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贵州西南部威-紫-罗断裂带构造特征及演化

张荣强 周雁 汪新伟 李双建 李松

张荣强, 周雁, 汪新伟, 等, 2009. 贵州西南部威-紫-罗断裂带构造特征及演化. 地质力学学报, 15 (2): 178-189.
引用本文: 张荣强, 周雁, 汪新伟, 等, 2009. 贵州西南部威-紫-罗断裂带构造特征及演化. 地质力学学报, 15 (2): 178-189.
ZHANG Rong-qiang, ZHOU Yan, WANG Xin-wei, et al., 2009. STRUCTURAL FEATURES AND TECTONIC EVOLUTION OF THE WEI-ZI-LUO FAULT ZONE IN SOUTHWESTERN GUIZHOU PROVINCE. Journal of Geomechanics, 15 (2): 178-189.
Citation: ZHANG Rong-qiang, ZHOU Yan, WANG Xin-wei, et al., 2009. STRUCTURAL FEATURES AND TECTONIC EVOLUTION OF THE WEI-ZI-LUO FAULT ZONE IN SOUTHWESTERN GUIZHOU PROVINCE. Journal of Geomechanics, 15 (2): 178-189.

贵州西南部威-紫-罗断裂带构造特征及演化

基金项目: 

国家重大专项项目 2008ZX05005

石油化工联合基金项目 40739904

国际合作项目 2007DFR20440

详细信息
    作者简介:

    张荣强(1975-), 男, 工程师, 硕士, 从事石油地质、构造地质研究。E-mail:zhangrq@pepris.com

  • 中图分类号: P54

STRUCTURAL FEATURES AND TECTONIC EVOLUTION OF THE WEI-ZI-LUO FAULT ZONE IN SOUTHWESTERN GUIZHOU PROVINCE

  • 摘要: 威-紫-罗断裂带作为扬子板块南缘陆内较大的断裂, 控制着周围地区的盆地沉积及构造样式。本文通过野外地质勘查、平衡剖面技术及流体包裹体测温, 探讨了威-紫-罗断裂带的空间结构特征及构造演化历史。结果显示, NW-SE向威-紫-罗断裂带空间分段特征清楚, 运动性质以逆冲和左旋走滑活动为主。流体包裹体测温结果指示该断裂变形环境位于上地壳, 以脆性变形为主, 温度小于200 ℃。剖面复原结果显示, 断裂带在早泥盆世-中三叠世时期处于引张伸展构造背景下, 控制了断裂两侧沉积序列。断裂带挤压变形起始于中三叠世晚期的印支运动时期, 强烈变形发生在晚侏罗世早燕山运动时期, 与华南地块的向西挤压有关。

     

  • 图  1  威-紫-罗断裂带构造纲要图

    Figure  1.  Structure outline map of the Wei-Zi-Luo fault zone

    图  2  威-紫-罗断裂带空间结构分段示意图

    1.威宁-水城段; 2.小河边-关岭段; 3.紫云-罗甸段; 4.南丹断裂; 5.宜州断裂

    Figure  2.  Schematic map showing segmentation of the Wei-Zi-Luo fault zone

    图  3  贵州威宁-垭都实测构造剖面图(PM01)(剖面位置见图 1)

    1.泥岩;2.粉砂质泥岩;3.泥质粉砂岩;4.粉砂岩;5.钙质粉砂岩;6.长石砂岩;7.长石石英砂岩;8.含铁石英砂岩;9.石灰岩;10.砂质灰岩;11;白云质灰岩;12.条带状燧石灰岩;13.瘤状灰岩;14.泥灰岩;15.白云岩;16.灰质白云岩;17.逆断层;18.正断层

    Figure  3.  Structural section of Weining - Yadu, Guizhou Province (PM01) (see Fig.l for location)

    图  4  贵州关岭实测构造剖面图(PM02)(剖面位置见图 1)

    1.页岩;2.泥岩;3.粉砂质泥岩;4.泥质粉砂岩;5.粉砂岩;6.石灰岩;7.砂质灰岩;8.泥灰岩;9.白云岩;10.碎裂岩化带;11.角砾岩化带;12.节理化带;13.逆断层;14.正断层

    Figure  4.  Structural section of Guanling, Guizhou Province (PM02)

    图  5  贵州罗甸沫阳实测构造基干剖面(PM03)(剖面位置见图 1)

    1.泥岩; 2.粉砂质泥岩; 3.泥质粉砂岩; 4.粉砂岩; 5.石灰岩; 6.泥灰岩; 7.瘤状灰岩; 8.条带状燧石灰岩; 9.竹叶状灰岩; 10.硅质岩; 11.角砾岩化带; 12.逆断层; 13.正断层

    Figure  5.  Structural section of Luodian-Moyang, Guizhou Province (PM03)

    图  6  威-紫-罗断裂带断裂结构模式图

    1.角砾岩带; 2.碎裂岩化带; 3.节理破碎带; 4.方解石脉体带; 5.牵引褶皱带; 6.构造透镜体带; 7.劈理化带; 8.逆断层; 9.正断层; 10.地名

    Figure  6.  Block diagram of the Wei-Zi-Luo fault zone

    图  7  威紫罗断裂威宁-紫云段构造岩包裹体均一温度分布

    Figure  7.  Distribution of homogenized temperatures of fluid inclusions in the Weining-Ziyun section of Wei-Zi-Luo fault zone

    图  8  威紫罗断裂紫云-罗甸段构造岩包裹体均一温度分布

    Figure  8.  Distribution of homogenized temperatures of fluid inclusions in the Ziyun-Luodian segment of the Wei-Zi-Luo fault zone

    图  9  威紫罗断裂宜州-南丹段构造岩包裹体均一温度分布

    Figure  9.  Distribution of homogenized temperatures of fluid inclusions in the Yizhou-Nandan section of the Wei-Zi-Luo fault zone

    图  10  贞丰-镇宁构造剖面复原图

    Figure  10.  Restoration of the structural section of the line Zhenfeng-Zhenning

    表  1  威紫罗断裂带构造岩包裹体测试结果

    Table  1.   Result of fluid inclusion analysis in Wei-Zi-Luo fault zone

    表  2  贞丰-镇宁剖面伸长量统计表

    Table  2.   I, e, β statistics of line Zhenfeng-Zhenning

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  • 收稿日期:  2009-05-20
  • 刊出日期:  2009-06-01

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