首页|微动探测技术在连城岩溶塌陷的研究

微动探测技术在连城岩溶塌陷的研究

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在岩溶塌陷点开展观测台阵阵形对比和已知钻孔点的微动视S波波速测试试验,并进一步布设"十"字剖面开展研究区微动探测.试验和探测结果表明,观测台阵以嵌套式三重圆阵形为佳,但其高频段的频散谱能量集中度和连续性不如直线形台阵和L形台阵.庙前地区岩溶发育段石灰岩与砂土类地层接触带相对低速异常,及其石灰岩内视速度大致小于650 m/s,故判断该地区岩溶发育.通过建立地下空间速度性质的立体结构图,直观显示岩溶发育的空间形态,为准确探讨覆盖型岩溶/溶洞发育形成机制提供一定的依据.
Study on Microtremor Surver Technology in Karst Collapse in Liancheng County
Array comparison of observation stations at karst collapse sites and test of microtremor apparent S-wave velocity at known drilling points,then the cross-section is further arranged for the Microtremor Surver in the study area.Experimental studies and detection results show that,the triple-circle nested array is the best choice for the Microtremor observation array,but its high frequency band dispersion spectrum energy concentration and continuity is not as good as linear array and L-shaped array.In Miaoqian area the basic principle of judging karst development is the relatively low velocity anomaly in the contact between limestone and sandy soil,or the apparent velocity in limestone is less than 650 m/s.Therefore,it is judged that karst development in this area.Through the establishment of three-dimensional velocity structure map of underground space,the spatial morphology of karst development can be visualized,which provides a certain advantage basis for accurately discussing the mechanism of overlying karst/karst cave development.

microtremor surverkarst collapsearray contrastLiancheng County

温枝美

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福建省地质调查研究院,福州,350013

微动探测 岩溶塌陷 台阵对比 连城

2024

福建地质
福建省地质测绘院

福建地质

影响因子:0.304
ISSN:1001-3970
年,卷(期):2024.43(3)