右江地区新生代断裂活动及构造变形机制的物理模拟分析

聂冠军; 于红梅; 何声; 李冰溯; 潘黎黎

doi:10.12090/j.issn.1006-6616.2020.26.03.029

右江地区新生代断裂活动及构造变形机制的物理模拟分析

doi: 10.12090/j.issn.1006-6616.2020.26.03.029

聂冠军^{1, 2,},
于红梅³,
何声^{1, 2},
李冰溯^{1, 2},
潘黎黎^{1, 2}

1.
广西壮族自治区地震局, 广西南宁 530022
2.
广西工程防震研究院, 广西南宁 530022
3.
中国地震局地质研究所, 北京 100029

基金项目:

中国地震局地震科技星火计划项目 XH19033Y

广西重点研发计划 AB1850042

广西重点研发计划 AB18126040

详细信息

作者简介:
聂冠军(1987-), 男, 博士, 高级工程师, 主要从事构造地质学专业研究。E-mail:120279026@qq.com

中图分类号: P542
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- 被引次数: 0
出版历程
- 收稿日期: 2019-05-10
- 修回日期: 2020-01-20
- 刊出日期: 2020-06-30

Physical simulation analysis of the Cenozoic fault activities and structural deformation mechanism of the Youjiang area

NIE Guanjun^{1, 2
,},
YU Hongmei³,
HE Sheng^{1, 2},
LI Bingsu^{1, 2},
PAN Lili^{1, 2}

1.
Earthquake Administration of Guangxi Zhuang Autonomous Region, Nanning 530022, Guangxi, China
2.
Guangxi academy of engineering shock prevention, Nanning 530022, Guangxi, China
3.
Institute of Geology, China Earthquake Administration, Beijing 100029, China

摘要

摘要: 右江地区北西向断裂起源于晚古生代右江盆地内发育的同沉积断裂，这些断裂近等间距平行分布，新生代以来发生了多期次左旋走滑活动，进而导致了右江地区整体发生简单剪切变形。利用三维沙箱模型展开了物理模拟实验，对新生代右江地区的变形机制进行了分析。实验结果表明，早期在红河断裂的左旋剪切错动和印支地块的顺时针旋转联合作用下，右江地区北西向断裂复活，并发生明显的左旋走滑活动；随后川滇地块发生东南向的挤出运动，对右江地区产生侧向挤压，导致了右江地区北西向断裂新一轮的快速左旋走滑活动，同时还导致了右江地区西部的地壳压缩增厚。实验证实新生代右江地区的简单剪切变形以及北西向断裂的走滑活动是印支地块和川滇地块挤出运动共同作用的结果，同时也是印度-欧亚板块碰撞产生的连锁反应之一。
- 右江地区 /
- 走滑断裂 /
- 变形机制 /
- 地块 /
- 物理模拟
Abstract: The NW-trending faults in the Youjiang area originated from synsedimentary faults developed in the Youjiang Basin of Late Paleozoic. In Cenozoic these equidistantly spaced faults have undergone multiple left-lateral strike-slip activities,which then led to a simple-shear deformation of the Youjiang area. A 3-D sandbox model is designed to study the deformation mechanism of the Youjiang area. The experimental results show that the NW-trending faults were reactivated and a strikingly left-lateral strike slip occurred under the left-lateral movement and the clockwise rotation of the Indochina block. And then the lateral compression of the Sichuan-Yunnan block resulted in a new round of fast left-lateral strike-slip of the NW-trending faults in the Youjiang area,and it also resulted in crustal compression and thickening in the western part of the Youjiang area. Both the left-lateral strike-slip activities of the NW-trending faults and the simple-shear deformation occurred in the Youjiang area in Cenozoic were driven by the extrusion of the Indochina Block and the Sichuan-Yunnan Block,and they can be viewed as one of the consequences of the India-Eurasia collision.
- Youjiang area /
- strike-slip fault /
- deformation mechanism /
- block /
- physical simulation
注释:

责任编辑：范二平

HTML全文

图 1 右江地区及邻区的断裂分布、大地构造、活动地块和变形模式图

a-右江地区断裂分布图；b-右江地区及邻区大地构造简图(据任纪舜，2003修改)；c-右江地区周边活动地块分布图；d-右江地区简单剪切变形模式图

Figure 1. Faults distribution, geotectonics, active blocks and deformation pattern in the Youjiang area and its adjacent areas

下载: 全尺寸图片幻灯片

图 2 右江盆地构造演化示意图(据杜远生等，2009修改)

Figure 2. Tectonic evolution of the Youjiang Basin (modified after Du et al., 2009)

下载: 全尺寸图片幻灯片

图 3 右江地区北西向断裂的野外出露照片和卫星影像图

Figure 3. Photos and satellite images of the NW faults in the Youjiang area

下载: 全尺寸图片幻灯片

图 4 北西向断裂的卫星影像图

a-巴马-博白断裂左旋错移燕山晚期花岗岩岩体；b-靖西-崇左断裂左旋错移北东向山脊；c-那坡断裂的尾部垂向拉张；d-文山断裂左旋错移不同时代地层

Figure 4. Satellite images of the NW faults

下载: 全尺寸图片幻灯片

图 5 2005年文山5.3级地震房屋墙体破坏照片及其断层剖面图

Figure 5. Failure of the building wall in Wenshan M_S5.3 earthquake in 2005 and its fault profile

下载: 全尺寸图片幻灯片

图 6 模型设置示意图

a-模型横切面示意图；b-模型正面示意图

Figure 6. Schematic diagram of the model setting

下载: 全尺寸图片幻灯片

图 7 两个阶段不同加载时期的实验结果照片

a-第一阶段A中期；b-第一阶段A末期；c-第二阶段中期；d-第二阶段末期

Figure 7. Photos of experimental results of different loading stages in two phases

下载: 全尺寸图片幻灯片

图 8 两个阶段各断裂的相对错移量和绝对错移量

实线为拟合曲线
a-第一阶段A各断裂的相对错移量；b-第二阶段各断裂的相对错移量；c-第一阶段A和第二阶段各断裂的绝对错移量

Figure 8. Relative and absolute displacements of the faults in two phases

下载: 全尺寸图片幻灯片

表 1 北西向断裂伴生盆地统计表(聂冠军等，2019)

Table 1. Accompanying basins of the NW faults(Nie et al., 2019)

断裂名称	断裂伴生盆地	盆地类型	盆地开启年代
巴马-博白断裂	宾阳盆地	半地堑式断陷盆地	第四纪
右江断裂	永乐盆地	拉分盆地	始新世
	百色盆地	拉分盆地	始新世
	隆安盆地	拉分盆地	始新世
	南宁盆地	尾张型拉张盆地	始新世
靖西-崇左断裂	宁明盆地	半地堑式断陷盆地	渐新世
	海渊盆地	半地堑式断陷盆地	渐新世
	上思盆地	半地堑式断陷盆地	渐新世
	广南盆地	拉分盆地	中新世
那坡断裂	Caobang basin	拉分盆地	中新世
	Thatkhe basin	拉分盆地	中新世
	Naduong basin	拉分盆地	中新世
	Tien Yen Bay	尾张型拉张盆地	-
文山断裂	文山盆地	拉分盆地	始新世

下载: 导出CSV

表 2 各实验阶段的加载参数设置

Table 2. Parameter setting for the loading in different experimental stages

实验阶段	加载方式	加载速率/(mm/s)	移动量/cm
第一阶段A	在模型下侧边界施加带顺时针旋转的左旋剪切	0.05	20
第一阶段B	在模型的下侧边界施加单侧左旋剪切	0.05	20
第二阶段	在模型的左侧下方施加向右的挤压	0.01	2

下载: 导出CSV

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