144-151
.Buck, W.R, Modes of continental lithospheric extension, Journal Geophysics Research, 1991, 96: 20161-20178
A.J. Hurford and P. F. Green, The zeta age calibration of fission track dating, Isotope geosciences, 1983, 1:285-317
Allerton, S., Escartin,J. R., Searle,C, Extremely asymmetric magmatic accretion of oceanic crust at the ends of slow-spreading ridge segments, Geology, 2000, 28(2): 179-182
Ames, L, Tilton,G.R., Zhou, G., Timing of collision of the Sino-Korean and Yangtze Cratons: U-Pb zircon dating of coesite-bearing eclogites, Geology, 1993,21:239-342
Anonymous, post-collisional magmatic, Lithos, Special edit, 1998,45.
B.Cong Ultrahigh-pressure metamorphic rocks in the Dabieshan-Sulu region of China, Science Press, 1995, Beijing.
Batt, G. E., Brandon, M.T., Farley, K.A., Tectonic synthesis of the Olympic Mountains segment of the Cascadia wedge, using two-dimensional thermal and kinematic modeling of thermochronological ages, J. Geophys. Res. 2001,106 (B11):26,731 26,742
Bird, P., Toksoz, M.N., Sleep,N.H., Thermal and mechanical models of continent-continent convergent zones; Journal of Geophysical Research, 1975, 80:4405-4416
Bodnar, R.J., Revised equation and table for determining the freezing point depression of H2O-NaCl solutions, Geochim. Cosmochim. Acta, 1993,57:683-684
Bonini,M., Sokoutis, D., Mulugeta,G., Boccaletti,M., Corti,G., Dynamics of magma emplacement in centrifuge models of continental extension with implications for flank volcanism, Tectonics, 2001,20(6): 1053-65
Boulier, A.M., Fluid inclusions:tectonic indicators, Journal of Structural Geology, 1999,1229-1235
Chen,B., Jahn,B., Wei, C., Petrogenesis of Mesozoic granitoids in the Dabie UHP complex, central China; trace element and Nd-Sr isotope evidence,Lithos, 2002, 60(1-2): 67-88
Christeson, G. L, Nakamura, Y., .Buffler, R.T, Morgan, J., Wamer, M., Deep crustal structure of the Chicxulub impact crater, J. Geophys. Res. 2001, 106 (B10): 21,751-21,765
Coward,M.P., Dewey, J.F., Hancock,P.L., Continental Extensional Tectonics, Blackwell,Oxford, 1987
Crowley, K.D., Thermal significance of fission track lenth distributions, Nuclear Tracks, 1985,10:311-322
Davies, J.H., Vonblanckenburg,F., Slab breakoff: a mondel of lithosphere detachment and its test in the magmatism and deformation of collisional orogens, Earth & Planet Science Letter, 1955, 129:85-102
Davies, G.F., Thermomechanical erosion of the lithosphere by mantle plumes, Journal Geophysics Research, 1995,99:15709-15722
DeCelles, P.G., Robinson, D. M., Quade,J., Ojha,.T.P., Stratigraphy, structure, and tectonic evolution of the Himalayan fold-thrust belt in western Nepal Tectonics, 2001, 20(4): 487-509
DiPietro,J.A., Isachsen,C. E., U-Pb zircon ages from the Indian plate in northwest Pakistan and their significance to Himalayan and pre-Himalayan geologic history, Tectonics 2001, 20(4): 510-518
Dobrzhinetskaya, L.F., Microdiamond in high-grade metamorphic rocks of the Western Gneiss region, Norwqy, Gology, 1995, 23:597-600
Donelick, R.A., Ketcham R. A., Carlson, W. D., Variability of apatite fission-track annealing kinetics
Ⅱ:crystalograpic orientation effects, American Mineralogist, 1999, 84:1224-1234
Eide,E.A., McWilliams, M.O., Liou,J.G., ~(40)Ar/~(39)Ar geochronology and exhumation of high-pressure to ultrahigh-pressure metamorphic rocks in east-central China, Geology, 1994,22:601-604
Ernst, W.G., Zhou, J., Liou, J.G, Eide, E., Wang, X., High-pressure and superhigh-pressure metamorphic terrances in the Qinling-Dabie Mountain belt, central China, Early-to Mid- Phamerozoic accretion of the western paleo-pacific rim, Pacific science association information bulletin 1991, 43: 6-15
Ernst, W.G., Liou,J.G, Hacker, B.R. Petrotectonic significance of high and ultrhigh-pressure metamorphic belts: inferences for subduction zone histories, International Geology Review: 1994,36:213-237
Fitzgerald,P.G.., Munoz.,J.A., Coney, P.J., Baldwin, S.L., Asymmetric exhumation across the Pyrenean orogen: implications for the tectonic evolution of a collisional orogen, Earth and planetary Science Letters, 1999, 173:157-170
Gleadow, A.J.W., Duddy, I. R., Green P. F., Lovering,J.F., Confined fission track lengths in apatite: a diagnostic tool for thermal history analysis, Contrib. Mineral Petrol. 1986, 94:405-415
Godin,L., Parrish, R., Brown,R.L., Hodges, K.V., Crustal thickening leading to exhumation of the Himalayan Metamorphic core of central Nepal: Insight from U-Pb Geochronology and ~(40)Ar/~(39)Ar Thermochronology, Tectonics 2001, 20(5): 729-741
Green, P.F., Statistics in fission-track dating [J]. Nuclear Tracks, 1981, 5(1/2):77～86
Green, P.F., Duddy, I. R., Laslett, G. M., Can fission trak annealing in apatite be described by first order kinetics? Earth planet sciences letter, 1988,87:216-228
Hacker,B.R, Ratschbacher, L., Webb, L., Ireland, T.R., alker, D.W, Dong,S., U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie Orogen, China Earth and Planetary Science Letters, 1998,161(1-4):215-230
Hacker,B.R., Ratschbacher, L, Webb, L, McWilliams, M.O., Exhumation of ultrahigh-pressure continental crust in east central China: late Triassic-early Jurassic tectonic unroofing, Journal of Geophysical Research, 2000, 105(B6): 13339-13364
Hall, D.L., Freezing point depression of NaCl-KCl-H_2O solution, Economic Geology, 1988, 83:197-202
Hall, D.L., Stemer, S.M., Preferential waterloss from synthetic fluid inclusions. Contribution Mineral Petrology, 1993,114: 489-504
Hardebeck, J.L, Hauksson,E., Crustal stress field in southern California and its implications for fault mechanics, J. Geophys. Res. 2001,106 (B10): 21,859-21,875
Hodges, K.V., Hurtado, J.M., Whipple, K.,Southward extrusion of Tibetan crust and its effect on Himalayan tectonics, Tectonics, 2001, 20(6):799-809
Hofmann ,A., Dirks, H. G.,Paul., M H., Jelsma,A., Horizontal tectonic deformation geometries in a late Archaean sedimentary sequence, Belingwe greenstone belt, Zimbabwe,Tectonics 2001, 20(6): 909-932
Hollistar, L.S., Enrichment of CO2 in fluid inclusions in quartz by removal of H_2O during crystal-plastic deformation. Journal Structural Geology, 1990,7:895-901
House,M.A., Wemicke,B. P., .Farley, K. A., Dating topography of the Sierra Nevada, California, using apatite (U-Th)/He ages, Nature, 1998, 396(5): 66-69
Hsu,K. J., Wang, Q., Li,J., Tectonic evolution of Qinling Mountains, China, Eclogae Geologicae Helvetiae. 1991, 80(3): 735-752
Huismans R.S., Podladchikov, Y. Y., Cloetingh, S., Dynamic modeling of the transition from passive to active rifting, application to the Pannonian basin, Tectonics, 2001,. 20 (6): 1021-1039
Hurford A.J., Green,P. F., A users'guide to fission track dating calibration, Earth Planet Science Letter, 1982, 59:343-354
Isacks, B., Molnar, P., Mantel earthquake mechanisms and sinking of the lithosphere, Nature, 1969, 223:1121-1124
Isacks, B.L., Oliver, J, Sykes, L.R., Seismology and the new global tectonics, Journal of Geophysical Research, 1968,73:5855-5900
Jahn, B., Wu,F., .Lo,C,Tsai, C., Crust-mantle interaction induced by deep subduction of the continental crust; geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie Complex, central China, Chemical Geology, 1999,157(1-2): 119-146
Johnson,E.L., Hollister, L. S., Syndeformational fluid trapping in quartz:determining the p-T conditions of deformation from fluid inclusions and the formation of pure CO_2 fluid inclusions during grain-boundary migration, Journal Metamorphic Geology, 1995,13:239-249
Jonckheere,R., Van den haute., P., De Corte,F., Wagner.,G.A, Fission track Age Calibration]-the next generation Abstracts of the Ninth International Conference on Fission Track Dating and Thermochronology, Lorne, Australia. Geological society of Australia abstracts series, 2000, 58, 187～188
Kohn,B.P, Gleadow, A.J.W, Cox, S.J.D., Denudation history of the Snowy Mountains: constraints from apatite fission track thermochronology, Earth and planetary science letters, 1998, 164:451-465
Laslett, G.M., Green,P.F., Duddy I.R, Thermaal annealing of fission tracks in apatite. 2. A quantitative analysis, Chemical Geology, Isotope Geoscience Section, 1987,65:1-13
Laslett, G.M., Kendall, W. S., Gleadow A. J. W., Duddy, I. R., Bias in measurement of fission-track length distributions Nucl. Tracks, 1982, 6:79-85
Lewis, J. C., Byrne,T. B., Fault kinematics and past plate motions at a convergent plate boundary: Tertiary Shimanto Belt, southwest Japan, Tectonics, 2001, 20(4), 548-565
Li, F., Huang,Y., Geochemical and geochronological constraints on the suture location between the North and South China Blocks in the Dabie orogen, Central China, Physics and Chemistry of the Earth, 2001,26:655-672
Li, S., Liou,D., Chen,Y, The Sm-Nd isotopic age of coesite-bearing eclogite from the southern Dabie Mountains, Chinese Science Bulletin, 1992,37(190):1638-1641
Li, S., Chen,Y, Cong,B., Collision of the North China and Yangtze Blocks and formation of ecoesite-bearing eclogites: timeing and processes, Chemical Geology, 1993,109:70-89
Liou,Y., Lo,C., Tsai,C., Chung, S., Qiu, J., Li,X., ~(40)Ar/~(39)Ar geochronology of volcanic and intrusive rocks in the Dabie and Sulu terranes, eastern China, and their tectonic implications,Journal of the Geological Society of China, 1999,42(4):493-520
Maruyama,S., Liou, J.G., Zhang,R., Tectonic evolution of the ultrhigh-pressure (UHP) and high-pressure (HP) metamophic belts from central China, The Island Arc, 1994, (3): 112-121
Matsuhisa, Y., Goldsmith,J.R.,Clayton, R.N.,Oxygen isotopic fractionation in the system quartz-albite-anorthite-water, Geochimica et Cosmochimica Acta, 1979, 43(7): 1131-1140
Minear, J.W., Toksoz, M.N., Thermal regime of a downgoing and new global tectonics, Journal of Geophysical Research, 1970, 1397-1419
P. Philippot, P. Chevallier, C. Chopin, J. Duhessy, fluid comosition and evolution in coesite-bearing rocks Dora Maira massif, Western Alps: implications for element rechycling during subduction, Contributions to Mineralogy Petrology, 1995,121:29-44
Rahn,M.K., Grasemann,B., Fission track and numerical thermal modeling of differential exhumation of the Glarus thrust plane (Switzerland), Earth and Planetary Science Letters, 1999, 169:245-259
Ratschbacher, L., Hacker, B. R., Webb,L. E., Dong,S., exhumation of the ultrahigh-pressure continental crustin East-Central China: Cretaceous and Cenozoic unroofing and the Tan-Lu fault, Journal of
Geophysical Research, 2000, 105 (B6): 13321-13338
Raza.,A., Mesozoic thermo-tectonic evolution of central eastern Australia and the Waltemata Basin, North Island, New Zealand: A fission track study, International Geology Review, 1997, 39: 107-124
Reiners, P.W., Farley, K.A., Helium diffusion and (U-Th)/He thermochronometry of titanite: Geochimica et Cosmochimica Acta, 1999, 63: 3845-3859
Reiners, P.W., Ehlers, T.A, Garver, J. I., Late Miocene exhumation and uplift of the Washington Cascade Range, Geology(Boulder),2002, 30 (9): 767-770
Roedder, E., Liquid CO_2 inclusion in olivine bearing and phenocrysts from basalts, America Mineral. 1965, 50:1746-1786
Roedder, E., Fluid inclusions. Res.Mineralogy, 1984.12:337-359
Roselle, G. T., Engi,M., Ultra high pressure (UHP) terrains; lessons from thermal modeling,American Journal of Science, 2002,302(5):410-441
Sack, P.E., Secor Jr, S.T., Delamination in collisional orogens, Geology, 1990, 18:999-1002
Santosh,M., Nature and evolution of metamorphic fluid in the precambrian khondalites of Kerala, South India, Precambrian Research, 1986,33:283-302
Sterner, S.M., Bodnar, R.J., Synthetic fluid inclusions: Re-equilibration of fluid inclusions in quartz during laboratory-simulated metamorphic burial and uplift, Journal Metamorphic Geology, 1989,7:243-260
Suo,S., Zhong,Z, You,Z., Extensional deformation of post ultrahigh-pressure metamorphism and exhumation process of ultrahigh-pressure metamorphic rocks in the Dabie Massif, China, Science in China. Series D, 2000,43(3):225-236
Tagami,T., Nishimura S., Determination of zeta calibration constant for fisson track dating, Nuclear Tracks Radiation Measurement, 1987, 13:127～130
Tsai, C.H., Lo,C.H., Liou, J.G., Jahn, B., Evidence against subduction-related magmatism for the Jiaoziyan Gabbro, northern Dabie Shan, China, Geology (Boulder), 2000,28(10):943-946
Turner, S., Sandiford,M., Foden, J., Some geodynamic and compositional constraints on 'postorogenic' magmatism, Geoloy, 1992,931-934
Wagner, G.A., Haute. P. V., Fission-track dating, The Netherlands. Ferdinand Enke Verlag Stuttgart, Dordrecht, 1992, 285
Wang, X., Liou,G., Mao,H.K. Coesite-bearing eclogite from the Dabie Mountains in central China,Geology, 1989,17:1085-1088
Warnock,A.C., Zeitler, P.K., Wolf, R.A., S Bergman,.C., An evaluation of low-temperature apatite U-Th/He thermochronometry: Geochimica et Cosmochimica Acta, 1997, 61: 5371-5377
Wessel,P., Global distribution of seamounts inferred from gridded Geosat/ERS-1 altimetry, J. Geophys. Res. 2001. 106(B9): 19,431-19,442
Whitehead,Jr.,J.A., Dick, H.J.B., Schouten, H., A mechanism for magmatic accretion under spreading centers, Nature, 1984,312:146-147
Wickham, S.M., Oxburgh, E.R., Continental rifts as a setting for regional metamorphism, Nature, 1985, 318:330-333
Xiao,Y., Hoefs,J., van den Kerkhof, A. M., Fiebig, J., Zheng, Y., Fluid history of UHP metamorphism in Dabie Shall, China:a fluid inclusion and oxygen isotope study,2000
Xu,S., Okay, A, I, Ji, S. et al, Diamond from metamorphic rocks and its implication for tetonic setting, Science, 1992,256:80-82
Zhang,R.Y., Liou,J.G., Cong,B.L., Talc-,magnesite-and Ti-clinohumite-bearing ultrahigh-pressure
meta - mafic and ultramafic complex in the Dabie Mountains, China, Journal of Petrology, 1995,36:1011-1037
Zheng,Y. F., Fu, B., Cong,B., Extreme ~(18)O depletion in eclogite from the Su-Lu terane in east China, Europen Journal of Mineral, 1996,317-323
安徽省地质局，中华人民共和国区域地质调查报告，六安、岳西幅(1：20万)，1974；
安徽省地质矿产局，安徽省区域地质志，地质出版社，1987，北京
陈道公，Etienne Deloule，夏群科，程昊，北大别片麻岩中锆石U-Pb年龄离子探针初步测定，岩石学报 2000，(2)
陈道公，李彬贤，夏群科，吴元保，程昊，大别超高压碰撞造山带岩石锆石U-Pb同位素框架年代学，矿物岩石地球化学通报，2001，20(4)：253-255
从柏林，王清晨，大别山-苏鲁超高压变质带研究的最新进展，科学通报，1999，44(11)：1127-1132
杜建国，顾连兴，孙先如，岳书仓，大别山带的流体系统与成矿作用，地质学报，2001，75(4)：507-517
杜建国，徐晓春，孙先如，戴圣潜，大别造山带核部罗田陈林沟金矿成矿时代，贵金属地质，2000，9(2)：91-96
杜建国，张鹏，大别造山带北部的中生代火山岩，现代地质，1999，13(1)：57-65
方中，徐士进，王汝成，大别山超高压变质带花岗岩两期变质作用和造山带抬升的年代学证据，矿物岩石地球化学通报，2001，20(2)：256-258．
傅斌，肖益林，J. L. R. Touret, A. M. Van den Kerkhof, J. Hoefs，郑永飞，大别山双河和碧溪岭超高压变质岩流体包裹体研究，岩石学报，2000，16(1)：119-126
郭锋，吴有林，范蔚茗，林舸，湖南省宁远——道县中生代玄武岩中辉长岩包体的岩石学初步研究，大地构造与成矿学，1996，1：38-45
郭震宇，董火根，郭令智，大别造山带变质岩地层年龄及其构造意义，地层学杂志，1998，22(3)：185-195
郭正府，邓晋福，许志琴，莫宣学，罗照华，青藏东昆仑晚古生代末—中生代中酸性火成岩与陆内造山过程，现代地质，1998，12(3)：344-352
韩喜球，马维林，金翔龙，杨树锋，冲绳海槽南部玄武岩中的流体包裹体成分及其意义，海洋与湖沼，2002，(01): 42-46
韩郁菁，张泽明，高压超高压变质作用中的流体，地学前缘，1996，3(3-4)：222-229
郝杰，刘小汉，桐柏大别碰撞造山带大型推覆—滑脱构造及其演化，地质科学，1988，(1)：1-10
季克俭，王立本，热液源研究的重要进展和“三源”交待成矿学说，地学前缘，1994，1(4)：126～131
简平，杨巍然，造山带构造年代学基本问题——论同位素体系与变质作用的关系，地球科学进展，1998，13(5)：452-456
江万，莫宣学，赵崇贺，郭铁鹰，张双全，矿物裂变径迹年龄与青藏高原隆升速率研究，地质力学学报，1998，4(1)：13-18
金成伟，郑祥身，大别岳西地区花岗岩类岩石学及其成因，岩石学报，1998，14(4)：493-502
李曙光，黄方，李晖，大别-苏鲁造山带碰撞后的岩石圈拆离，科学通报，2001，46(17)：1487-1491
李曙光，肖益林，刘德良，大别山石马地区石榴黑云片麻岩的Sm-Nd、K-Ar年龄及冷却速率，地质科学1995，30(2)：174-182
李一良，郑永飞，傅斌，大别山榴辉岩中石英脉的氧同位素研究，中国科学(D辑)，2001，31(4)：305-314
李勇，孙爱珍，龙门山造山带构造地层学研究，地层学杂志，2000，03：201-206
李忠，李任伟，孙枢，张雯华，大别地块北缘侏罗系花岗岩类砾石的Rb-Sr年代学特征，科学通报 2001(7)
刘斌，沈昆，流体包裹体热力学，地质出版社，1999，北京
刘凤山，石准立，太行山—燕山地区中生代花岗岩生成动力学机制与陆内造山作用，地球学报1998，19(1)：13-18
刘和甫，盆山耦合类型，地学前缘2000，7(4)：469-475
刘景波，叶凯，从柏林，范宏瑞，大别山超高压变质带片麻岩锆石中重晶石和硬石膏包裹体及其意义，岩石学报，2000，16(4)：482-484
刘文灿，王果胜，北淮阳地区中生代逆冲推覆构造，现代地质，1998，13(2)：143-149
卢焕章，李秉伦，沈昆等，包裹体地球化学，地质出版社，1990，北京
路玉林，钱存超，周存亭，安徽岳西脉状英安质角砾熔岩的发现、特征及意义，安徽地质，1996，6(4)：41-46
毛建仁，陶奎元，杨祝良，朱云鹤，薛怀民，Geodynamic Background of the Mesozoic Intracontinental Magmatism in Southeast China, Chinese Journal of Geochemistry 1997, 16(3):230-239
潘国强,钱存超 贾十军，安徽大别山腹地中生代火山岩的发现及其地质意义，安徽地质，1998，8(1)：27-31
桑隆康，王人镜，张泽明等，九资河-天堂寨地区燕山晚期花岗岩与大别山带核部隆升，地质学报，2000，74(3)：234-246
索书田，钟增球，游振东，大别地块超高压变质期后伸展变形及超高压变质岩石折返过程，中国科学(D辑)，2000，30(1)：9-17
陶士振，卫延召，刘德良，杨晓勇，造山带超高压变质流体中气体组成及成藏条件初探，地质科学，2001，36(1)：91-100
王成善，丁学林，喜马拉雅的隆升及其沉积反应研究新进展，地质科技情报，1998，17(1)：1-7(3)：338-344
王椿镛，张先康，陈步云，大别造山带的地壳结构研究，中国科学(D辑)，1997，27(3)：221-226
王光杰，滕吉文，张中杰，中国华南大陆及陆缘地带的大地构造基本格局，地球物理学进展，2000，15(03)：25-44
王国灿，杨巍然，大别造山带中新生代隆升作用的时空格局—构造年代学证据，地球科学，1998，23(5)：461-466
王强，邱家骧，王人镜，大别造山带核部典型燕山期花岗岩岩浆演化的p-T轨迹，矿物岩石，1999，19(4)：15-20
王强，赵振华，熊小林，桐柏—大别造山带燕山晚期A型花岗岩的厘定，岩石矿物学杂志，2000，19(4)：297-315
王清晨，从柏林，大别山超高压变质带的大地构造框架，岩石学报，1998，14(4)：481-492
王人镜，王强，何勇，大别山造山带核部九资河—天堂寨花岗岩的成因和时代，矿物岩石地球化学通报，1998，17(4)：224-228
王岳军，北淮阳晚中生代火山岩定年及火山砾石地球化学：对大别灰色片麻岩隆升和中生代地层格架的约束，科学通报，2002，47(20)：1528-1534
魏春景，单振刚，张立飞等，北大别榴辉岩的确定及其地质意义，科学通报，1996，42(17)：1832-1835
魏春景，张立飞，王式洗，安徽省大别山东段中生代高钾花岗质岩石及其地质意义，中国科学(D辑)，2000，30(4)：355-363
吴堑虹，刘厚昌，(U-Th)/He定年—低温热年代学研究的一种新技术，地球科学进展，2002，(1)：126-131
吴珍汉，崔盛芹，吴淦国等，燕山山脉隆升过程的热年代学分析，地质论评，2000，(1)：49-57
夏新宇，王先彬，陈江峰，葛宁洁，大别山双河地区超高压变质岩流体包裹体成分及二氧化碳碳同位
素研究，中国科学D辑，1999，29(4)：314-320
徐启东，张本仁，单光祥，蒋敬业，马振东，大别造山带中生代花岗岩类成分的时空分布与造山带演化的关系，地球科学，1997，22(6)：595-598
徐启东，钟增球，索书田，齐先茂，桐柏——大别地区中温热液金矿床成矿流体性质与沉淀机理，矿床地质，1995，1：59-72
徐树桐，江来利，刘贻灿等．大别山区(安徽部分)的构造格局和演化过程．地质学报，1992，66(1)：1～13
徐树桐，刘贻灿，吴维平，江来利，大别山造山带研究的主要进展及存在问题，自然科学进展796-803
杨坤光，马昌前，许长海，杨巍然，北淮阳构造带与大别造山带的差异性隆升，中国科学，1999，29(2)：97-103
杨坤光，马昌前，杨巍然，北淮阳马畈加里东岩体的研究及其地质意义，地球科学，1998，23，(3)：236-241
杨巍然，王国灿，简平，大别造山带构造年代学，中国地质大学出版社，2000，武汉
杨文采，余长青，根据地球物理资料分析大别—苏鲁超高压变质带演化的运动学与动力学，地球物理学报，2001，44(3)：346-359
杨晓勇，郑永飞，刘德良，陶士振，中国东部橄榄岩包体和榴辉岩中CO_2流体包裹体的碳同位素组成，岩石学报，2000，16(4)：473-481
杨志华，苏生瑞，李勇，张传林，周美夫，赵太平，中国大地构造几个重大问题的探讨，地学前缘，2001，8(2)：395-406
杨志华，苏生瑞，李勇，张传林，周美夫，赵太平，中国大地构造几个重大问题的探讨，地学前缘2001，(2)
张鸿翔，徐志方，黄智龙，刘从强，地幔流体基本特征及成因，地质地球化学，2000，28(2)：1-7
张泽明，韦必则，韩郁菁，游振东，鄂北高压榴辉岩相变质带的变质、变形和流体演化，岩石学报1999，15(1)：48-56
郑度，林振耀，张雪芹，青藏高原与全球环境变化研究进展，地学前缘，2002，9(1)：95-102
郑建平，路凤香，华北地台深部地幔流体的组成——来自金刚石不纯净组分的报道，地质科学，1998，33(1)：52-60
郑永飞，魏春生，王峥嵘等，大龙山岩体冷却史及其成矿关系的同位素研究，地质科学，1997，32(4)：465-477
郑永飞，陈江峰，稳定同位素地球化学，科学出版社，2000，北京
郑永飞，傅斌，李一良，肖益林，龚冰，大别山超高压变质作用期前和期后水岩相互作用的氢氧同位素证据，1999，29(2)：113-121
周泰禧，陈江峰，张巽，等，北淮阳花岗岩—正长岩带地质地球化学特征及其大地构造意义，地质论评，1995，2：144-151