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

川西岷江松潘段第四纪与新构造运动特征分析

韩建恩 郭长宝 吴瑞安 任三绍 胥彪 杨志华

韩建恩, 郭长宝, 吴瑞安, 等, 2017. 川西岷江松潘段第四纪与新构造运动特征分析. 地质力学学报, 23 (6): 864-881.
引用本文: 韩建恩, 郭长宝, 吴瑞安, 等, 2017. 川西岷江松潘段第四纪与新构造运动特征分析. 地质力学学报, 23 (6): 864-881.
HAN Jian'en, GUO Changbao, WU Ruian, et al., 2017. CHARACTERISTICS ANALYSIS OF QUATERNARY AND NEOTECTONIC MOVEMENTS FROM SONGPAN SECTION, MINJIANG UPPER REACHES, WESTERN SICHUAN. Journal of Geomechanics, 23 (6): 864-881.
Citation: HAN Jian'en, GUO Changbao, WU Ruian, et al., 2017. CHARACTERISTICS ANALYSIS OF QUATERNARY AND NEOTECTONIC MOVEMENTS FROM SONGPAN SECTION, MINJIANG UPPER REACHES, WESTERN SICHUAN. Journal of Geomechanics, 23 (6): 864-881.

川西岷江松潘段第四纪与新构造运动特征分析

基金项目: 

中国地质调查局项目 DD20160271

中国地质调查局项目 12120113038000

中国地质调查局项目 1212011087114

中国地质科学院地质力学研究所基本科研业务费项 DZLXJK201710

中国地质科学院基本科研业务费项目 YYWF201511

详细信息
    作者简介:

    韩建恩(1980-), 男, 博士, 高级工程师, 构造地质专业, 主要从事区域地质、沉积相与古环境研究。E-mail:hanjianen@163.com

  • 中图分类号: P534.63;P546

CHARACTERISTICS ANALYSIS OF QUATERNARY AND NEOTECTONIC MOVEMENTS FROM SONGPAN SECTION, MINJIANG UPPER REACHES, WESTERN SICHUAN

  • 摘要: 在已有调查研究的基础上,通过野外地质调查和剖面测量,重点分析了岷江松潘段的漳腊盆地、斗鸡台盆地地貌特征、第四纪沉积物类型、物质成分、空间分布等特征,并系统测量和研究了松潘段岷江干流及其支流的河流阶地特征。研究表明,新构造运动控制了松潘段第四纪盆地的形态和地貌演化过程,漳腊盆地和斗鸡台盆地形成于中新世末至上新世初,西侧控盆断裂为东倾正断层,东侧为西倾逆断层,盆地为断块发生西降东升的翘板式断块运动过程中形成的,称之为"翘板式箕状盆地"。松潘段岷江河谷地貌呈现出宽谷和窄谷交替出现的特点,岷江干流及其支流中发育多处湖相地层,沉积特征表现为堰塞湖。岷江上游松潘段最多发育6级阶地,以侵蚀阶地和堆积阶地为主,主要形成于中更新世晚期—全新世时期。阶地级数具有分段性特点,不同区段阶地阶面宽窄不一,受区内新构造活动控制明显。岷江上游新构造运动表现为南北条带性和东西向差异掀斜抬升的特点,红桥关以上整体为构造隆升区,至少具有3次构造隆升,岷江上游斗鸡台盆地构造隆升强度整体上大于漳腊盆地。在尕米寺地区可能发生了6次构造抬升,红桥关一带构造抬升明显要强于漳腊盆地。

     

  • 图  1  岷江上游及其邻区活动构造纲要图(据文献[7]修改)

    a-区域构造纲要图; b-岷江上游活动构造; c-图 3位置

    Figure  1.  Outline map of active tectonics on the upper reaches of the Minjiang River and its adjacent regions

    图  3  岷江断裂带构造简图与实测阶地位置图(据文献[7]修改)

    Figure  3.  Simplified strucural map of the Minjiang fault zone and location of measured terrace sections of the Minjiang river

    图  2  岷江松潘段堆积物类型

    Figure  2.  Deposit types in Songpan section on the upper reaches of the Minjiang River

    图  4  岷江上游沉积盆地第四纪地层特征

    Figure  4.  Characteristics of Quaternary strata in sedimentary basin on the upper reaches of the Minjiang River

    图  5  岷江上游盆地控盆断裂

    Figure  5.  Basin-controlling faults of the basins on the upper reaches of Minjiang River

    图  6  岷江上游盆地“翘板式箕状盆地”形成模式示意图

    1-晚更新统1全新统; 2-中更新统; 3-古近系; 4-石炭系-二叠系; 5-中二叠统; 6-断层; 7-正断层; 8-推测断层

    Figure  6.  Diagram of formation mode of seesaw type dustpan-like basin on the upper reaches of the Minjiang River

    图  7  岷江上游河源至镇江关段河流阶地横剖面图

    Figure  7.  Cross section plan of river terraces from Heyuan to Zhenjiangguan section on the upper reaches of the Minjiang River

    图  8  岷江(弓嘎岭—镇江关)河流阶地位相图

    Figure  8.  River terrace phase diagram of the Minjiang River(Gonggaling-Zhenjiangguan)

    表  1  岷江上游AMS14C测年结果

    Table  1.   AMS14C dating results of shell in lacustrine strata

    样号 实验室编号 测年材料 14C年龄/a BP 校正年龄/a BP 资料来源
    SCL16G1050-1 Beta-446565 炭块 11210±40 11250±40 样品采集
    - Beta-320196 炭块 10180±40 10230±40 文献[18]
    注:AMS14C年龄测试由美国Beta实验室完成
    下载: 导出CSV

    表  2  岷江上游泉华分布点

    Table  2.   Distribution of tufa on the upper reaches of the Minjiang River

    序号 地点 坐标 海拔(m) 性质 时代 流域
    经度 纬度
    1 尕米寺南 103°40′26.33″ 33°53′24.70″ 3318 钙华 岷江干流
    2 山巴乡 103°38′55.45″ 32°50′18.15″ 3050 钙华 岷江干流
    3 漳腊村 103°38′34.22″ 32°47′55.47″ 3050 钙华 岷江干流
    4 窑沟村 103°35′14.15″ 32°37′41.62″ 2878 钙华 岷江干流
    5 二道沟 103°32′38.67″ 32°38′39.87″ 3071 钙华 岷江支流
    6 三联村 103°41′0.17″ 32°34′39.67″ 2969 钙华 岷江支流
    7 扎噶瀑布 103°32′30.95″ 32°34′17.95″ 2921 钙华 现代 岷江支流
    8 黄龙沟 103°49′59.24″ 32°43′28.95″ 3570 钙华 现代 涪江支流
    下载: 导出CSV

    表  3  岷江上游河流阶地高程统计表

    Table  3.   Statistical table of terrace elevation on the upper reaches of the Minjiang River

    序号 地点 坐标 河面海拔/m 拔河高度/m
    经度 纬度 T1 T2 T3 T4 T5 T6
    1 黄泥坡 103°41′57.74″ 33°0′25.50″ 3420 7.1 13.0 19.0
    2 七藏沟口 103°41′53.45″ 32°59′0.25″ 3345 6.0 29.0 36.0
    3 卡卡沟口 103°41′24.20″ 32°58′32.63″ 3330 7.0 39.0 44.0
    4 卡卡沟 103°42′25.18″ 32°57′27.29″ 3290 7.0 28.0 37.0 41.0 44.0
    5 尕米寺北 103°42′1.06″ 32°55′20.73″ 3226 2.0 15.0 24.0 33.0 35.0 42.0
    6 尕米寺 103°41′0.17″ 32°53′59.66″ 3183 8.0 16.0 25.0 29.0
    7 安备村 103°40′20.29″ 32°53′3.77″ 3137 2.0 4.0 12.0 20.0 24.0 30.0
    8 山巴乡 103°38′57.40″ 32°50′13.71″ 3058 7.0 10.0 28.5
    9 大屯村 103°36′59.51″ 32°43′11.11″ 2921 2.0 14.0 20.0
    10 云屯村 103°37′40.30″ 32°32′23.36″ 2762 4.0 8.7
    11 新塘关 103°39′39.42″ 32°28′33.44″ 2674 2.5
    12 镇江关 103°43′50.65″ 32°20′40.84″ 2509 3.5 6.5
    注:拔河高度使用图帕斯200测距仪和皮尺测制
    下载: 导出CSV

    表  4  岷江上游支流河流阶地统计表

    Table  4.   Statistical table of terrace elevation of brunches on the upper reaches of the Minjiang River

    序号 地点 坐标 河面海拔/m 支流 拔河高度/m
    经度 纬度 T1 T2
    1 七藏沟 103°41′20.71″ 32°59′29.25″ 3404 七藏沟 4.0 10.7
    2 安备村 103°40′26.96″ 32°53′6.21″ 3345 安备沟 33.0 38.0
    3 东北村 103°34′29.88″ 32°47′55.62″ 3055 羊洞河 3.0 17.6
    4 二道海 103°30′30.87″ 32°40′1.20″ 3284 牟尼沟 2.0
    5 桥头 103°32′30.16″ 32°39′17.43″ 3096 牟尼沟 2.0
    6 上寨村 103°32′48.89″ 32°37′46.80″ 3031 牟尼沟 5.0
    7 包座村 103°32′18.37″ 32°36′26.88″ 3013 牟尼沟 2.0
    8 安宏村 103°37′16.18″ 32°30′55.40″ 2741 牟尼沟 2.0
    注:拔河高度使用图帕斯200测距仪和皮尺测制
    下载: 导出CSV

    表  5  岷江上游阶地测年数据表

    Table  5.   Dating data of river terraces on the upper reaches of the Minjiang River

    序号 地点 阶地 拔河高度(m) 测试方法 年龄(ka) 数据质量 资料来源
    1 小西天北 T3 40 TL 31.2±2.3 可信 文献[11]
    2 川盘 T2 25 ESR 287.27 参考 文献[23]
    3 川盘 T2 25 TL 30.2±2.3 可信 文献[4]
    4 川盘 T2 25 TL 46.4±3.7 可信 文献[4]
    5 川盘 T2 28 ESR 642.7 参考 文献[23]
    6 尕米寺 T2 - OSL 46.7±3.1 可信 文献[6]
    7 山巴乡 T4 150 TL 134.8±10.2 参考 文献[4]
    8 漳腊北 T2 60 14C 7.75±0.057 可信 文献[15]
    9 漳腊北 T2 35 14C 6.12±0.057 可信 文献[15]
    10 漳腊 T1 10 14C 2.81±0.077 可信 文献[15]
    11 漳腊 T2 40 TL 15.3±1.2 可信 文献[11]
    12 漳腊 T2 80 TL 23.6±2.0 参考 文献[11]
    13 祁命 T2 120 TL 27±2.1 参考 文献[4]
    14 川主寺 T2 35 14C 12.94±0.185 可信 文献[15]
    15 传子沟 T2 200 14C 23.46±0.350 参考 文献[15]
    16 传子沟 T4 80 IRSL 157±28 参考 文献[15]
    17 传子沟 T4 300 IRSL 254±35 参考 文献[15]
    18 传子沟 T4 160 TL 157.6±11.8 参考 文献[11]
    19 传子沟 T4 250 TL 830±68.9 参考 文献[11]
    20 漳腊盆地 T4 ~140 ESR 264±29 参考 文献[19]
    21 漳腊盆地 T5 ~230 ESR 471±47 参考 文献[19]
    22 漳腊盆地 T6 ~300 ESR 588±76 参考 文献[19]
    23 斗鸡台盆地 T5 ~230 ESR 376.3 参考 文献[38]
    24 斗鸡台盆地 T5 124 ESR 322.6 参考 文献[38]
    下载: 导出CSV
  • [1] 杨景春, 邓天岗, 王元海, 等.岷江上游地区第四纪构造应力状态及其与地震的关系[J].地震地质, 1979, 1(3):68~75. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzdz197903007&dbname=CJFD&dbcode=CJFQ

    YANG Jingchun, DENG Tian'gang, WANG Yuanhai, et al. The Quaternary Tectonic Stress States over the up-stream area of Minjiang river in Sichuan and its relations to earthquakes[J]. Seismology and Geology, 1979, 1(3):68~75.(in Chinese with English abstract) http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzdz197903007&dbname=CJFD&dbcode=CJFQ
    [2] 唐荣昌, 文德华, 黄祖智, 等.松潘-龙门山地区主要活动断裂带第四纪活动特征[J].中国地震, 1991, 7(3):64~71. http://www.cqvip.com/qk/95750x/1991003/661051.html

    TANG Rongchang, WEN Dehua, HUANG Zuzhi, et al. The Quaternary activity characteristics of several major active faults in the Songpan-Longmenshan Region[J]. Earthquake Research in China, 1991, 7(3):64~71.(in Chinese with English abstract) http://www.cqvip.com/qk/95750x/1991003/661051.html
    [3] 唐荣昌, 韩渭宾.四川活动断裂与地震[M].北京:地震出版社, 1993.

    TANG Rongchang, HAN Weibin. Sichuan Active Fault and Earthquake[M]. Beijing:Seismological Press, 1993. (in Chinese)
    [4] 周荣军, 蒲晓虹, 何玉林, 等.四川岷江断裂带北段的新活动、岷山断块的隆起及其与地震活动的关系[J].地震地质, 2000, 22(3):285~294. http://www.cqvip.com/Main/Detail.aspx?id=4527696

    ZHOU Rongjun, PU Xiaohong, HE Yulin, et al. Recent activity of Minjiang Fault Zone, Uplift of Minshan block and their relationship with seismicity of Sichuan[J]. Seismology and Geology, 2000, 22(3):285~294. (in Chinese with English abstract) http://www.cqvip.com/Main/Detail.aspx?id=4527696
    [5] 张岳桥, 杨农, 孟晖.岷江上游深切河谷及其对川西高原隆升的响应[J].成都理工大学学报(自然科学版), 2005, 32(4):331~339. doi: 10.3969/j.issn.1671-9727.2005.04.001

    ZHANG Yueqiao, YANG Nong, MENG Hui. Deep-incised valleys along the Minjiang river upstream and their responses to the uplift of the West Sichuan Plateau, China[J]. Journal of Chengdu University of Technology(Science & Technology Edition), 2005, 32(4):331~339. (in Chinese with English abstract) doi: 10.3969/j.issn.1671-9727.2005.04.001
    [6] 张岳桥, 李海龙, 李建华.青藏高原东缘中更新世伸展作用及其新构造意义[J].地质论评, 2010, 56(6):781~791. http://www.oalib.com/paper/4885146

    ZHANG Yueqiao, LI Hailong, LI Jianhua. Middle Pleistocene extension along the eastern margin of Xizang(Tibetan) Plateau and its neotectonic significance[J]. Geological Review, 2010, 56(6):781~791. (in Chinese with English abstract) http://www.oalib.com/paper/4885146
    [7] 张岳桥, 李海龙, 吴满路, 等.岷江断裂带晚新生代逆冲推覆构造:来自钻孔的证据[J].地质论评, 2012, 58(2):215~223. http://www.oalib.com/paper/4886046

    ZHANG Yueqiao, LI Hailong, WU Manlu, et al. Late Cenozoic thrust and nappe structure along the Minjiang upstream:evidence from a drill hole[J]. Geological Review, 2012, 58(2):215~223. (in Chinese with English abstract) http://www.oalib.com/paper/4886046
    [8] 四川省地质局第二区域地质测量队. 1: 20万漳腊幅区域地质调查报告[R]. 成都: 四川省地质局, 1978.

    The 2nd Regional Geological Survey Team, Geology Bureau of China. The report of regional geological survey of Zhangla sheet at the scale of 1:200000[R]. Chengdu:Geology Bureau of China, 1978. (in Chinese)
    [9] 邓起东, 陈社发, 赵小麟.龙门山及其邻区的构造和地震活动及动力学[J].地震地质, 1994, 16(4):389~403. http://www.cqvip.com/Main/Detail.aspx?id=1309616

    DENG Qidong, CHEN Shefa, ZHAO Xiaolin. Tectonics, scismisity and dynamics of Longmenshan mountains and its adjacent regions[J]. Seismology and Geology, 1994, 16(4):389~403. (in Chinese with English abstract) http://www.cqvip.com/Main/Detail.aspx?id=1309616
    [10] 赵小麟, 邓起东, 陈社发.龙门山逆断裂带中段的构造地貌学研究[J].地震地质, 1994, 16(4):422~428. http://www.cqvip.com/Main/Detail.aspx?id=1309608

    ZHAO Xiaolin, DENG Qidong, CHEN Shefa. Tectonic geomorphology of the Central Segment of the Longmenshan Thrust Belt, western Sichuan, southwestern China[J]. Seismology and Geology, 1994, 16(4):422~428. (in Chinese with English abstract) http://www.cqvip.com/Main/Detail.aspx?id=1309608
    [11] 赵小麟, 邓起东, 陈社发.岷山隆起的构造地貌学研究[J].地震地质, 1994, 16(4):429~439. http://bianke.cnki.net/Web/Article/DZDZ404.017.html

    ZHAO Xiaolin, DENG Qidong, CHEN Shefa. Tectonic Geomorphology of the Minshan uplift in western Sichuan, southwestern China[J]. Seismology and Geology, 1994, 16(4):429~439. (in Chinese with English abstract) http://bianke.cnki.net/Web/Article/DZDZ404.017.html
    [12] 陈社发, 邓起东, 赵小麟, 等.龙门山中段推覆构造带及相关构造的演化历史和变形机制(一)[J].地震地质, 1994, 16(4):404~412. http://www.cqvip.com/QK/95728X/199404/1309607.html

    CHEN Shefa, DENG Qidong, ZHAO Xiaolin, et al. Deformational characteristics, evolutionary history, and deformation mechanism of the Middle Longmenshan thrust-nappes and related tectonics(1)[J]. Seismology and Geology, 1994, 16(4):404~412. (in Chinese with English abstract) http://www.cqvip.com/QK/95728X/199404/1309607.html
    [13] 陈社发, 邓起东, 赵小麟, 等.龙门山中段推覆构造带及相关构造的演化历史和变形机制(二)[J].地震地质, 1994, 16(4):413~421. http://www.cqvip.com/Main/Detail.aspx?id=1309607

    CHEN Shefa, DENG Qidong, ZHAO Xiaolin, et al. Deformational characteristics, evolutionary history, and deformation mechanism of the Middle Longmenshan thrust-nappes and related tectonics(2)[J]. Seismology and Geology, 1994, 16(4):413~421. (in Chinese with English abstract) http://www.cqvip.com/Main/Detail.aspx?id=1309607
    [14] Chen S F, Wilson C J L, Deng Q D, et al. Active faulting and block movement associated with large earthquakes in the Min Shan and Longmen Mountains, northeastern Tibetan Plateau[J]. Journal of Geophysical Research:Solid Earth, 1994, 99(B12):24025~24038. doi: 10.1029/94JB02132
    [15] Kirby E, Whipple K X, Burchfiel B C, et al. Neotectonics of the Min Shan, China:Implications for mechanisms driving Quaternary deformation along the eastern margin of the Tibetan Plateau[J]. GSA Bulletin, 2000, 112(3):375~393. doi: 10.1130/0016-7606(2000)112<375:NOTMSC>2.0.CO;2
    [16] 周荣军, 李勇, Densmore A L, 等.青藏高原东缘活动构造[J].矿物岩石, 2006, 26(2):40~51. http://d.wanfangdata.com.cn/Periodical/kwys200602007

    ZHOU Rongjun, LI Yong, Densmore A L, et al. Active Tectonics of the eastern margin of the Tibet Plateau[J]. Journal of Mineralogyand Petrology, 2006, 26(2):40~51. (in Chinese with English abstract) http://d.wanfangdata.com.cn/Periodical/kwys200602007
    [17] 张会平, 杨农, 张岳桥, 等.岷江水系流域地貌特征及其构造指示意义[J].第四纪研究, 2006, 26(1):126~135. http://www.oalib.com/paper/1571277

    ZHANG Huiping, YANG Nong, ZHANG Yueqiao, et al. Geomorphology of the Minjiang Drainage System(Sichuan, China) and its Structural implications[J]. Quaternary Sciences, 2006, 26(1):126~135. (in Chinese with English abstract) http://www.oalib.com/paper/1571277
    [18] 张军龙, 任金卫, 陈长云, 等.岷江断裂全新世古地震参数及模型[J].地球科学-中国地质大学学报, 2013, 38(S1):83~90. http://www.cqvip.com/QK/94035X/2013S1/1005606332.html

    ZHANG Junlong, REN Jinwei, CHEN Changyun, et al. Paleo-earthquake parameters of Minjiang fault in Holocene[J]. Earth Science-Journal of China University of Geosciences, 2013, 38(S1):83~90. (in Chinese with English abstract) http://www.cqvip.com/QK/94035X/2013S1/1005606332.html
    [19] 张军龙, 陈长云, 李建军, 等.青藏高原东缘活动块体隆升过程与形成机制[M].北京:地质出版社, 2016.

    ZHANG Junlong, CHEN Changyun, LI Jianjun, et al. Uplifting Process and Mechanism of Active Blocks on the Eastern Margin of the Qinghai-Tibetan Plateau[M]. Beijing:Geological Publishing House, 2016. (in Chinese)
    [20] 唐文清, 孙志明.四川松潘弓嘎岭-漳腊盆地新构造运动[J].特提斯地质, 1999, 23:103~107. http://www.cqvip.com/QK/98500A/199900/684848368199900010.html

    TANG Wenqing, SUN Zhiming. The neotectonic movement in the Gonggaling-Zhangla Basin, Songpan, Sichuan[J]. Tethyan Geology, 1999, 23:103~107. (in Chinese with English abstract) http://www.cqvip.com/QK/98500A/199900/684848368199900010.html
    [21] 唐文清, 刘宇平, 陈智梁, 等.岷山隆起边界断裂构造活动初步研究[J].沉积与特提斯地质, 2004, 24(4):31~34. http://www.cqvip.com/Main/Detail.aspx?id=11861723

    TANG Wenqing, LIU Yuping, CHEN Zhiliang, et al. The preliminary study of the tectonic activities along the boundary faults around the Minshan uplift, western Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2004, 24(4):31~34. (in Chinese with English abstract) http://www.cqvip.com/Main/Detail.aspx?id=11861723
    [22] Kirby E, Reiners P W, Krol M A, et al. Late Cenozoic evolution of the eastern margin of the Tibetan Plateau:Inferences from 40Ar/39Ar and (U-Th)/He thermochronology[J]. Tectonics, 2002, 21(1):1001. doi: 10.1029/2000TC001246/pdf
    [23] 杨农, 张岳桥, 孟辉, 等.川西高原岷江上游河流阶地初步研究[J].地质力学学报, 2003, 9(4):363~370. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20030444&flag=1

    YANG Nong, ZHANG Yueqiao, MENG Hui, et al. Study of the Minjiang river terraces in the western Sichuan plateau[J]. Journal of Geomechanics, 2003, 9(4):363~370. (in Chinese with English abstract) http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20030444&flag=1
    [24] 李勇, 黎兵, 周荣军, 等.剥蚀-沉积体系中剥蚀量与沉积通量的定量对比研究——以岷江流域为例[J].地质学报, 2007, 81(3):332~343. http://www.cqvip.com/Main/Detail.aspx?id=24500581

    LI Yong, LI Bing, ZHOU Rongjun, et al. The Quantitative correlation between denudation volume and sedimentary flux in the Denudation-accumulation system:Examples from Minjiang River Drainage system[J]. Acta Geologica Sinica, 2007, 81(3):332~343. (in Chinese with English abstract) http://www.cqvip.com/Main/Detail.aspx?id=24500581
    [25] 吴小平, 胡建中.岷江源地区新构造运动特征[J].现代地质, 2009, 23(3):430~439. http://www.cqvip.com/QK/96868X/200903/30743371.html

    WU Xiaoping, HU Jianzhong. Features of Neotectonic movement in the source area of the Minjiang river[J]. Geoscience, 2009, 23(3):430~439. (in Chinese with English abstract) http://www.cqvip.com/QK/96868X/200903/30743371.html
    [26] 王书兵, 李毅, 夏雄刚, 等.四川茂县较场湖相沉积磁性地层初步研究[J].地质力学学报, 2006, 12(4):416~422. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20060459&flag=1

    WANG Shubing, LI Yi, XIA Xionggang, et al. Magnetostratigraphic study of lake sediments in Jiaochang, Maoxian county, Sichuan[J]. Journal of Geomechanics, 2006, 12(4):416~422. (in Chinese with English abstract) http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20060459&flag=1
    [27] 杨文光, 朱利东, 罗虹, 等.川西漳腊黄土地层与气候变化[J].华南地质与矿产, 2011, 27(3):231~237. http://www.cqvip.com/QK/91196A/201103/39637560.html

    YANG Wenguang, ZHU Lidong, LUO Hong, et al. Stratigraphy of Zhangla Loess in Western Sichuan Plateau and its Paleoclimatic change record[J]. Geology and Mineral Resources of South China, 2011, 27(3):231~237. (in Chinese with English abstract) http://www.cqvip.com/QK/91196A/201103/39637560.html
    [28] 刘再华, 袁道先, Dreybrodt W, 等.四川黄龙钙华的形式[J].中国岩溶, 1993, 12(3):185~191. http://image.hanspub.org:8080/Html/1-1770366_17972.htm

    LIU Zhaihua, YUAN Daoxian, Dreybrodt W, et al. The formation of tufa in Huanglong, Sichuan[J]. Carsologica Sinica, 1993, 12(3):185~191. (in Chinese with English abstract) http://image.hanspub.org:8080/Html/1-1770366_17972.htm
    [29] 王华, 杨更, 覃嘉铭, 等.四川黄龙大湾-张家沟钙华沉积剖面的古气候记录研究[J].地球学报, 2007, 28(5):469~474. http://www.cqvip.com/QK/98325A/200705/25794735.html

    WANG Hua, YANG Geng, QIN Jiaming, et al. Records of Palaeoclimate changes based on the Dawan-Zhangjiagou travertine deposition profile in Huanglong, Sichuan[J]. Acta Geoscientica Sinica, 2007, 28(5):469~474. (in Chinese with English abstract) http://www.cqvip.com/QK/98325A/200705/25794735.html
    [30] 钱洪, 马声浩, 龚宇.关于岷江断裂若干问题的讨论[J].中国地震, 1995, 11(2):140~146. http://www.cqvip.com/qk/95750x/1995002/1957441.html

    QIAN Hong, MA Shenhao, GONG Yu. Discussions on the Minjiang fault[J]. Earthquake Research in China, 1995, 11(2):140~146. (in Chinese with English abstract) http://www.cqvip.com/qk/95750x/1995002/1957441.html
    [31] 徐锡伟, 于贵华, 马文涛, 等.中国大陆中轴构造带地壳最新构造变动样式及其动力学内涵[J].地学前缘, 2003, 10(S1):160~167. http://www.cqvip.com/QK/98600X/2003U08/8196254.html

    XU Xiwei, YU Guihua, MA Wentao, et al. Model of latest crustal tectonic motion of the central tectonic zone on the mainland of China[J]. Earth Science Frontiers, 2003, 10(S1):160~167. (in Chinese with English abstract) http://www.cqvip.com/QK/98600X/2003U08/8196254.html
    [32] Zhang Y Q, Dong S W, Yang N. Active faulting pattern, present-day tectonic stress field and block kinematics in the East Tibetan Plateau[J]. Acta Geologica Sinica(English Edition), 2009, 83(4):694~712. doi: 10.1111/j.1755-6724.2009.00093.x
    [33] 邵兆刚, 孟宪刚, 朱大岗, 等.西藏阿里札达盆地的"翘板式"形成机制[J].地质论评, 2006, 52(2):215~218. http://www.cqvip.com/Main/Detail.aspx?id=21431642

    SHAO Zhaogang, MENG Xian'gang, ZHU Dagang, et al. Formation mechanism of Seesaw type in Zanda basin, Ngari, Xizang(Tibet)[J]. Geological Review, 2006, 52(2):215~218. (in Chinese with English abstract) http://www.cqvip.com/Main/Detail.aspx?id=21431642
    [34] 刘勇, 赵志军, 李才林, 等.川西高原杂谷脑河阶地的形成[J].地理学报, 2006, 61(3):249~254. doi: 10.11821/xb200603003

    LIU Yong, ZHAO Zhijun, LI Cailin, et al. Formation of the Zagunao river terraces in western Sichuan Plateau, China[J]. Acta Geographica Sinica, 2006, 61(3):249~254. (in Chinese with English abstract) doi: 10.11821/xb200603003
    [35] 韩建恩, 邵兆刚, 朱大岗, 等.黄河源区河流阶地特征及源区黄河的形成[J].中国地质, 2013, 40(5):1531~1541. http://d.g.wanfangdata.com.cn/Periodical_zgdizhi201305018.aspx

    HAN Jian'en, SHAO Zhaogang, ZHU Dagang, et al. Characteristics of river terraces and formation of the Yellow River in the source region of Yellow River[J]. Geology in China, 2013, 40(5):1531~1541. (in Chinese with English abstract) http://d.g.wanfangdata.com.cn/Periodical_zgdizhi201305018.aspx
    [36] 李海龙, 张岳桥, 李建华.青藏高原东缘南北向河流系统及其伴生古堰塞湖研究[J].第四纪研究, 2010, 30(4):812~824. http://www.docin.com/p-346264590.html

    LI Hailong, ZHANG Yueqiao, LI Jianhua. Meridional river systems and ancient dammed lakes on the east margin of the Tibetan Plateau[J]. Quaternary Sciences, 2010, 30(4):812~824. (in Chinese with English abstract) http://www.docin.com/p-346264590.html
    [37] 李吉均, 方小敏, 马海洲, 等.晚新生代黄河上游地貌演化与青藏高原隆起[J].中国科学(D辑), 1996, 26(4):316~322. https://www.cnki.com.cn/qikan-JDXK199604004.html

    LI Jijun, FANG Xiaomin, MA Haizhou, et al. Geomorphological and environmental evolution in the upper reaches of the Yellow River during the Late Cenozoic[J]. Science in China (Series D), 1996, 39(4):380~390. https://www.cnki.com.cn/qikan-JDXK199604004.html
    [38] 王书兵. 川西中部晚更新世地层与环境[D]. 北京: 中国地质科学院, 2005.

    WANG Shubing. Study on the strata and environment of the Late Pleistocene in the Central western Sichuan area[D]. Beijing:Chinese Academy of Geological Sciences, 2005.(in Chinese)
    [39] 沈玉昌, 龚国元.河流地貌学概论[M].北京:科学出版社, 1986.

    SHEN Yuchang, GONG Guoyuan. Outline of River Geomorphology[M]. Beijing:Science Press, 1986. (in Chinese)
    [40] Maddy D, Bridgland D, Westaway R. Uplift-driven valley incision and climate-controlled river terrace development in the Thames Valley, UK[J]. Quaternary International, 2001, 79(1):23~36. doi: 10.1016/S1040-6182(00)00120-8
  • 加载中
图(8) / 表(5)
计量
  • 文章访问数:  364
  • HTML全文浏览量:  139
  • PDF下载量:  32
  • 被引次数: 0
出版历程
  • 收稿日期:  2017-03-10
  • 刊出日期:  2017-12-01

目录

    /

    返回文章
    返回