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    湖南NW向常德-安仁断裂的地质特征、活动历史及构造性质

    柏道远 李银敏 钟响 李彬 黄乐清 伍贵华 李超 姜文

    柏道远, 李银敏, 钟响, 李彬, 黄乐清, 伍贵华, 李超, 姜文, 2018. 湖南NW向常德-安仁断裂的地质特征、活动历史及构造性质. 地球科学, 43(7): 2496-2517. doi: 10.3799/dqkx.2018.571
    引用本文: 柏道远, 李银敏, 钟响, 李彬, 黄乐清, 伍贵华, 李超, 姜文, 2018. 湖南NW向常德-安仁断裂的地质特征、活动历史及构造性质. 地球科学, 43(7): 2496-2517. doi: 10.3799/dqkx.2018.571
    Bai Daoyuan, Li Yinmin, Zhong Xiang, Li Bin, Huang Leqing, Wu Guihua, Li Chao, Jiang Wen, 2018. Geological Features, Activity History and Tectonic Attribute of NW-Trending Changde-Anren Fault in Hunan. Earth Science, 43(7): 2496-2517. doi: 10.3799/dqkx.2018.571
    Citation: Bai Daoyuan, Li Yinmin, Zhong Xiang, Li Bin, Huang Leqing, Wu Guihua, Li Chao, Jiang Wen, 2018. Geological Features, Activity History and Tectonic Attribute of NW-Trending Changde-Anren Fault in Hunan. Earth Science, 43(7): 2496-2517. doi: 10.3799/dqkx.2018.571

    湖南NW向常德-安仁断裂的地质特征、活动历史及构造性质

    doi: 10.3799/dqkx.2018.571
    基金项目: 

    中国地质调查局项目 DD20160031

    详细信息
      作者简介:

      柏道远(1967-), 男, 研究员级高级工程师, 长期从事区域地质调查与基础地质研究

    • 中图分类号: P542;P548

    Geological Features, Activity History and Tectonic Attribute of NW-Trending Changde-Anren Fault in Hunan

    • 摘要: 常德-安仁断裂是湖南东部一条NW向大断裂,关于其地质特征、活动历史及构造性质等尚缺乏系统研究.基于区域地质调查和基础地质研究资料,总结了常德-安仁断裂的总体特征,重塑了断裂的活动历史,探讨了断裂的构造性质和变形机制.主要认识如下:常德-安仁断裂走向NW330°,为一基底隐伏断裂,地质上表现为一NW向岩浆隆起带.该断裂为贯穿中、下地壳并切入岩石圈地幔的深大断裂,断裂倾向NE,倾角约54°.断裂具有长期活动历史:新元古代冷家溪期作为转换断层具走滑活动;冷家溪末期武陵(晋宁)运动中在区域S-N向挤压下右行走滑;板溪期早期和南华纪早期均具伸展活动并控制沉积相带的展布;加里东运动中在区域S-N向挤压下右行走滑;中三叠世晚期印支运动中在区域NW-NWW向挤压下左行走滑兼逆冲;晚三叠世-早侏罗世在区域S-N向挤压下右行走滑;中侏罗世晚期早燕山运动中在区域NWW向挤压下左行走滑;白垩纪-古近纪产生伸展活动.常德-安仁断裂在冷家溪期可能为一横切扬子陆块东南缘弧后盆地、岛弧和华南洋的转换断层.印支运动中断裂带因深部逆冲活动而构造隆升.该断裂具隐伏特征的原因可能与冷家溪期-南华纪同沉积活动、震旦系底部滑脱层发育、多条NE-NNE向大断裂的截切以及断裂沿线花岗岩体和断陷盆地的发育等有关.

       

    • 图  1  研究区区域地质图

      Fig.  1.  Regional geological sketch of research area

      图  2  结晶基底顶界面埋深

      图据湖南省地质调查院(2017)修改

      Fig.  2.  Inference of crystalline basement isobaths

      图  3  莫霍面构造推断图

      图据湖南省地质调查院(2017)修改

      Fig.  3.  Structural inference on the Moho surface

      图  4  岩石圈厚度

      图据湖南省地质调查院(2017)修改

      Fig.  4.  Inference on the lithosphere thickness

      图  5  武潭-桃江地区地质图

      位置见图 1;据湖南省1:50万地质图、1:25万益阳市幅地质图(湖南省地质调查院,2017)修改.Q.第四系;KEb.白垩系-古近系百花亭组;C.石炭系;D3.上泥盆统;D2.中泥盆统;S.志留系;O.奥陶系;∈.寒武系;Z.震旦系;Nh.南华系;Qb2bh+n.青白口系板溪群百合垅组和牛牯坪组;Qb2w+dy.板溪群五强溪组和多益塘组;Qb2dy.板溪群多益塘组;Qb2t.板溪群通塔湾组;Qb2m.板溪群马底驿组;Qb2hl+m.板溪群横路冲组和马底驿组;Qb1x.青白口系冷家溪群小木坪组;Qb1h.冷家溪群黄浒洞组;Qb1l.冷家溪群雷神庙组;Qb1p.冷家溪群潘家冲组;Qb1y.冷家溪群易家桥组;γT.三叠纪花岗岩.1.青白口系板溪群;2.青白口系冷家溪群;3.花岗岩;4.断裂;5.平移断裂;6.逆断裂;7.地质界线/角度不整合地质界线;8.地层产状;9.断裂编号.F1.牛田断裂;F2.大福坪断裂;F3.长塘断裂;F4.安化-马迹塘断裂;F5.丰家铺-谢林港断裂

      Fig.  5.  Geological sketch of Wutan-Taojiang area

      图  6  常德-安仁断裂(CAF)不同阶段活动派生构造

      Fig.  6.  Secondary structures in different periods origined from Changde-Anren fault (CFA)

      图  7  桃花江水库地区地质图

      位置见图 1;Qh.全新统;C1zs.下石炭统樟树湾组;C1sb.下石炭统尚保冲组;D3w.上泥盆统吴家坊组;D3yl.上泥盆统岳麓山组;D2q.中泥盆统棋梓桥组;D2y.中泥盆统易家湾组;D2t.中泥盆统跳马涧组;S1lj.下志留统两江河组;O2-3y-OSl.奥陶系烟溪组-志留系龙马溪组;O1-2q.下-中奥陶统桥亭子组;O1bs.中奥陶统白水溪组;∈2-3w~∈3-4t.寒武系污泥塘组和探溪组;∈1-2n.下寒武统牛蹄塘组;Z.震旦系;Nh3.上南华统;Nh1-2.下-中南华统;Qb2n.青白口系板溪群牛牯坪组.1.断裂;2.平移断裂;3.逆断裂;4.整合地质界线;5.角度不整合地质界线;6.岩层产状;7.断裂编号.F1.油次冲-杨家坳断裂;F2.石鸭头断裂;F3.台山冲断裂;F4.杨家仑断裂;F5.王家山断裂

      Fig.  7.  Geological map of Taohuajiang reservoir area

      图  8  川口地区地质图

      位置见图 1;据湖南省1:50万地质图和1:5万铁丝塘幅和草市幅地质图(湖北地质调查院,2017)修改.E.古近系;K.白垩系;T1.下三叠统;P2-P3.中-上二叠统;CPH.上石炭统-下二叠统壶天群;D3.上泥盆统;D2.中泥盆统;Nh.南华系;Qb2y.青白口系高涧群岩门寨组;Qb1x.青白口系冷家溪群小木坪组;Qb1h.冷家溪群黄浒洞组;γT.三叠纪花岗岩;γS.志留纪花岗岩.1.断裂;2.逆平移断裂;3.正断裂;4.地质界线;5.角度不整合地质界线.F1.水垅冲断裂;F2.草市断裂

      Fig.  8.  Geological sketch of Chuankou area

      图  9  水垅冲断裂特征

      a.断裂剖面(水垅冲).①粉砂质板岩;②钙质页岩;③粉砂岩;Qb1x.冷家溪群小木坪组;D2y.泥盆系易家湾组;b.断裂剖面(高湖西侧).①劈理化带;②褶皱;③页岩;④泥岩;D3o.泥盆系欧家冲组;c.断裂露头(高湖西侧)

      Fig.  9.  Feature of Shuilongchong fault

      图  10  油次冲-杨家坳断裂露头

      Fig.  10.  Outcrop of Youcichong-Yangjia'ao fault

      图  11  韶山-湘乡地区地质图

      位置见图 1;据湖南省1:50万地质图(湖南省地质调查院,2017)、1:25万邵阳市幅地质图和1:25万株洲市幅地质图修改.Q.第四系;E1.古近系;K2.上白垩统;K1.下白垩统;J1.下侏罗统;T3.上三叠统;T1.下三叠统;P2-P3.中-上二叠统;CPH.上石炭统-下二叠统壶天群;C1.下石炭统;D3.上泥盆统;D2.中泥盆统;∈1.下寒武统;Z.震旦系;Nh.南华系;Qb2.青白口系板溪群、高涧群;γJ.侏罗纪花岗岩;γT.三叠纪花岗岩.1.断裂;2.逆断裂;3.正断裂;4.地质界线;5.角度不整合地质界线;6.地层产状;7.断裂编号.F1.棋梓-乌石断裂;F2.杨林断裂;F3.中沙断裂;F4.月山断裂;F5.翻江断裂

      Fig.  11.  Geological sketch of Shaoshan-Xiangxiang area

      图  12  溪江地区地质图

      位置见图 1;据湖南省1:50万地质图(湖南省地质调查院,2017)、1:25万邵阳市幅地质图修改.K2.上白垩统;K1.下白垩统;CPH.上石炭统-下二叠统壶天群;C1.下石炭统;D3.上泥盆统;D2.中泥盆统;O.奥陶系;∈.寒武系;Z.震旦系;Nh.南华系;Qb2j+y.青白口系高涧群架枧田组和岩门寨组;Qb2z.高涧群砖墙湾组组;Qb2s+hs.高涧群石桥铺组和黄狮洞组;Qb1x.青白口系冷家溪群小木坪组;γT.三叠纪花岗岩;γS.志留纪花岗岩;1.断裂;2.平移断裂;3.正断裂;4.地质界线;5.角度不整合地质界线.F1.界牌断裂;F2.枣子坪断裂

      Fig.  12.  Geological sketch of Xijiang area

      图  13  枣子坪断裂露头

      白色箭头所指处发育指示右行走滑的正阶步

      Fig.  13.  Outcrop of Zaoziping fault

      图  14  板溪期早期岩相古地理格局

      湖南省地质调查院(2017)修改;Ⅰ.河流-滨海相区;Ⅱ.广海陆棚相区;Ⅲ.陆坡相区;Ⅳ.洞庭古陆

      Fig.  14.  Paleogeography in Early Banxi Period

      图  15  南华纪早期岩相古地理

      湖南省地质调查院(2017)修改;Ⅰ.后滨沼泽-泻湖浮冰相区;Ⅱ.滨岸浮冰带相区;Ⅲ.陆棚-陆坡浮冰带相区;Ⅳ.边缘海槽盆浮冰相区;Ⅴ.古陆

      Fig.  15.  Paleogeography in Early Nanhuan Period

      图  16  冷家溪期构造格局推断图

      Fig.  16.  Inference on the tectonic framework in Lengjiaxi Period

      表  1  常德-安仁断裂派生次级构造

      Table  1.   Secondary structures origined from Changde-Anren fault

      序号 次级构造类型 形成时代 次级构造及其形成时代依据 常德-安仁断裂活动性质
      1 NWW向褶皱 Qb中期 桃江北面NWW向褶皱,卷入地层为冷家溪群. 武陵运动中在区域S-N向挤压下右行走滑
      2 NWW向逆断裂 S晚期 牛田断裂,切割下古生界并被上古生界所覆;石鸭头断裂,切割下古生界并被上古生界所覆. 加里东运动中在区域S-N向挤压下右行走滑
      3 NW向左行平移断裂 T2晚期 水垅冲断裂,切割最新地层为上古生界且南东段被白垩系所掩,叠加了晚三叠世-早侏罗世逆冲活动. 印支运动中在区域NW(W)向挤压下左行走滑
      4 NWW向逆断裂 T3-J1 油次冲-杨家坳断裂,切割上古生界并被印支期NE向断裂所限;杨林断裂,西端切入晚三叠世花岗岩,东端被侏罗系所掩覆;棋梓-乌石断裂,切割上古生界并被白垩系所掩覆、被印支期NE向断裂所限. 在区域S-N向挤压下右行走滑
      5 NWW向隆起 T3-J1 龙山-桥亭子串珠状隆起,卷入了上古生界并被中侏罗世早燕山运动褶皱叠加;沩山隆起,卷入了上古生界并有三叠纪花岗岩侵位. 在区域S-N向挤压下右行走滑
      6 NEE向右行平移断裂 J2晚期 枣子坪断裂,切割了晚三叠世花岗岩,东端被白垩系所掩覆. 早燕山运动中在区域NWW向挤压下左行走滑
      7 断陷盆地端部或边部断裂 K-E 湘阴凹陷、湘潭盆地、株洲盆地、醴攸盆地等NNE向盆地南西端端部NW向断裂、衡阳盆地北东边界,控制断陷盆地的延伸. 区域伸展构造体制下产生拉张活动
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