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Characteristic Analysis of Anomalies of Strong Earthquakes along the Tancheng-Lujiang Fault Zone and Both Its Sides

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Earthquake Research in china 2015年第4期29卷 498-513页

作者： Li Jianyong Li Jie zhang Rui Li yu Han yufei Wang Tan National Earthquake Infrastructure Service State Key Laboratory of geodesy and Earth's Dynamics Institute of Geodesy and GeophysicsChinese Academy of Sciences Earthquake Administration of Shandong Province

This article made a systematic statistical analysis on the duration,spatial distribution,form,range,type and reliability of precursory anomalies based on the observations of precursors of 24 moderate-strong earthquakes occurring along the Tancheng-Lujiang fault zone and its bilateral areas in Shandong,Liaoning,Hebei,Jiangsu and Jiangxi Provinces in the period from 1966 to 2005. Results show that:( 1) For M7. 0 and M6. 0earthquakes,med-term abnormities are the greatest in number,short-term abnormities come second,and imminent anomalies are the least. For M5. 0 earthquakes,short-term abnormities are often the most in number,imminent anomalies come second,and the med-term ones are the least.( 2) Precursory anomalies are periodical,part of the med and short-term anomalies are shown as short-term and imminent anomalies during their development.( 3) The development of precursor shows quasi-synchronism; the closer to earthquake occurrence time,the more turning changes of anomalies will appear.( 4)Anomalies mainly occur within an epicenter distance of 100 km, showing a relative concentrated distribution in space,and the shorter the distance to epicenter,the higher the anomaly station / item rate.( 5) The spatial distribution of anomalies is relatively correlated to the strike of structures,having a good consistency with the structure.( 6)There is no significant correlation between duration of abnormities and the epicenter distance.( 7) The higher the magnitude of the earthquake,the greater the amplitude of the abnormities measured with the same observation approach.( 8) In terms of the itemsof the observations,fluid abnormities are the greatest in number,followed by deformation and electromagnetism observations.( 9) For all observation items,med and short-term abnormities make up the majority and short-term and imminent anomalies the minority.( 10) In fluid,deformation and electromagnetism observations,fairly reliable anomalies are about double the number of reliable anomal

关键词： Tancheng-Lujiang fault zone Characteristics of precursory anomaly Fluid anomaly Deformation anomaly Electromagnetic anomaly

Spatiotemporal characteristics, patterns, and causes of land-use changes in china since the late 1980s

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Journal of Geographical sciences 2014年第2期24卷 195-210页

作者： LIU Jiyuan KUANG Wenhui zhang Zengxiang XU Xinliang QIN yuanwei NING Jia ZHOU Wancun zhang Shuwen LI Rendong YAN Changzhe WU Shixin SHI Xuezheng JIANG Nan yu Dongsheng PAN Xianzhang CHI Wenfeng institute of Geographic sciences and Natural Resources Research CAS Beijing 100101 China institute of Remote Sensing and Digital Earth CAS Beijing 100101 China University of chinese academy of sciences Beijing 100049 China Chengdu institute of Mountain Hazards and Environment CAS Chengdu 610041 China Northeast institute of Geography and Agricultural Ecology CAS Changchun 130012 China wuhan institute of geodesy and geophysics CAS Wuhan 430077 China Cold and Arid Regions Environmental and Engineering Research institute CAS Lanzhou 730000 China Xinjiang institute of Ecology and Geography CAS Urumqi 830011 China institute of Soil Science CAS Nanjing 210008 China Nanjing institute of Geography and Limnology CAS Nanjing 210008 China

Land-use/land-cover changes （LUCCs） have links to both human and nature inter- actions. china＇s Land-Use/cover Datasets （CLUDs） were updated regularly at 5-year inter- vals from the late 1980s to 2.10, with standard procedures based on Landsat TM／ETM＋ im- ages. A land-use dynamic regionalization method was proposed to analyze major land-use conversions. The spatiotemporal characteristics, differences, and causes of land-use changes at a national scale were then examined. The main findings are summarized as fol- lows. Land-use changes （LUCs） across china indicated a significant variation in spatial and temporal characteristics in the last 20 years （1990-2.10）. The area of cropland change de- creased in the south and increased in the north, but the total area remained almost un- changed. The reclaimed cropland was shifted from the northeast to the northwest. The built-up lands expanded rapidly, were mainly distributed in the east, and gradually spread out to central and western china. Woodland decreased first, and then increased, but desert area was the opposite. Grassland continued decreasing. Different spatial patterns of LUC in china were found between the late 20th century and the early 21st century. The original 13 LUC zones were replaced by 15 units with changes of boundaries in some zones. The main spatial characteristics of these changes included （1） an accelerated expansion of built-up land in the Huang-Huai-Hai region, the southeastern coastal areas, the midstream area of the Yangtze River, and the Sichuan Basin; （2） shifted land reclamation in the north from northeast china and eastern Inner Mongolia to the oasis agricultural areas in northwest china; （3） continuous transformation from rain-fed farmlands in northeast china to paddy fields; and （4） effective- ness of the ＂Grain for Green＂ project in the southern agricultural-pastoral ecotones of Inner Mongolia, the Loess Plateau, and southwestern mountainous areas. In the last two decades, although climate

关键词： satellite remote sensing land-use change characteristics spatial pattern china

基于GNSS和InSAR约束的2021年玛多M_(S)7.4地震同震滑动分布及应用

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地球物理学报 2022年第2期65卷 509-522页

作者：余鹏飞熊维陈威乔学军王迪晋刘刚赵斌聂兆生李瑜赵利江张怀中国地震局地震研究所武汉430071 中国地震局地震大地测量重点实验室武汉430071 湖北省地震局武汉430071 中国地震局地球物理研究所北京100081 中国地震台网中心北京100045 青海省基础测绘院西宁810001

2021年5月22日青海省果洛藏族自治州玛多县发生M_(S)7.4地震,震中位于青藏高原中部的巴颜喀拉块体,这是近20多年来在巴颜喀拉块体周边发生8次M≥7级强震后,块体内部的一次强震,也是汶川地震以来中国大陆发生的最大一次地震,因此该地震... 详细信息

2021年5月22日青海省果洛藏族自治州玛多县发生M_(S)7.4地震,震中位于青藏高原中部的巴颜喀拉块体,这是近20多年来在巴颜喀拉块体周边发生8次M≥7级强震后,块体内部的一次强震,也是汶川地震以来中国大陆发生的最大一次地震,因此该地震的成因及周边地区未来的地震危险性值得重点关注.本文利用震后及时获取的39个近场流动GNSS观测,联合61个GNSS连续观测、Sentinel-1和ALOS-2 InSAR观测获取了本次地震精细的同震形变场,以此为约束,基于均匀弹性半无限位错模型,反演了发震断层的滑动分布,并计算了同震库仑应力变化.GNSS水平同震形变十分显著,断层南北两侧的GNSS点位,最大水平形变分别达0.7 m和-1.2 m,距震中200 km的测点仍有1 cm左右的同震形变.Sentinel-1和ALOS-2的升降轨InSAR同震形变场显示此次地震造成了约160 km长的地表破裂,最大视线向形变分别达0.9 m和1.2 m.同震滑动分布模型显示,发震断层由主段和次段组成,长度分别为170 km和20 km,主段倾向北,倾角85°,平均滑动角为-4.36°,表明玛多地震是一次典型的走滑型地震.次段倾向南,倾角68°,平均滑动角为-11.84°.地震破裂主要集中在0~15 km深度范围,最大滑动量为4.4 m,对应深度6.97 km.反演给出的矩震量为1.61×10^(20)N·m,对应矩震级M_(W)7.4.主发震断层上存在4个凹凸体,玛多地震是一次不对称双侧破裂事件.结合余震精定位、野外调查及地质资料,我们认为主发震断裂为昆仑山口—江错断裂,东部的次级破裂与主破裂机制不同.同震库仑应力结果显示,东昆仑断裂玛沁段应力有所增加(>0.01 MPa),处于应力加载状态,未来发生强震的危险性较高.

关键词： 2021玛多地震 GNSS InSAR 同震形变滑动分布

维普期刊数据库博看期刊

东昆仑断裂滑动速率变化及其对2.17年九寨沟地震的应力加载

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地球物理学报 2019年第3期62卷 912-922页

作者：李琦谭凯赵斌张彩红鲁小飞王东振余建胜中国地震局地震研究所中国地震局地震大地测量重点实验室武汉430071

为了解东昆仑断裂活动对2.17年8月8日九寨沟M_S7.0地震的影响,本文选取1999—2007年、2.13—2.17年GPS速度场作为约束,基于块体-位错模型反演计算东昆仑断裂两个时间段的块体运动速率、断裂滑动速率和滑动亏损率,并进一步研究青藏高原... 详细信息

为了解东昆仑断裂活动对2.17年8月8日九寨沟M_S7.0地震的影响,本文选取1999—2007年、2.13—2.17年GPS速度场作为约束,基于块体-位错模型反演计算东昆仑断裂两个时间段的块体运动速率、断裂滑动速率和滑动亏损率,并进一步研究青藏高原东缘最大剪应变率场和九寨沟震区的震间库仑应力累积速率.结果显示,东昆仑断裂中西段左旋走滑速率较高,东段走滑速率较低,自西向东逐步递减,存在明显的梯度.在两个时间段,阿坝块体刚性运动的方向顺时针偏转0.2°,运动速率由12.22mm·a^(-1)增大到15.96mm·a^(-1);东昆仑断裂左旋走滑速率升高,其中西段较为明显(升高约1.2±0.3mm·a^(-1));东昆仑断裂东段闭锁深度和闭锁程度增加;2.13—2.17年,东昆仑断裂滑动引起的九寨沟震区库仑应力累积速率是1999—2007年的3倍,最大剪应变率也明显升高.因此本文认为:2008年汶川地震和2.13年芦山地震后,龙门山断裂部分解锁,阿坝地块活动性增强,东昆仑断裂滑动速率增大,导致九寨沟震区库仑应力加载速率增加,加速了九寨沟地震的孕育过程.

关键词：九寨沟地震东昆仑断裂滑动速率震间库仑应力累积速率