地震
地震
지진
EARTHQUAKE
2001年
1期
39-46
,共8页
杨志荣%田兆%安景生%张宏科%陶茂松
楊誌榮%田兆%安景生%張宏科%陶茂鬆
양지영%전조%안경생%장굉과%도무송
蓄水后形变异常%诱发水库地震预测%新疆克孜尔水库
蓄水後形變異常%誘髮水庫地震預測%新疆剋孜爾水庫
축수후형변이상%유발수고지진예측%신강극자이수고
应用库区多项形变观测资料,对克孜尔水库蓄水后出现的形变异常及诱发水库地震的危险性进行了研究。结果认为:①穿过水库大坝的F2活断层在蓄水后出现水平和垂直形变的特大异常变化主要是前期水库施工开挖土石方、填筑土石方及水库蓄水引起地面负荷变化的综合效应所致;②克孜尔水库虽然存在诱发水库地震的潜在因素,但从库容、坝高、F2活断层产状、地质构造背景、水文地质条件、岩性以及世界各国发生水库诱发地震的成因、特点等多方面综合分析表明,克孜尔水库不具备发生水库诱发地震的充分条件;③由库区各项形变观测资料分析表明,库区地壳形变已由施工-蓄水初期时的反向异常变化恢复到了施工蓄水前的正常变化状态,各种受力因素经过调整达到了新的平衡,已进入相对稳定的继承性运动期,因此今后因蓄水诱发水库地震的可能性不大。
應用庫區多項形變觀測資料,對剋孜爾水庫蓄水後齣現的形變異常及誘髮水庫地震的危險性進行瞭研究。結果認為:①穿過水庫大壩的F2活斷層在蓄水後齣現水平和垂直形變的特大異常變化主要是前期水庫施工開挖土石方、填築土石方及水庫蓄水引起地麵負荷變化的綜閤效應所緻;②剋孜爾水庫雖然存在誘髮水庫地震的潛在因素,但從庫容、壩高、F2活斷層產狀、地質構造揹景、水文地質條件、巖性以及世界各國髮生水庫誘髮地震的成因、特點等多方麵綜閤分析錶明,剋孜爾水庫不具備髮生水庫誘髮地震的充分條件;③由庫區各項形變觀測資料分析錶明,庫區地殼形變已由施工-蓄水初期時的反嚮異常變化恢複到瞭施工蓄水前的正常變化狀態,各種受力因素經過調整達到瞭新的平衡,已進入相對穩定的繼承性運動期,因此今後因蓄水誘髮水庫地震的可能性不大。
응용고구다항형변관측자료,대극자이수고축수후출현적형변이상급유발수고지진적위험성진행료연구。결과인위:①천과수고대패적F2활단층재축수후출현수평화수직형변적특대이상변화주요시전기수고시공개알토석방、전축토석방급수고축수인기지면부하변화적종합효응소치;②극자이수고수연존재유발수고지진적잠재인소,단종고용、패고、F2활단층산상、지질구조배경、수문지질조건、암성이급세계각국발생수고유발지진적성인、특점등다방면종합분석표명,극자이수고불구비발생수고유발지진적충분조건;③유고구각항형변관측자료분석표명,고구지각형변이유시공-축수초기시적반향이상변화회복도료시공축수전적정상변화상태,각충수력인소경과조정체도료신적평형,이진입상대은정적계승성운동기,인차금후인축수유발수고지진적가능성불대。
After the Kizil Reservoir in Xinjiang Region stored water, the horizontal andvertical deformation appeared in the reservoir area. According to the references, the seismicrisk induced by the reservoir was studied by using multi-item deformation data. The resultshows: ① Active fault F2, crossing the reservoir area, deformed largely after the reservoir wasstored water. It is thought that the changing of the load on the ground caused the deforma-tion. ② Although there is potential factor inducing earthquakes in the Kizil reservoir area, thePrecent condition of the reservoir water storage, dam height, fault F2 occurrence, geologicaltectonic background, hydrogeological condition, and the property of rocks could not induce areservoir earthquake. ③ Because the crustal deformation now has recovered to normal statefrom the opposite anomaly in the period of construction and initial water storage, and everykind of force-affected factors have reached a new balance, the probability to induce a reser-voir earthquake is less in the future.