首页|藏东贡觉地区地应力场分布特征及影响因素研究

藏东贡觉地区地应力场分布特征及影响因素研究

扫码查看
藏东贡觉地区位于金沙江断裂带北段,经历了复杂的地质构造演化.本文基于水压致裂法地应力实测数据,通过计算评价主应力量值、侧压力系数、主应力方位及构造应力等地应力特征参数,分析了贡觉地区现今地应力场分布规律及其影响因素.结果表明:藏东贡觉地区实测主应力随深度增加而增大,浅部(<500 m)数据较为离散,深部(>500 m)数据呈线性分布,表现为Sv>SH>Sh,水平主应力随深度变化梯度低于背景地块相应梯度水平;实测最大水平主应力优势方位为NNE向,与区域应力场优势方位NE—NEE向呈现逆时针偏转;通过对研究区侧压力系数、水平应力比、剪应力相对大小(μm)以及Sheorey模型分析得出,研究区水平构造应力积累程度和活动程度均较低,区内字嘎寺—德钦断层处于稳定状态.研究区地应力场影响因素主要为重力作用、地形特征以及构造作用.岩体自重对地应力的影响主要遵循静水压力规律;地形地貌的影响主要体现为浅部(<500 m)水平向主应力值较离散,在深切峡谷区侧压力系数由谷底至坡顶逐渐减小;构造作用对研究区地应力场的影响主要集中在字嘎寺—德钦断层两侧一定范围内,表现为局部地应力场的主应力方位偏转及主应力量值异常.研究结果可为藏东贡觉地区及类似地质环境区域稳定性评价以及地下工程选址建设提供理论依据.
Study on distribution characteristics and influencing factors of in-situ stress field in Gonjo region of eastern Tibet
Gonjo region of eastern Tibet which is located in the northern section of Jinshajiang fault zone has undergone complex geological tectonic evolution.The distribution and influencing factors of in-situ stress field are discussed through the characteristic parameters analysis of the main stress value and orientation,lateral pressure coefficients,tectonic stress value based on the measured data of in-situ geostress using hydraulic fracturing method.The results show that the measured main stress increases with depth.The stress are scattered at the depth less than 500 m but manifested as Sv>SH>Sh in linear at the depth more than 500 m.The gradient of horizontal main stress versus depth is lower than that of the regional background blocks.The regional dominant orientation of maximum horizontal principal stress is NNE,which shows a counterclockwise deflection comparing with the dominant NE-NEE regional tectonic stress direction derived from other tectonic stress indicators.Based on the analysis of lateral pressure coefficients,horizontal stress ratio,ratio of maximum shear stress and average horizontal stress(μm)and Sheorey model,it is indicates that the horizontal tectonic stress accumulation is in the low level and the Zigasi—Deqin fault is stable in this region.The influencing factors of the in-situ stress field mainly include gravity,topography and tectonic action.The influence of gravity action on geostress follows the law of hydrostatic pressure.Under the influence of topography the horizontal geostress is discrete in superficial crust(<500 m)and the lateral pressure coefficient decreases from bottom to the top of slope in deep-cutting gorge.The tectonic action mainly concentrates on the range of Zigasi—Deqin fault on both sides,where the values and directions of the main stress are abnormal in local area.It is expected to provide theoretical basis for regional stability evaluation,site selection and construction of underground engineering.

Gonjo regionIn-situ stress fieldDistribution characteristicsTopography characteristicsTectonic stress

廖昕、吕改杰、陈仕阔、王虎、赵晓彦、黄涛

展开 >

西南交通大学地球科学与环境工程学院,成都 611756

四川省环青藏高原交通廊道地质灾害生态化防治工程技术研究中心,成都 611756

中国铁路设计集团有限公司,天津 300142

贡觉地区 地应力场 分布特征 地形特征 构造应力

四川省重点研发项目四川省自然科学基金青年学者项目西南交通大学地质工程与测绘工程创新实践基地

2022YFWZ00092022NSFSC1117YJG-2022-JD04

2024

地球物理学进展
中国科学院地质与地球物理研究所 中国地球物理学会

地球物理学进展

CSTPCD北大核心
影响因子:1.761
ISSN:1004-2903
年,卷(期):2024.39(3)