高原地震
高原地震
고원지진
EARTHQUAKE RESEARCH IN PLATEAU
2011年
4期
10-12
,共3页
张立%赵洪声%苏有锦%赵小艳
張立%趙洪聲%囌有錦%趙小豔
장립%조홍성%소유금%조소염
年度预测%地下水位%年变化率%指标观测井%强震预测指标
年度預測%地下水位%年變化率%指標觀測井%彊震預測指標
년도예측%지하수위%년변화솔%지표관측정%강진예측지표
Annual forecast%Underground water level%Annual changing rate%Index well%Index of strong earthquakes forecasting
为进行强震的年度预测,采取年变化率做为水位变化参量,大于或小于一定的年变化率值即为强震异常。在研究多年的强震前地下水位异常震例的基础上,在云南3个地震区分别确定了指标观测井及其强震的预测指标:丽江地震区选择丽江井,水位异常判定指标为年变化率R临≤-1.10;楚雄地震区为大姚井,指标是R临≥0.03;滇西南地震区为双江井,指标是R临≤-0.30。分区建立的预测指标对于强震的时空强三要素可做出一定程度的预测。这些研究结果可在今后的预测实践中检验与修正。
為進行彊震的年度預測,採取年變化率做為水位變化參量,大于或小于一定的年變化率值即為彊震異常。在研究多年的彊震前地下水位異常震例的基礎上,在雲南3箇地震區分彆確定瞭指標觀測井及其彊震的預測指標:麗江地震區選擇麗江井,水位異常判定指標為年變化率R臨≤-1.10;楚雄地震區為大姚井,指標是R臨≥0.03;滇西南地震區為雙江井,指標是R臨≤-0.30。分區建立的預測指標對于彊震的時空彊三要素可做齣一定程度的預測。這些研究結果可在今後的預測實踐中檢驗與脩正。
위진행강진적년도예측,채취년변화솔주위수위변화삼량,대우혹소우일정적년변화솔치즉위강진이상。재연구다년적강진전지하수위이상진례적기출상,재운남3개지진구분별학정료지표관측정급기강진적예측지표:려강지진구선택려강정,수위이상판정지표위년변화솔R림≤-1.10;초웅지진구위대요정,지표시R림≥0.03;전서남지진구위쌍강정,지표시R림≤-0.30。분구건립적예측지표대우강진적시공강삼요소가주출일정정도적예측。저사연구결과가재금후적예측실천중검험여수정。
In order to do better in the annual strong earthquake forecast, the authors consider that the annual changing rate higher or lower than certain value is anomaly before strong earthquakes by using the annual changing rate as changing before some strong confirmed in three parameter of water-level. Based on the analysis of many years water level anomalies earthquakes, the index of water-level wells and strong earthquake forecasting have been seismic zones of Yunnan area: in Lijiang earthquake zone, the index well is Lijiang Well and the index of water-level anomaly is the annual changing rate R临≤ - 1.10 ; in Chuxiong earthquake zone, it is Dayao Well and the index is R临≥ 30. 03 ; in southwest Yunnan, Shuangjiang Well has been chosen and the index is R临≤ - 0. 30. The subarea indexes can do certain forecasting of the earthquakes' space-time-magnitude, so these results should be tested and modified in the forecasting practice in the future.