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辽西义县地区黄花山角砾岩研究的新进展 被引量:6
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作者 张宏 杨芳林 +6 位作者 张立君 李之彤 王五力 马兵 孙武国 郑少林 郑月娟 《地球学报》 EI CAS CSCD 北大核心 2004年第3期321-326,共6页
对辽西地区黄花山角砾岩层的研究表明 ,黄花山角砾岩是一套火山碎屑岩 火山碎屑沉积岩类。黄花山角砾岩的形成大致可分为 2个阶段 :早期阶段以火山熔岩溢流和剧烈的火山爆发作用为主 ,不同地区形成了火山角砾岩 (火山碎屑岩 )或火山熔... 对辽西地区黄花山角砾岩层的研究表明 ,黄花山角砾岩是一套火山碎屑岩 火山碎屑沉积岩类。黄花山角砾岩的形成大致可分为 2个阶段 :早期阶段以火山熔岩溢流和剧烈的火山爆发作用为主 ,不同地区形成了火山角砾岩 (火山碎屑岩 )或火山熔岩 ;晚期阶段 ,黄花山角砾岩成层性较好 ,以厚 中层为主 ,并且向上部韵律逐渐发育 ,表明这个时期渐变为以沉积作用为主 ,形成了火山碎屑沉积岩。黄花山角砾岩层和义县晚期的酸性火山熔岩同是义县组的顶部层位 ,二者为同时异相关系(但不是过渡关系 )。黄花山角砾岩层的定位对正确认识义县组以及研究阜新 义县盆地的演化史有着重要意义。 展开更多
关键词 角砾岩 时异相关系 岩层定位 构造演化
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A Discussion on the Abnormal Tidal Phase Relationship between Water Level and Water Temperature in Qixian Well
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作者 Ma Yuchuan Wang Bo Wang Yan 《Earthquake Research in China》 2014年第3期350-359,共10页
Tidal phase of water temperature in Qixian well,Shanxi Province is ahead of water level,which is different from the normal tidal relationship between water temperature and water level. Observation curves of this pheno... Tidal phase of water temperature in Qixian well,Shanxi Province is ahead of water level,which is different from the normal tidal relationship between water temperature and water level. Observation curves of this phenomenon are introduced in this paper,and co-seismic response data of water temperature and water level are used to check the thermometer time system,confirming that this phenomenon is true. Using the harmonic analysis method,variations of time difference between water temperature and water level for the M2 wave are worked out,which indicates that this phenomenon exists during the whole observation. According to the variations of phase lags for water temperature and water level,and the survey of observation conditions, it is considered that the abnormal phenomenon may be related to inadequate passage of water caused by a well blockage at the depth where the water temperature probe was set. 展开更多
关键词 Water level Water temperature Earth tide Co-seismic
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