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    雪峰山西侧梵净山—桑植地区构造变形特征

    周小军 李三忠 王岳军 刘静

    周小军, 李三忠, 王岳军, 刘静, 2011. 雪峰山西侧梵净山—桑植地区构造变形特征. 地球科学, 36(6): 985-992. doi: 10.3799/dqkx.2011.104
    引用本文: 周小军, 李三忠, 王岳军, 刘静, 2011. 雪峰山西侧梵净山—桑植地区构造变形特征. 地球科学, 36(6): 985-992. doi: 10.3799/dqkx.2011.104
    ZHOU Xiao-jun, LI San-zhong, WANG Yue-jun, LIU Jing, 2011. Tectonic Features of the Fanjing Mount and Sangzhi Area on the West of Xuefeng Uplift. Earth Science, 36(6): 985-992. doi: 10.3799/dqkx.2011.104
    Citation: ZHOU Xiao-jun, LI San-zhong, WANG Yue-jun, LIU Jing, 2011. Tectonic Features of the Fanjing Mount and Sangzhi Area on the West of Xuefeng Uplift. Earth Science, 36(6): 985-992. doi: 10.3799/dqkx.2011.104

    雪峰山西侧梵净山—桑植地区构造变形特征

    doi: 10.3799/dqkx.2011.104
    基金项目: 

    中国石化总公司重大科技攻关项目"中国南方(中上扬子)大陆构造与海相油气前景" G0800-06-ZS281

    详细信息
      作者简介:

      周小军(1978-), 男, 讲师, 主要从事含油气盆地构造解析方向研究.E-mail: zhouxiaojun2000@sina.com

    • 中图分类号: P544

    Tectonic Features of the Fanjing Mount and Sangzhi Area on the West of Xuefeng Uplift

    • 摘要: 梵净山—桑植地区是雪峰山西缘扩展构造带的一部分, 该区构造变形复杂, 阐明该地区构造变形特征, 不但能够更好的认识和理解江南—雪峰隆起带及其周缘的构造变形特征, 而且能够更好的指导我国南方海相油气勘探.本文通过对该区域复杂构造特征的详细解析, 厘定出该区发育了NEE-EW和NE走向两幕印支期变形, 以及NE向和NNE-NS走向两幕燕山期变形.结合区域大地构造背景, 认为印支期的构造变形, 主要与古特提斯洋的关闭、扬子板块与华北板块的剪刀式拼合有关; 燕山期的构造变形, 主要与伊泽奈崎板块和库拉-太平洋板块的俯冲有关.

       

    • 图  1  梵净山地区构造简图

      Ⅰ.雪峰山核部隆起带;Ⅱ.雪峰山西缘扩展带;Ⅲ.齐岳山隔槽式复合构造带;F1.慈利-保靖断裂;F2.龙里-印江断裂

      Fig.  1.  The structure map of Fanjing Mountain

      图  2  石门和酉阳附近加里东期平行不整合特征(图例见图 1)

      Ⅱ.雪峰山西缘扩展带;Ⅲ.齐岳山隔槽式复合构造带;F1.慈利-保靖断裂;F2.龙里-印江断裂

      Fig.  2.  The Caledonian parallel unconformity near Shimen and Youyang

      图  3  石门和桑植附近印支期不整合特征(图例见图 1)

      Ⅰ.雪峰山核部隆起带;Ⅲ.齐岳山隔槽式复合构造带;F1.慈利-保靖断裂;F2.龙里-印江断裂

      Fig.  3.  The Indo-Chinese unconformity near Shimen and Sangzhi

      图  4  印支期两幕褶皱发育特征

      F1.慈利-保靖断裂;F2.龙里-印江断裂

      Fig.  4.  The feature of the two episodes deformation in Indosinian epoch

      图  5  桑植附近燕山期不整合特征

      Fig.  5.  The Yanshanian unconformity near Sangzhi

      图  6  燕山期二幕褶皱特征

      F1.慈利-保靖断裂;F2.龙里-印江断裂

      Fig.  6.  The second episode deformation in Yanshan epoch

      图  7  酉阳—松桃剖面上断层发育特征

      Fig.  7.  The faults in the Youyang-Songtao profile

      图  8  研究区区印支—燕山期构造变形机制

      a.印支期一幕变形机制;b.印支期二幕变形机制;c.燕山一幕变形机制;d.燕山二幕变形机制

      Fig.  8.  The deformation mechanism from Indosinian epoch to Yanshan epoch in this area

    • Cheng, Y.Q., 1994. The generality of China regional geology. Geological Publishing House, Beijing (in Chinese).
      Cui, M., Tang, L.J., Guo, T.L., et al., 2009. Structural style and thrust breakthrough model of fold in Southeast Guizhou. Earth Science—Journal of China University of Geosciences, 34(6): 907-913 (in Chinese with English abstract). doi: 10.3799/dqkx.2009.103
      Ding, D.G., Guo, T.L., Hu, M.X., et al., 2007. Basement decoupling structure in Jiangnan-Xuefeng-series 1 of the southern structure studies. Petroleum Geology & Experiment, 29(2): 120-127, 132 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYSD200702004.htm
      Ding, D.G., Pan, W.L., Peng, J.N., et al., 2008. Transformation and deformation of the Meso-Paleozoic basins in the Yangtze Plate. Oil & Gas Geology, 29(5): 597-606 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_oil-gas-geology_thesis/0201218371691.html
      Dong, W.P., 1997. Stratigraphy (lithostratic)of Guizhou Province (Bureau of Geology and Mineral Resources of Guizhou Province). China University of Geosciences Press, Wuhan (in Chinese).
      Fan, X.L., Jiang, X.G., Jiang, H.K., et al., 1994. Preliminary study on the deep geological structure in the Xuefeng area (the Jiangkou-Dongkou section). Experimental Petroleum Geology, 16(2): 128-135 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYSD402.002.htm
      Gao, C.L., Shan, X.L., Qin, D.Y., 2005. The basement tectonic characteristics of the Paleozoic basin, China. Petroleum Geology & Experiment, 27(6): 551-558, 564 (in Chinese with English abstract).
      Guo, L.Z., Shi, Y.S., Ma, R.S., et al., 1984. Tectonostratigraphic terranes of Southeast China. Journal of Nanjing University, 20(4): 732-739 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SXXT198404014.htm
      Jin, C., Li, S.Z., Wang, Y.J., et al., 2009. Diachronous and progressive deformation during the Indosinian-Yanshanian movements of the Xuefeng Mountain intracontinental composite tectonic system. Oil & Gas Geology, 30(5): 598-607 (in Chinese with English abstract). http://www.researchgate.net/publication/285873188_Diachronous_and_progressive_deformation_during_the_Indosinian-Yanshanian_movements_of_the_Xuefeng_Mountain_intracontinental_composite_tectonic_system
      Li, S.G., Hart, S.R., Zheng, S.G., et al., 1989. Timing of collision between the North and South China blocks—the Sm-Nd isotopic age evidence. Science in China (Ser. B), 32(11): 1393-1400. http://www.cnki.com.cn/Article/CJFDTotal-JBXG198911011.htm
      Ma, L., Chen, H.J., Gan, K.W., et al., 2004. Geotectonics and petroleum geology of marine sedimentary rocks in Southern China(Book 1 and 2). Geological Publishing House, Beijing (in Chinese).
      Qiu, Y.X., 1994. Fanjingshan "klippe" and Lantian tectonic window—views on the Jiangnan-Xuefeng nappe. Geology of Anhui, 4(1-2): 23-26 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-AHDZ4Z1.003.htm
      Qiu, Y.X., Ma, W.P., Fan, X.L., et al., 1996. Tectonic nature and tectonic evolution of the "Xuefengoldland" in the caledonian stage. Regional Geology of China, 2: 150-160 (in Chinese with English abstract). http://www.researchgate.net/publication/285855537_Tectonic_nature_and_tectonic_evolution_of_the_'Xuefeng_Oldland'_in_the_Caledonian_stage
      Qiu, Y.X., Zhang, Y.C., Ma, W.P., et al., 1999. The Tectonic nature and evo1ution of Xuefeng Mountains: the formation and evolution of a intracontinent orogen. Geological Publishing House, Beijing (in Chinese).
      Ren, J.S., Niu, B.G., Liu, Z.G., 1999. Soft collision, superposition orogeny and polycyclic suturing. Earth Science Frontiers, 6(3): 85-93 (in Chinese with English abstract). http://www.researchgate.net/publication/310793773_Soft_collision_superposition_orogeny_and_polycyclic_suturing
      Xu, Z.Q., Lu, Y.L., Tang, Y.Q., et al., 1988. The formation of the complex mountain chain in the east of Qinling. China Environment and Science Press, Beijing (in Chinese).
      Yin, H.F., Peng, Y.Q., 1995. Evolution of the Phanerozoic paleo-ocean of Qinling. Earth Science—Journal of China University of Geosciences, 20(6): 605-611 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX506.000.htm
      Yin, H.F., Wu, S.B., Du, Y.S., et al., 1999. South China defined as part of Tethyan archipelagic ocean system. Earth Science—Journal of China University of Geosciences, 24(1): 1-12 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX901.000.htm
      Zhang, G.W., 1988. Formation and evolution of the Qinling orogenic belt. Northwest University Press, Xi'an (in Chinese).
      Zhu, X., 1983a. Notes on geodynamic background of the Meso-Cenozoic petroliferous basins in China. In: Zhu, X., ed., Notes on the tectonic of petroliferous basins in China. Petroleum Industry Press, Beijing (in Chinese).
      Zhu, X., 1983b. Notes on ancient global tectonics and paleozoic petroliferous basins. Oil & Gas Geology, 4(1): 1-33 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT198301000.htm
      程裕淇, 1994. 中国区域地质概论. 北京: 地质出版社.
      崔敏, 汤良杰, 郭彤楼, 等, 2009. 黔东南地区褶皱构造样式及其断层突破模式. 地球科学——中国地质大学学报, 34(6): 907-913. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200906005.htm
      丁道桂, 郭彤楼, 胡明霞, 等, 2007. 论江南-雪峰基底拆离式构造——南方构造问题之一. 石油实验地质, 29(2): 120-127, 132. doi: 10.3969/j.issn.1001-6112.2007.02.003
      丁道桂, 潘文蕾, 彭金宁, 等, 2008. 扬子板块中、古生代盆地的改造变形. 石油与天然气地质, 29(5): 597-606. doi: 10.3321/j.issn:0253-9985.2008.05.008
      董卫平, 1997. 贵州省岩石地层(全国地层多重划分对比研究52). 武汉: 中国地质大学出版社.
      范小林, 江兴歌, 蒋洪堪, 等, 1994. 雪峰区(江口-洞口)深部地质构造初探. 石油实验地质, 16(2): 128-135. https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD402.002.htm
      高长林, 单翔麟, 秦德余, 2005. 中国古生代盆地基底大地构造特征. 石油实验地质, 27(6): 551-558, 564. doi: 10.3969/j.issn.1001-6112.2005.06.001
      郭令智, 施央申, 马瑞士, 等, 1984. 中国东南部地体构造的研究. 南京大学学报, 20 (4): 732-739. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ198404014.htm
      金宠, 李三忠, 王岳军, 等, 2009. 雪峰陆内复合构造系统印支-燕山期构造穿时递进特征. 石油与天然气地质, 30(5): 598-607. doi: 10.3321/j.issn:0253-9985.2009.05.010
      李曙光, Hart, S.R., 郑双根, 等, 1989. 中国华北、华南陆块碰撞时代的钐-钕同位素年龄证据. 中国科学(B辑), 19(3): 312-319. https://www.cnki.com.cn/Article/CJFDTOTAL-JBXK198903011.htm
      马力, 陈焕疆, 甘克文, 等, 2004. 中国南方大地构造和海相油气地质(上、下卷). 北京: 地质出版社.
      丘元禧, 1994. 从梵净山"飞来峰"到兰田构造窗——对江南-雪峰推(滑)体的若干认识. 安徽地质, 4(1-2): 23-26. https://www.cnki.com.cn/Article/CJFDTOTAL-AHDZ4Z1.003.htm
      丘元禧, 马文璞, 范小林, 等, 1996. "雪峰古陆"加里东期的构造性质和构造演化. 中国区域地质, 2: 150-160. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD602.007.htm
      丘元禧, 张渝昌, 马文璞, 等, 1999. 雪峰山的构造性质与演化: 一个陆内造山带的形成演化模式. 北京: 地质出版社.
      任纪舜, 牛宝贵, 刘志刚, 1999. 软碰撞、叠覆造山和多旋回缝合作用. 地学前缘, 6(3): 85-93. doi: 10.3321/j.issn:1005-2321.1999.03.008
      许志琴, 卢一伦, 汤耀庆, 等, 1988. 东秦岭复合山链的形成. 北京: 中国环境科学出版社.
      殷鸿福, 彭元桥, 1995. 秦岭显生宙古海洋演化. 地球科学——中国地质大学学报, 20(6): 605-611. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX506.000.htm
      殷鸿福, 吴顺宝, 杜远生, 等, 1999. 华南是特提斯多岛洋体系的一部分. 地球科学——中国地质大学学报, 24(1): 1-12. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX901.000.htm
      张国伟, 1988. 秦岭造山带的形成及其演化. 西安: 西北大学出版社.
      朱夏, 1983a. 试论中国中、新生代油气盆地的地球动力学背景. 见: 朱夏编著, 论中国含油气盆地构造. 北京: 石油工业出版社.
      朱夏, 1983b. 试论古全球构造与古生代油气盆地. 石油与天然气地质, 4(1): 1-33. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT198301000.htm
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    • 收稿日期:  2011-03-10
    • 网络出版日期:  2021-11-10
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