• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    桐柏-大别碰撞造山带的基本组成与结构

    钟增球 索书田 张宏飞 周汉文

    钟增球, 索书田, 张宏飞, 周汉文, 2001. 桐柏-大别碰撞造山带的基本组成与结构. 地球科学, 26(6): 560-567.
    引用本文: 钟增球, 索书田, 张宏飞, 周汉文, 2001. 桐柏-大别碰撞造山带的基本组成与结构. 地球科学, 26(6): 560-567.
    ZHONG Zengqiu, SUO Shutian, ZHANG Hongfei, ZHOU Hanwen, 2001. MAJOR CONSTITUENTS AND TEXTURE OF THE TONGBAI-DABIE COLLISIONAL OROGENIC BELT. Earth Science, 26(6): 560-567.
    Citation: ZHONG Zengqiu, SUO Shutian, ZHANG Hongfei, ZHOU Hanwen, 2001. MAJOR CONSTITUENTS AND TEXTURE OF THE TONGBAI-DABIE COLLISIONAL OROGENIC BELT. Earth Science, 26(6): 560-567.

    桐柏-大别碰撞造山带的基本组成与结构

    基金项目: 

    国家重点基础研究发展规划项目 G1999075506

    国家自然科学基金项目 49794041

    国家自然科学基金项目 40073005

    详细信息
      作者简介:

      钟增球(1947-), 男, 教授, 1982年毕业于武汉地质学院研究生院, 获硕士学位, 现主要从事变质岩、变质构造及岩石圈流变学方面的教学和研究

    • 中图分类号: P313;P542+.2

    MAJOR CONSTITUENTS AND TEXTURE OF THE TONGBAI-DABIE COLLISIONAL OROGENIC BELT

    • 摘要: 桐柏-大别碰撞造山带的组成与结构, 主要是印支期碰撞及高压、超高压变质期后伸展构造和中新生代热-构造演化的结果.在组成上, 除了燕山期及其后的岩浆活动和盆地堆积产物以外, 主要包括核部杂岩单元、超高压单元、高压单元、绿帘-蓝片岩单元和沉积盖层单元等, 此外还有一些镁铁质和超镁铁质岩体残留或侵入其中.桐柏-大别碰撞造山带的整体结构样式类似于北美西部的变质核杂岩带, 即以总体具穹隆形态及多层拆离滑脱带的发育为特征, 构成了以罗田和桐柏山为核部的两个穹隆.超高压单元、高压单元和绿帘蓝片岩单元作为不同的岩片夹持于核部杂岩和沉积盖层之间, 其分布格局受碰撞期后伸展构造格架所制约.

       

    • 图  1  桐柏-大别山三叠纪碰撞期后构造简图

      1.边界断裂; 2.构造缝合带; 3.下伸展滑脱带; 4.中伸展滑脱带; 5.上伸展滑脱带; 6.顶伸展滑脱带.QHF.确山-合肥断裂; XFF.信阳-肥西断裂; JMF.军马河-马蹄湾断裂; GMF.龟山-梅山断裂; BMXF.八里畈-晓天-磨子潭断裂; XGF.襄樊-广济断裂; TLF.郯城-庐江断裂; CC.核部杂岩单元; UHP.超高压单元; HP.高压单元; EB.绿帘蓝片岩单元; SC.沉积盖层.

      图  2  湖北麻城木子店地区地质图

      1.黑云斜长片麻岩; 2.石榴夕线石片麻岩; 3.角闪石榴二辉岩; 4.斜长角闪岩; 5.磁铁石英岩; 6.中酸性麻粒岩; 7.剪切带; 8.面理化二长花岗岩; 9.面理; 10.线理

      图  3  超高压(UHP) 单元和核部杂岩(CC) 单元中片麻岩及面理化花岗岩的w (An)-w (Ab)-w (Or) 及w (K2O)-w (Na2O)-w (CaO) 图解

      Fig.  3.  Diagrams of w (An)-w (Ab)-w (Or) and w (K2O)-w (Na2O)-w (CaO) of gneiss and foliated granites in ultra-high-pressure and core complex units

      图  4  安徽岳西大别山北部地质简图

      1.边界断裂; 2.滑脱带; 3.花岗岩; 4.镁铁质-超镁铁质侵入岩; 5.变形橄榄岩; 6.榴辉岩.CC.核部杂岩; UHP.超高压变质单元; BMXF.八里畈-晓天-磨子潭断裂; TLF.郯庐断裂

    • [1] 从柏林, 王清晨. 大别山-苏鲁超高压变质带研究的最新进展[J]. 科学通报, 1999, 44(11): 1127-1141. doi: 10.3321/j.issn:0023-074X.1999.11.002
      [2] 从柏林, 王清晨. 中国高压变质岩评述[J]. 科学通报, 1994, 39(24): 2214-2218. https://cdmd.cnki.com.cn/Article/CDMD-11415-1011077602.htm
      [3] 王清晨, 从柏林. 大别山超高压变质岩的地球动力学意义[J]. 中国科学(D辑), 1996, 26: 271-276. doi: 10.3321/j.issn:1006-9267.1996.03.007
      [4] 王清晨, 从柏林. 大别山超高压变质带的大地构造框架[J]. 岩石学报, 1998, 14: 481-492. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB804.006.htm
      [5] 李曙光, Jagoutz E, 肖益林, 等. 大别山-苏鲁地体超高压变质年代学: Ⅰ. Sm-Nd同位素体系[J]. 中国科学(D辑), 1996, 26: 249-257. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199603008.htm
      [6] 李曙光, 李惠民, 陈移之, 等. 大别山-苏鲁地体超高压变质年代学: Ⅱ. U-Pb同位素体系[J]. 中国科学(D辑), 1997, 27: 200-206. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199703001.htm
      [7] Ernst WG, Liou J G. Contrasting plate-tectonic styles of Qinling-Dabie-Sulu and Franciscan metamorphic belts[J]. Geology, 1995, 23: 353-356.
      [8] Hacker B R, Wang X, Eide E A, et al. Qinling-Dabie ultrahigh-pressure metamorphism in central China[J]. Tectonics, 1996, 14: 994-1006.
      [9] Liou J G, Zhang R Y, Eide E A, et al. Metamorphism and tectonics of high-p and ultrahigh-p belts in Dabie-Sulu regions, eastern Central China[A]. In: Yin A, Harrison TM, eds. The Tectonic evolution of Asia, Rubey volumeⅨ[C]. Cambridge, United Kingdom: Cambridge University Press, 1996. 300-343.
      [10] Jahn BM. Geochemical and isotopic characteristics of UHP eclogites and ultramafic rocks of the Dabie orogen: implications for continental subduction and collisional tectonics[A]. In: Hacker B R, Liou JG, eds. When continents collide: geodynamics of ultrahigh-pressure rocks[C]. Dordrecht/ Boston/ London: Kluwer Academic Publisher, 1998. 203-239.
      [11] Okay A I, Sengor AM C. Tectonics of an ultrahigh-pressure metamorphic terrane: the Dabie Shan/Tongbai Shan orogen, China[J]. Tectonics, 1993, 12: 1320-1334. doi: 10.1029/93TC01544
      [12] Suo S T, Zhong Z Q, You Z D. Extensional deformation of post-ultrahigh pressure metamorphism and exhumation process of ultrahigh-pressure metamorphic rocks in the Dabie massif, China[J]. Science in China(Series D), 2000, 43(3): 225 -236. doi: 10.1007/BF02906818
      [13] Webb L E, Hacher B R, Ratschbacher L, et al. Thermochronologic constraints on deformation and cooling history of high-and ultrahigh-pressure rocks in the Qinling-Dabie orogen, eastern China[J], Tectonics, 1999, 18(4): 621638.
      [14] Davis G H. Shear zone modal for the origin of metamorphic core complex[J]. Geology, 1983, 11(6): 342-347. doi: 10.1130/0091-7613(1983)11<342:SMFTOO>2.0.CO;2
      [15] 索书田, 桑隆康, 韩郁菁, 等. 大别山前寒武纪地体岩石学与构造学[M]. 武汉: 中国地质大学出版社, 1993.
      [16] Suo S T, Zhong Z Q. Rheology of ancientmiddle-lower continental crust in Qinling Orogenic Belt, central China[A]. In: Zheng Y D, Davis G H, eds. Proc 30th Int'l Geol Congr [C]. Holland: VSP, 1997, 14: 16-26.
      [17] Zhang HF, Zhang B R, Zhong Z Q. Geochemistry of gneisses from Dabie complex and Tongbai complex in Qinling-Tongbai-Dabie orogenic belt: implications for location of YangtzeSino-Korean suture[J]. Journal of China University of Geosiences, 2000, (4): 392-405.
      [18] 刘贻灿, 徐树桐, 陈冠宝, 等. 大别山北部中酸性片麻岩的岩石地球化学特征及其古大地构造意义[J]. 大地构造与成矿学, 1999, 23(3): 222-229. doi: 10.3969/j.issn.1001-1552.1999.03.004
      [19] Xie Z, Chen J F, Zhou TX, et al. U-Pb zircon ages of the rocks in the North Dabie Terrain, China[J]. Scientia Geologica Sinica, 1998, 7(4): 501-511.
      [20] 吴元保, 陈道公, Deloule E, 等. 北大别片麻岩的锆石U -Pb年龄离子探针测定及其地质意义[J]. 地质论评, 47(3): 239-244.
      [21] 游振东, 韩郁菁, 杨巍然, 等. 东秦岭大别高压超高压变质带[M]. 武汉: 中国地质大学出版社, 1998.
      [22] Zhong Z Q, ZhangHF, Suo S T, et al. Patial melting in exhumation of ultrahigh-pressure metamophic rocks, Dabieshan Mountains, China[J]. Journal of China University of Geosciences, 1999, 10(3): 194-199.
      [23] 刘景波, 吴颍, 国连杰. 榴辉岩和围岩片麻岩之间的关系: 来自片麻岩副矿物包裹体的研究[J]. 科学通报, 1997, 42(23): 2531-2534. doi: 10.3321/j.issn:0023-074X.1997.23.016
      [24] Ye K, Yao Y, Katayama I, et al. Large areal extentof ultrahigh-pressure metamorphism in the Sulu ultrahigh-pressure terrane of east China: new implications from coesite and omphacite inclusion in zircon of granitic gneisses[J]. Lithos, 2000, 52: 157-164. doi: 10.1016/S0024-4937(99)00089-4
      [25] Carswell D A, Wilson RA, Zhai M. Metamorphic evolution, mineral chemistry and thermobarometry of schists and orthogneisses hosting ultrahigh-pressure eclogite in the Dabieshan of central China[J]. Lithos, 2000, 52: 121155.
      [26] 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[J]. 科学通报, 1997, 2(17): 1832-1835. doi: 10.3321/j.issn:0023-074X.1997.17.012
      [27] 徐树桐, 苏文, 吴怡灿, 等. 大别山北部榴辉岩的发现及其岩相学特征[J]. 科学通报, 1999, 44(13): 1452-1456. doi: 10.3321/j.issn:0023-074X.1999.13.021
      [28] 刘景波, 游振东, 钟增球. 豫南鄂北大别山中部和北部的榴辉岩类[J], 中国科学(D辑), 1996, 26(3): 277-281. doi: 10.3321/j.issn:1006-9267.1996.03.008
      [29] 马文璞. 大别山北麓的石炭系及其大地构造意义[J]. 地质学报, 1991, 65(1): 7-26. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199101001.htm
      [30] Zhang Q, Mao B, Liu R, et al, A relic slice of continental lithospheric mantle[J]. Science in China(Series B), 1995, 25(8): 867-873.
      [31] 李曙光, 洪吉安, 李惠民, 等. 大别山辉石岩-辉长岩体的锆石U-Pb年龄及其地质意义[J]. 高校地质学报, 1999, 5(3): 351-355. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX199903015.htm
      [32] Li S, Nie Y, Zheng S, et al. Interaction between subducted continental crust and upper mantle: major and trace elements of the syn-collision mafic-ultramafic rocks[J]. Science in China(Series D), 1998, 28: 18-22.
      [33] 谢智, 陈江峰, 周泰禧, 等. 大别造山带变质岩和花岗岩的钕同位素组成及其地质意义[J]. 岩石学报, 1996, 12 (3): 401-408. doi: 10.3321/j.issn:1000-0569.1996.03.005
      [34] Wang C, Zeng R, Mooney W O, et al. A crustal model of the ultrahigh-pressure Dabie Shan orogenic belt, China derived from deep seismic refraction profiling. Journal of Geophysical Research, 2000, 105: 10857-10869. doi: 10.1029/1999JB900415
      [35] Zhai MG, Cong B L, Zhao Z Y, et al. Petrological-tectonic units in the coesite-bearing metamorphic terrain of the Dabie mountains, central China and their geotectonic implications [J]. Journal of Southeast Asian Earth Sciences, 1995, 11 (1): 1-13. doi: 10.1016/0743-9547(94)00036-E
      [36] Wang Q C, Liu X H, Maruyama S, et al. Top boundary of the Dabie UHPM rocks, central China and their geotectonic implications[J]. Journal of Southeast Asian Earth Sciences, 1995, 11(4): 295-300. doi: 10.1016/0743-9547(94)00035-D
      [37] 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[J]. 地质学报, 1992, 66(1): 1-15. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199201000.htm
      [38] Hacker B R, Ratschbacher L, Webb L. U/Pb zircon ages constrain the architecture of the ultrahigh-pressure QinlingDabie orogen, China[J]. Earth and Planetary Science Letters, 1998, 161(1-4): 215-236. doi: 10.1016/S0012-821X(98)00152-6
      [39] 游振东, 钟增球, 张泽明. 桐柏-大别山区高压变质相的构造配置[J]. 地学前缘, 1999, 6(4): 237-245. doi: 10.3321/j.issn:1005-2321.1999.04.006
    • 加载中
    图(4)
    计量
    • 文章访问数:  4223
    • HTML全文浏览量:  508
    • PDF下载量:  25
    • 被引次数: 0
    出版历程
    • 收稿日期:  2001-07-05
    • 刊出日期:  2001-11-25

    目录

      /

      返回文章
      返回