摘要
在深入剖析新疆新04井(泉)水文地质构造背景的基础上,探讨了新04井(泉)流体测项长程趋势变化与区域地震活动性、气温等物理场的相关性。新04井(泉)流体测项长程趋势变化是由于区域应力场增强与浅层水渗入量增加共同作用的结果。
Based on analyzing hydrogeology tectonic background of new No. 4 well （spring） of Urumql, Xinjiang, the article discusses the relation between long-distance trendy change of fluid items of new No. 04 well and regional seismicity and physical field of temperature etc.. Long-distance trendy change of fluid items of new No. 04 well results from strengthening of regional stress field and increasing of penetrating flux of shallow-layer water.
出处
《内陆地震》
2006年第1期81-87,共7页
Inland Earthquake
基金
国家自然科学基金(140374019)
地震科学联合基金(1040106)联合资助
关键词
流体测项
趋势变化
日长增量变化
区域应力场
区域地震活动
Fluid items
Trendy change
Daily-increment change
Regional stress field
Re gional seismicity
