Is the Qinling Orogen an Indosinian Collisional Orogenic Belt?
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摘要: 国内外一些学者认为秦岭是一个印支碰撞造山带.但迄今为止,秦岭尚未发现三叠纪或古生代延续到三叠纪的洋盆存在的任何痕迹.秦岭泥盆系-三叠系为滨、浅海相沉积,没有远洋沉积,更没有镁铁质和超镁铁质岩石及与之密切相关的放射虫硅质岩组成的蛇绿岩套.泥盆系与下伏地质体之间有一个清楚的区域性角度不整合.商丹断裂并不是印支期,而是加里东期的板块缝合带;其两侧,中朝板块南缘和扬子板块北缘均有十分清楚的加里东造山作用的记录.沉积于扬子板块北缘的中上泥盆统刘岭群的放射性铅同位素组成与北秦岭相近,碎屑锆石年龄谱系亦证明其物质主要来自中朝板块南缘的北秦岭造山带.所谓勉略印支缝合带中的勉略和三里岗蛇绿混杂岩中的镁铁质岩,同位素测年均为元古代之产物,后者又被南华系-震旦系沉积覆盖.所谓勉略缝合带,实为一区域性大断裂带.早古生代,其北侧属扬子板块北部被动边缘;南侧为扬子板块核心部分的扬子准地台(小克拉通).所以,秦岭的印支造山作用,并不是洋盆消失后的陆陆碰撞造山作用,而是海盆消失后的中朝与扬子2个小陆块间逆冲-叠覆造山作用.作为秦岭东延的大别山超高压变质带被认为是秦岭印支碰撞造山的重要证据之一,但大别山超高压变质岩是在造山作用过程中动态超高压条件下形成的,仅用简单的静岩压力来计算其形成深度,显然是不符合实际情况的.野外地质观察、构造地质学、变质岩石学、同位素地质学、地球化学、地球物理学以及物理实验等方面的实际资料和研究结果均说明超高压变质作用并不是在上地幔而是在地壳内进行的.南秦岭-大别山的地壳构造层次,上地壳自上而下依次为:未变质的沉积岩层、绿帘-蓝片岩层、高压变质岩层、超高压变质岩层;下地壳为未卷入超高压变质作用的麻粒岩相-高角闪岩相变质杂岩.含柯石英的超高压单位只是位于上地壳下部的厚约10~12 km的席状构造岩片.初步认为上地壳这一从低压到高压再到超高压的构造系统,是印支造山期间,南秦岭-大别山的上地壳以下地壳顶部为主剪切滑动面,多层次剪切作用造成的.上地壳下部的超高压变质岩,则可能是强烈剪切引起的频繁地震的震源区瞬时超高压作用的结果.Abstract: Since the late 1980s, the Qinling orogen has been considered an Indosinian collisional orogenic belt by some Chinese and foreign geologists. However, no trace of a Triassic oceanic basin or a Paleozoic oceanic basin that continued to Triassic has been found as yet in the Qinling area. It has been suggested that the Devonian-Triassic of the Qinling area is characterized by coastal to shallow marine sediments, and there are no pelagic sediments or ophiolites. There is a clear regional angular unconformity between the Devonian and its underlying rocks. The Shangdan fault is not an Indosinian but a Caledonian suture zone, both sides of which (i.e. the southern margin of the Sino-Korean plate and the northern margin of the Yangtze plate) have a clear record of the Caledonian orogeny. The Pb isotopic compositions of the Liuling Group of the Middle-Upper Devonian, deposited on the northern margin of the Yangtze plate, are similar to those of the North Qinling belt. The detrital zircon age spectrum also suggests that the sediments came from the North Qinling orogenic belt. Mafic rocks from the Mianlue and Sanligang ophiolitic melanges within the Mianlue Indosinian suture zone show a Proterozoic age, and the Sanligang ophiolitic melange is overlain by the sediments of the Nanhuan-Sinian. The so-called Mianlue suture zone is actually a huge regional fracture zone, to the north of which was the passive margin of the Yangtze plate in Early Paleozoic and to the south lay the Yangtze paraplatform (small craton), the core of the Yangtze plate. Therefore, the Indosinian orogen of the Qinling should be attributed to the thrusting and overlapping of the continental crust rather than the continent-continent collision after the disappearance of the oceanic basin. The ultrahigh pressure (UHP) metamorphic belt of the Dabieshan, the eastern extension of the Qinling orogen, is considered an important piece of evidence suggesting that the Qinling was an Indosinian collisional orogen. However, the Dabieshan UHP metamorphic rocks were formed under dynamic UHP conditions during the orogenic process. Therefore, it is inappropriate to convert the estimated thermodynamic pressure to depth by assuming that the pressure was static simply due to burial. Accumulating data from field geological observations, structural geology, metamorphic petrology, isotope geology, geochemistry, geophysics, and physical experiments all indicate that the UHP metamorphism did not occur in the upper mantle but in the earth crust. Structurally, the upper crust of the South Qinling-Dabie region can be subdivided, from top to bottom, into four layers:unmetamorphosed sedimentary rocks, epidote-glaucophane schists, high pressure metamorphic rocks, and UHP metamorphic rocks. The lower crust is represented by the upper amphibolite-granulite facies rocks which were not affected by the UHP metamorphism. The coesite-bearing metamorphic rocks are merely sheeted slices of about 10-12 km thick in the lower part of the upper crust. Based on these observations, our preliminary conclusion is that the low-high-ultrahigh pressure tectonic system of the upper crust in the South Qinling-Dabie region was the result of multilayered decollement above the lower crust, acting as a main shear slide plane during the Indosinian orogeny. The UHP metamorphic rocks of the lower part of the upper crust were formed in response to repeated transient UHP events in the focal area, where frequent earthquakes were likely caused by severe shearing.
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图 1 旬阳县潘家西北下泥盆统(D1)砾岩、砂岩不整合于下志留统(S1)泥质粉砂岩之上
据江小均等(2019)修改
Fig. 1. The Lower Devonian (D1) conglomerate and sandstone unconformably overlie the Lower Silurian (S1) muddy siltstone in northwest Panjia area of Xunyang County
图 2 秦岭造山带206Pb/204Pb-207Pb/204Pb和206Pb/204Pb-208Pb/204Pb图
据路凤香等(2006)修改
Fig. 2. Plots of 206Pb/204Pb versus 207Pb/204Pb and 206Pb/204Pb versus 208Pb/204Pb of Qinling orogen showing that the provenance of Liuling Group is from North Qinling
图 3 大别-苏鲁地区榴辉岩的氦同位素分布图
据Li et al., (2000);李善芳等(2005)修改
Fig. 3. Helium isotope compositions of eclogites from Dabie-Sulu region
图 4 大别山构造层次简图
据《大别山超高压变质作用与碰撞造山动力学》编写组(2005)修改.GMF.龟梅断裂;MXF.磨子潭-晓天断裂;XGF.襄樊-广济断裂;TLF.郯庐断裂;QOB.秦岭造山带;SL.苏鲁带;SKP.中朝板块;NHY.北淮阳构造带;CMC.核部变质杂岩;UHP.超高压变质岩层;HP.高压变质岩层;EB.绿帘-蓝片岩层;US.未变质的沉积岩层
Fig. 4. Simplified tectonic level map of Dabieshan
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Chopin, C., 1984.Coesite and Pure Pyrope in High-Grade Blueschists of the Western Alps:A First Record and Some Consequences.Contributions to Mineralogy and Petrology, 86(2):107-118. https://doi.org/10.1007/bf00381838 Chopin, C., 1987.Very-High-Pressure Metamorphism in the Western Alps:Implications for Subduction of Continental Crust.Philosophical Transactions of the Royal Society of London, 321(1557):183-197. http://doi.org/10.1098/rsta.1987.0010 Cong, B.L., 1996.Ultrahigh-Pressure Metamorphic Rocks in the Dabieshan-Sulu Region of China.Science Press and Kluwet Acd.Publ., Beijing and Dordrecht. Ding, T.P., 2000.Isotopic Constraints on the Formation Depth of Ultrahigh Pressure Metamorphic Rocks in the Dabie Region.Journal of Geomechanics, 6(3):39-44(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLX200003003.htm Dong, Y.P., Liu, X.M., Neubauer, F., et al., 2013.Timing of Paleozoic Amalgamation between the North China and South China Blocks:Evidence from Detrital Zircon U-Pb Ages.Tectonophysics, 586:173-191. https://doi.org/10.1016/j.tecto.2012.11.018 Dong, Y.P., Zhang, G.W., Liu, X.M., et al., 1998.Disintegration of the Huashan Group in the Dahong Mountain Area, Northern Hubei.Regional Geology of China, 17(4):371-376, 397(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD804.005.htm Editing Board of Ultrahigh-Pressure Metamorphism and Collisional Dynamics of the Dabie Mountains, 2005.Ultrahigh-Pressure Metamorphism and Collisional Dynamics of the Dabie Mountains.Science Press, Beijing (in Chinese). Feng, Y.M., Cao, X.D., Zhang, E.P., 2004.Discussion on the Tectonic Features of the Mianxian-Lueyang Zone.Geological Review, 50(3):295-303(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000005405 Ge, X.H., Ma, W.P., 2014.A Course in Regional Tectonics of China.Geological Publishing House, Beijing (in Chinese). Hsü, K.J., Wang, Q.C., Li, J.L., et al., 1987.Tectonic Evolution of Qinling Mountains, China.Eclogae Geol.Helv., 80:735-752. http://d.old.wanfangdata.com.cn/Periodical/dzlp201801011 Hu, Z.X., Mao, X.W., Tian, W.X., et al., 2015.Discovery of the Jinningian Orogenic Belt on the Northern Margin of Yangtze Craton in Mountain Dahong.Geological Survey of China, 2(2):33-39(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZDC201502006.htm Huang, J.Q., Ren, J.S., Jiang, C.F., et al., 1974.Some New Observations on the Geotectonic Characteristics of China.Acta Geologica Sinica, 48(1):38-54(in Chinese with English abstract). Huang, J.Q., Ren, J.S., Jiang, C.F., et al., 1977.An Outline of the Tectonic Characteristics of China.Acta Geologica Sinica, 51(2):117-135(in Chinese with English abstract). Huang, J.Q., Xiao, X.C., Ren, J.S., et al., 1965.Fundamental Characteristics of the Geotectonics of China-An Explanatory Note to the 1:3 000 000 Scale Geotectonic Map of China.China Industry Press, Beijing (in Chinese). Jiang, C.F., Zhang, Q.G., Zhang, Y.X., et al., 1963.The Presence of the Indosinian Movement in Eastern Qinling Geosyncline.Geological Review, 9(3):116-121(in Chinese). Jiang, C.F., Zhu, Z.Z., Kong, F.Z., 1979.On the Liufengguan Flysch.Acta Geologica Sinica, 53(3):203-218(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dzxe197903003.htm Jiang, X.J., 2013.The Study of Sedimentary Characteristics and Tectonic Setting in Eastern Qinling Orogenic Belt (Dissertation).Chinese Academy of Geological Sciences, Beijing (in Chinese with English abstract). Jiang, X.J., Ren, J.S., Zhou, D.W., et al., 2019.The Caledonian Tectonic-Sedimentary Evolution Process in Eastern Qinling Orogenic Belt.Earth Science, 44(1):88-108(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201901007.htm Li, H.L., Song, C.Z., Han, J.J., et al., 2018.The Comparison about the Shear Zones in the Northern and the Southern Boundary of the Tongbai Complex and Constraints on the Tectonic Framework of the Tongbai Orogenic Belt.Acta Petrologica Sinica, 34(3):813-836(in Chinese with English abstract). Li, S.F., Li, Y.H., Ding, T.P., et al., 2005.Helium Isotope Compositions and Forming Conditions of UHP Metamorphic Eclogites from the Dabie Mts.Terrane in East China.Geological Review, 51(3):243-249(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000005173 Li, Y.H., Li, J.C., Song, H.B., 2000.Helium Isotope Geochemistry of Ultrahigh-Pressure Metamorphic Eclogites from the Dabie Mts.and Sulu Terrane in East China.Acta Geologica Sinica (English Edition), 74(1):14-18. http://www.cnki.com.cn/Article/CJFDTotal-DZXW200001002.htm Li, Y.H., Li, J.C., Song, H.B., et al., 1997.He Isotope of Eclogite from the Dabie and Su-Lu Region and Its Implication.Acta Geoscientia Sinica, 18(Suppl.):77-79(in Chinese with English abstract). Liu, F.L., Xu, Z.Q., Liou, J.G., et al., 2007.Ultrahigh-Pressure Mineral Assemblages in Zircons from the Surface to 5 158 m Depth in Cores of the Main Drill Hole, Chinese Continental Scientific Drilling Project, Southwestern Sulu Belt, China.International Geology Review, 49(5):454-478. https://doi.org/10.2747/0020-6814.49.5.454 Lu, F.X., Zhang, B.R., Han, Y.W., et al., 2006.The Three-Dimensional Lithospheric Chemical Structure of Qinling-Dabie-Sulu Area.Geological Publishing House, Beijing (in Chinese). Lü, G.X., Chen, J., Li, X.B., et al., 1998.The Formation Depth of Coesite Bearing Eclogite, Dabie UHPM Zone, China, Modified by Tectonooriginal Additional Hydrostatic Pressure.Chinese Science Bulletin, 43(24):2590-2602(in Chinese). Lü, G.X., Wang, F.Z., Liu, R.X., 2004.Additional Tectonic Pressure and Formation Depths of UHP Metamorphic Rocks.Science Press, Beijing (in Chinese). Okay, A.I., Xu, S.T., Sengör, A.M.C., 1989.Coesite from the Dabie Shan Eclogites, Central China.European Journal of Mineralogy, 1(4):595-598. https://doi.org/10.1127/ejm/1/4/0595 Ren, J.S., 1994.The Continental Tectonics of China.Acta Geoscientia Sinica, (3-4):5-13(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dzlp201802001 Ren, J.S., 2013.International Geological Map of Asia (1:5 000 000).Geological Publishing House, Beijing (in Chinese). Ren, J.S., Chen, T.Y., Niu, B.G., et al., 1990.Tectonic Evolution of the Continental Lithosphere in Eastern China and Adjacent Areas.Science Press, Beijing (in Chinese). Ren, J.S., Jiang, C.F., Zhang, Z.K., et al., 1980.Geotectonic Evolution of China.Science Press, Beijing (in Chinese). Ren, J.S., Wang, Z.X., Chen, B.W., et al., 1999.The Tectonics of China from a Global View-A Guide to the Tectonic Map of China and Adjacent Regions (1:5 000 000).Geological Publishing House, Beijing (in Chinese). Ren, J.S., Zhang, Z.K., Niu, B.G., et al., 1991.On the Qinling Orogenic Belt-Integration of the Sino-Korean and Yangtze Blocks.Northwest University Press, Xi'an, 99-110(in Chinese). Section of Structural Geology, Institute of Geology, Chinese Academy of Geological Sciences, 1979.Tectonic Map of China, Scale 1:4 000 000.Cartographic Publishing House, Beijing (in Chinese). Şengör, A.M.C., 1985.Geology:East Asian Tectonic Collage.Nature, 318(6041):16-17. https://doi.org/10.1038/318016a0 Shi, Y.R., Liu, D.Y., Zhang, Z.Q., et al., 2007.SHRIMP Zircon U-Pb Dating of Gabbro and Granite from the Huashan Ophiolite, Qinling Orogenic Belt, China:Neoproterozoic Suture on the Northern Margin of the Yangtze Craton.Acta Geologica Sinica (English Edition), 81(2):239-243. https://doi.org/10.1111/j.1755-6724.2007.tb00947.x Smith, D.C., 1984.Coesite in Clinopyroxene in the Caledonides and Its Implications for Geodynamics.Nature, 310(5979):641-644. https://doi.org/10.1038/310641a0 Su, W.H., 2011.The Formation Mechanism of Coesite Far from Equilibrium Phase-Boundary and the Physical Foundation of Hypothesis of Plate Subduction-Exhumation in the Earth.Geological Review, 57(4):457-472(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000003884 Su, W.H., Liu, S.E., Xu, D.P., et al., 2006.Effects of Local Mechanical Collision with Shear Stress on the Phase Transformation from α-Quartz to Coesite Induced by High Static Pressure.Physical Review B, 73(14):144110. https://doi.org/10.1103/physrevb.73.144110 Su, W.H., Liu, X.M., Xu, D.P., et al., 2009.On the Minimum Static Pressure for the Formation of Coesite and a New Mechanism of Coesite Formation near the Surface and Geological Implication.Progress in Natural Science, 159(7):730-745(in Chinese). Tian, H., Li, H.K., Zhou, H.Y., et al., 2017.Depositional Age of the Huashan Group on the Northern Margin of the Yangtze Plate and Its Constraints on Breakup of the Rodinia Supercontinent.Acta Geologica Sinica, 91(11):2387-2408(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZXE201711002.htm Wang, H.Z., 1985.Atlas of the Palaeogeography of China.Cartographic Publishing House, Beijing (in Chinese). Wang, Q.C., Sun, S., Li, J.L., et al., 1989.The Tectonic Evolution of the Qinling Mountain Belt.Scientia Geologica Sinica, (2):129-142(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/gxdzxb201802008 Wang, X.M., Liou, J.G., Mao, H.K., 1989.Coesite-Bearing Eclogite from the Dabie Mountains in Central China.Geology, 17(12):1085.https://doi.org/10.1130/0091-7613(1989)017<1085:cbeftd>2.3.co;2 doi: 10.1130/0091-7613(1989)017<1085:cbeftd>2.3.co;2 Xu, Z., 1987.Etude Tectonique et Microtectonique de la Chaine Paleozoique et Triasique des Quilings (Chine).Universite des Sciences et Techniques du Languedoc, France, 96-98. Xu, Z.Q., 2007.Continental Deep Subduction and Exhumation Dynamics:Evidence from the Main Hole of the Chinese Continental Scientific Drilling and the Sulu HP-UHP Metamorphic Terrane.Acta Petrologica Sinica, 23(12):3041-3053(in Chinese with English abstract). Yan, Q.R., Wang, Z.Q., Yan, Z., et al., 2007.SHRIMP Analyses for Ophiolitic-Mafic Blocks in the Kangxian-Mianxian Section of the Mianxian-Lueyang Mélange:Their Geological Implications.Geological Review, 53(6):755-764(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000004823 Yang, J., Smith, D.C., 1989.Evidence for a Former Sanidine-Coesite-Eclogite at Lanshantou, East China, and the Recognition of the Chinese"Su-Lu Coesite-Eclogite Province".In: Third International Eclogite Conference.Blackwell Scientific Publications, Oxford, 26. Yang, J.J., Fan, Z.F., Yu, C., et al., 2014a.Coseismic Formation of Eclogite Facies Cataclasite Dykes at Yangkou in the Chinese Su-Lu UHP Metamorphic Belt.Journal of Metamorphic Geology, 32(9):937-960. https://doi.org/10.1111/jmg.12101 Yang, J.J., Huang, M.X., Wu, Q.Y., et al., 2014b.Coesite-Bearing Eclogite Breccia:Implication for Coseismic Ultrahigh-Pressure Metamorphism and the Rate of the Process.Contributions to Mineralogy and Petrology, 167(6):1013-1030. https://doi.org/10.1007/s00410-014-1013-7 Yang, Y.Z., Li, H.P., 1991.Sedimentary Characteristics and Geological Significance of the Devonian System in Southeastern Shanyang, Shaanxi Province.Northwestern Geology, 12(1):5-10(in Chinese). Yui, T.F., Rumble Ⅲ, D., Lo, C.H., 1995.Unusually Low δ18O Ultra-High-Pressure Metamorphic Rocks from the Sulu Terrain, Eastern China.Geochimica et Cosmochimica Acta, 59(13):2859-2864. https://doi.org/10.1016/0016-7037(95)00161-R Zhang, G.W., Dong, Y.P., Lai, S.C., et al., 2003.Mianlüe Tectonic Zone and Mianlüe Suture Zone on Southern Margin of Qinling-Dabie Orogenic Belt.Science in China (Series D:Earth Sciences), 33(12):1121-1135(in Chinese). Zhang, G.W., Meng, Q.R., Lai, S.C., 1995.Tectonics and Structure of the Qinling Orogenic Belt.Science in China (Series B:Chemistry), 25(9):994-1003(in Chinese). http://d.old.wanfangdata.com.cn/Periodical/OA000002705 Zhang, G.W., Meng, Q.R., Yu, Z.P., et al., 1996.Orogenesis and Dynamics of Qinling Orogen.Science in China (Series D:Earth Sciences), 26(3):193-200(in Chinese). http://www.cnki.com.cn/Article/CJFDTotal-JDXG199603000.htm Zhang, H.J., Ye, Q., Mao, X.W., et al., 2013.Sedimentary Characteristics and Tectonic-Paleogeography Significance of Huashan Group in Qingbaikou Period of Dahong Mountain, Hubei.Resources Environment & Engineering, 27(6):737-740, 768(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-HBDK201306001.htm Zhang, R.Y., Hirajima, T., Banno, S., et al., 1989.Coesite-Eclogite from Donghai Area, Jiangsu Province in China.The 15th General Meeting of the International Mineralogical Association Abstracts, 2:923-924. Zhang, W.Y., 1986.Marine and Continental Geotectonics of China and Its Environs.Science Press, Beijing (in Chinese). Zheng, Y.F., Fu, B., Gong, B., et al., 1996.Extreme 18O Depletion in Eclogite from the Su-Lu Terrane in East China.European Journal of Mineralogy, 8(2):317-324. https://doi.org/10.1127/ejm/8/2/0317 丁悌平, 2000.大别山超高压变质岩形成深度的同位素限制.地质力学学报, 6(3):39-44. doi: 10.3969/j.issn.1006-6616.2000.03.004 董云鹏, 张国伟, 柳小明, 等, 1998.鄂北大洪山地区"花山群"的解体.中国区域地质, 17(4):371-376, 397. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD804.005.htm 《大别山超高压变质作用与碰撞造山动力学》编写组, 2005.大别山超高压变质作用与碰撞造山动力学.北京:科学出版社. 冯益民, 曹宣铎, 张二朋, 2004.勉县-略阳带大地构造属性之探讨.地质论评, 50(3):295-303. doi: 10.3321/j.issn:0371-5736.2004.03.014 葛肖虹, 马文璞, 2014.中国区域大地构造学教程.北京:地质出版社. 胡正祥, 毛新武, 田望学, 等, 2015.扬子陆块北缘大洪山地区发现晋宁期造山带.中国地质调查, 2(2):33-39. http://d.old.wanfangdata.com.cn/Periodical/zgdzdc201502004 黄汲清, 任纪舜, 姜春发, 等, 1974.对中国大地构造若干特点的新认识.地质学报, 48(1):38-54. http://www.cnki.com.cn/Article/CJFD1979-DZXE197401003.htm 黄汲清, 任纪舜, 姜春发, 等, 1977.中国大地构造基本轮廓.地质学报, 51(2):117-135. http://www.cnki.com.cn/Article/CJFDTotal-DZXE197702002.htm 黄汲清, 肖序常, 任纪舜, 等, 1965.中国大地构造基本特征——三百万分之一中国大地构造图说明书.北京:中国工业出版社. 姜春发, 张庆贵, 张玉岫, 等, 1963.东秦岭地槽型印支运动的存在.地质论评, 9(3):116-121. doi: 10.3321/j.issn:0371-5736.1963.03.002 姜春发, 朱志直, 孔凡宗, 1979.留凤关复理石.地质学报, 53(3):203-218. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197903003.htm 江小均, 2013.东秦岭泥盆系沉积特征和构造背景研究(博士学位论文).北京: 中国地质科学院. 江小均, 任纪舜, 周鼎武, 等, 2019.东秦岭加里东期沉积-构造演化过程.地球科学, 44(1):88-108. http://earth-science.net/WebPage/Article.aspx?id=4107 李海龙, 宋传中, 韩建军, 等, 2018.桐柏杂岩南北边界剪切带的对比以及对桐柏造山带构造格局的制约.岩石学报, 34(3):813-836. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201803018 李善芳, 李延河, 丁悌平, 等, 2005.大别山超高压变质榴辉岩的氦同位素组成及对其形成环境的制约.地质论评, 51(3):243-249. doi: 10.3321/j.issn:0371-5736.2005.03.003 李延河, 李金城, 宋鹤彬, 等, 1997.大别-苏鲁地区榴辉岩的He同位素特征及其地质意义.地球学报, 18(增刊):77-79. http://d.old.wanfangdata.com.cn/Conference/200319 路凤香, 张本仁, 韩吟文, 等, 2006.秦岭-大别-苏鲁地区岩石圈三维化学结构特征.北京:地质出版社. 吕古贤, 陈晶, 李晓波, 等, 1998.构造附加静水压力研究与含柯石英榴辉岩成岩深度测算.科学通报, 43(24):2590-2602. doi: 10.3321/j.issn:0023-074X.1998.24.003 吕古贤, 王方正, 刘瑞珣, 2004.超高压变质的构造附加压力与形成深度.北京:科学出版社. 任纪舜, 1994.中国大陆的组成、结构、演化和动力学.地球学报, (3-4):5-13. 任纪舜, 2013.1:500万国际亚洲地质图.北京:地质出版社. 任纪舜, 陈廷愚, 牛宝贵, 等, 1990.中国东部及邻区大陆岩石圈的构造演化与成矿.北京:科学出版社. 任纪舜, 姜春发, 张正坤, 等, 1980.中国大地构造及其演化.北京:科学出版社. 任纪舜, 王作勋, 陈炳蔚, 等, 1999.从全球看中国大地构造——中国及邻区大地构造图简要说明.北京:地质出版社. 任纪舜, 张正坤, 牛宝贵, 等, 1991.论秦岭造山带——中朝与扬子陆块的拼合过程.西安:西北大学出版社, 99-110. 中国地质科学院地质研究所构造地质室, 1979.中国大地构造图(1:400万).北京:地图出版社. 苏文辉, 2011.远离平衡相边界的柯石英形成机制及板块折返假说的物理基础.地质论评, 57(4):457-472. http://d.old.wanfangdata.com.cn/Periodical/dzlp201104001 苏文辉, 刘曙娥, 许大鹏, 等, 2009.柯石英最小静态形成压力与地表柯石英形成新机制及其地学意义.自然科学进展, 159(7):730-745. doi: 10.3321/j.issn:1002-008X.2009.07.006 田辉, 李怀坤, 周红英, 等, 2017.扬子板块北缘花山群沉积时代及其对Rodinia超大陆裂解的制约.地质学报, 91(11):2387-2408. doi: 10.3969/j.issn.0001-5717.2017.11.002 王鸿祯, 1985.中国古地理图集.北京:地质出版社. 王清晨, 孙枢, 李继亮, 等, 1989.秦岭的大地构造演化.地质科学, (2):129-142. doi: 10.3321/j.issn:0563-5020.1989.02.002 许志琴, 2007.深俯冲和折返动力学:来自中国大陆科学钻探主孔及苏鲁超高压变质带的制约.岩石学报, 23(12):3041-3053. doi: 10.3969/j.issn.1000-0569.2007.12.001 闫全人, 王宗起, 闫臻, 等, 2007.秦岭勉略构造混杂带康县-勉县段蛇绿岩块-铁镁质岩块的SHRIMP年代及其意义.地质论评, 53(6):755-764. doi: 10.3321/j.issn:0371-5736.2007.06.009 杨应章, 李海平, 1991.陕西山阳东南一带泥盆系的沉积特征及地质意义.西北地质, 12(1):5-10. http://www.cnki.com.cn/Article/CJFDTOTAL-XBDI199101001.htm 张国伟, 董云鹏, 赖绍聪, 等, 2003.秦岭-大别造山带南缘勉略构造带与勉略缝合带.中国科学(D辑:地球科学), 33(12):1121-1135. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200312001 张国伟, 孟庆任, 赖绍聪, 1995.秦岭造山带的结构构造.中国科学(B辑:化学), 25(9):994-1003. http://cdmd.cnki.com.cn/Article/CDMD-82501-2007213446.htm 张国伟, 孟庆任, 于在平, 等, 1996.秦岭造山带的造山过程及其动力学特征.中国科学(D辑:地球科学), 26(3):193-200. http://cdmd.cnki.com.cn/Article/CDMD-10697-2004104020.htm 张汉金, 叶琴, 毛新武, 等, 2013.湖北省大洪山地区青白口纪花山群沉积特征及其构造古地理意义.资源环境与工程, 27(6):737-740, 768. http://d.old.wanfangdata.com.cn/Periodical/hbdk201306001 张文佑, 1986.中国及邻区海陆大地构造.北京:科学出版社.