库车—沙雅地区位于塔里木克拉通北部,近年来该地区地震具有频次不断增多、震级不断增大、时间间隔逐渐缩短的趋势.本文利用中国地震台网中心2017年1月—2022年12月震相走时和宽频带数据,通过重新定位、CAP(Cut And Paste)方法获得了库...库车—沙雅地区位于塔里木克拉通北部,近年来该地区地震具有频次不断增多、震级不断增大、时间间隔逐渐缩短的趋势.本文利用中国地震台网中心2017年1月—2022年12月震相走时和宽频带数据,通过重新定位、CAP(Cut And Paste)方法获得了库车—沙雅地区1257个精定位及84个震源机制解结果,同时利用区域应力场反演方法获得研究区应力场结果.结合区域地质构造背景、人工地震剖面等方面综合研究库车—沙雅地区的孕震特征与发震机理,确定发震断裂及其活动特征,获得以下认知:(1)研究区地震的空间分布与“X”型走滑断裂分布相一致.(2)研究区的震源机制解,主要以走滑为主,结合人工地震剖面,确定了库车—沙雅中小地震的发震断层为研究区奥陶—寒武系中的NNE、NNW向共轭走滑断裂体系,通过应力场反演获得了库车—沙雅地区NNW向的应力场分布格局,且具有较好的一致性.(3)最大地震库车M_(S)5.6地震节面Ⅰ走向77°,倾角90°,滑动角7°;节面Ⅱ走向347°,倾角83°,滑动角-180°,矩震级M_(W)5.16,矩心深度为8.0 km,推测此次地震的发震断层为本文编号为F_(Ⅱ)18走滑断层.本文结合多学科资料对库车—沙雅地区中小地震发震构造进行详尽探讨,并分析了该地区区域应力场特征,为该地区发震断层活动性及地震危险趋势提供一定参考依据.展开更多
The new Eu 3+ doped lanthanum oxysulfide phosphors,which have the orange-red long afterg low emission,were synthesized by solid-state reaction method.The synthesized phosphors were characterized by X-ray diffraction.T...The new Eu 3+ doped lanthanum oxysulfide phosphors,which have the orange-red long afterg low emission,were synthesized by solid-state reaction method.The synthesized phosphors were characterized by X-ray diffraction.The excitation and emission spectra,afterglow spectra and afterglow decay curves were examined.XRD confirm ed the phosphor as pure phase La 2 O 2 S.The phosphors showed typical transitions 5 D J (J=0,1) → 7 F J (J=0,1,2,3,4)of Eu 3+ .The photoluminescence spectra and afterglow spectra presented the regular alteration with various Eu 3+ concentration,due to cross relaxation between energy levels of Eu 3+ .In addition,we studied the effects of activator concentration and dopants species on the afterglow property.The data showed afterglow result was the bes t with2%Eu 3+ and doped with Mg 2+ and Zr 4+ .A prominent phosphorescence can be seen in this phosphor after illuminated with UV light.展开更多
文摘库车—沙雅地区位于塔里木克拉通北部,近年来该地区地震具有频次不断增多、震级不断增大、时间间隔逐渐缩短的趋势.本文利用中国地震台网中心2017年1月—2022年12月震相走时和宽频带数据,通过重新定位、CAP(Cut And Paste)方法获得了库车—沙雅地区1257个精定位及84个震源机制解结果,同时利用区域应力场反演方法获得研究区应力场结果.结合区域地质构造背景、人工地震剖面等方面综合研究库车—沙雅地区的孕震特征与发震机理,确定发震断裂及其活动特征,获得以下认知:(1)研究区地震的空间分布与“X”型走滑断裂分布相一致.(2)研究区的震源机制解,主要以走滑为主,结合人工地震剖面,确定了库车—沙雅中小地震的发震断层为研究区奥陶—寒武系中的NNE、NNW向共轭走滑断裂体系,通过应力场反演获得了库车—沙雅地区NNW向的应力场分布格局,且具有较好的一致性.(3)最大地震库车M_(S)5.6地震节面Ⅰ走向77°,倾角90°,滑动角7°;节面Ⅱ走向347°,倾角83°,滑动角-180°,矩震级M_(W)5.16,矩心深度为8.0 km,推测此次地震的发震断层为本文编号为F_(Ⅱ)18走滑断层.本文结合多学科资料对库车—沙雅地区中小地震发震构造进行详尽探讨,并分析了该地区区域应力场特征,为该地区发震断层活动性及地震危险趋势提供一定参考依据.
文摘The new Eu 3+ doped lanthanum oxysulfide phosphors,which have the orange-red long afterg low emission,were synthesized by solid-state reaction method.The synthesized phosphors were characterized by X-ray diffraction.The excitation and emission spectra,afterglow spectra and afterglow decay curves were examined.XRD confirm ed the phosphor as pure phase La 2 O 2 S.The phosphors showed typical transitions 5 D J (J=0,1) → 7 F J (J=0,1,2,3,4)of Eu 3+ .The photoluminescence spectra and afterglow spectra presented the regular alteration with various Eu 3+ concentration,due to cross relaxation between energy levels of Eu 3+ .In addition,we studied the effects of activator concentration and dopants species on the afterglow property.The data showed afterglow result was the bes t with2%Eu 3+ and doped with Mg 2+ and Zr 4+ .A prominent phosphorescence can be seen in this phosphor after illuminated with UV light.
