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???????????????????????????????????10 d????λ?á???????????????????????????????????С??2 m????????????????????С??8 ns????????????С??0.5 m/s??????????С???2.5 m?????????2006?????????????????????????????     

COMPASSα�൥�㶨λ���ȷ���

??????COMPASS???????????COMPASSα?????????????????????????????4GEO+5IGSO????????COMPASSα????λ???????????????COMPASSα???·??Ч???????????0??3 m???仯???侫???0.3??0.7 m??????????????·??Ч??????????С??GEO??????????·??Ч??????????????С??IGSO?????COMPASSα????λ?????RMS????N??E??U?????????3.33??3.45??8.84 m??     

GALILEO�걸��ϵͳ��XPL�㷨�о�

????XPL????Ч?????????HPL??VPL??????????????????м?????????????????????HPL??VPL??????????????HPL??VPL?????????С??9 m??12 m?????????12 m??20 m?????????????????????????????????????     

ALOS PALSAR�״�Ӱ��InSAR���ݴ����еĻ��ߺ͵���������

?????????????InSAR?????е????????????????????ζ??α??????????????????????????????????????о?????????????????ALOS PALSAR???????????????????α????????????????????????ALOS PALSAR?????????3??5 m???????е???????????￡??α?????????????????????о?????????????????С?????????????????????DEM?????????￡?SRTM DEM????????ALOS PALSAR??????????1cm???α???????????????????С??400 m??     

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????IGS???????????????1995??2010?????????????????????????????????λ?????????????????е??????????????????????????????SISRE??С??2 m??????????????(6??20)??10 ^-9 s???????λ????澫???1.0??7.0 m?????????2.5??27.0 m??     

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????1999??2001??2001??2004??2004??2007??????ε?GPS????????????????????????????(RELSM)?о???С????????????????ε???????????ó?С???????????????????????3.0~7.1 mm/a????????????????????????Σ????GPS??????棬?о???????????????????????????????????1??С???????????β?????ε???????????η???н?????????????????????????????????????2??RELSM?ó?С???????λ??????????????????????????ε???ε?????????????????С??3??С????????????????????????????θ????б??Σ?????μ???β?????????????????4??С?????????????????????????????????????????     

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???GPS??????????????????????????????????????????????????????????????????????????????????????????δ??10??30??50??100??????????????????????????δ???????????????????????????????С?????????????????С????Σ?С??????????Σ????????????????????Σ??????????????????С???????????????Σ?С????????????Σ?С????????????????κ????????????Ρ?     

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???????????????????????????????????????????????????????????????е???????????з?????????????????????????????????????????????????????????????5 km??????????????????????????????????С????????25 km??????????93?????????6 Hz?????????????е?????????С?????????????75 m???????????290 m??     

T/P,Jason��1�������ټ���Ч���ߵ���֤��Ƚ�

????T/P(TOPEX/POSEIDON)????????????????????????????????????T/P?????????????????????????????????????????????????????????У??????С????????????????????????????????????????????????????Ч??????T/P?????Ч???????0.3m??????T/P????????Jason??1?????????????????????????????????????????????????????????????????????????????????????????????????????á?T/P??Jason??1????????????????Ч?????????????????????????0.21 m??0.05 m??     

TRACK��ƵGPS��λ����ʱ�ο�վ��ѡȡ����

??????TRACK????????????λ????????????ο???????????GPS????????е?????????????????????????????????????????????????·??Ч?С??0.2 m???????????????????????????????????????ο??????????????λ?????????????????????GIPSY??PANDA????????????????????     

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????λ????8.0???????????, ??????????????????Χ?????????????????????????е???NW??SE??????????????????400 m?????????????????8.0???????????????п????????Χ??????????????????????????????????н???????ò?????????Χ?????????????3~4 Hz???????????????Χ??????????????????ε???????????200????????????Щ???????????????????????磬?????β???????????S???????λ?????????????????????????λ???????????????λ??????     

Trapping mechanism for long waves over circular islands with power function profiles

Long waves such as tsunamis can be trapped by islands due to wave refraction, and these trapped waves will cause huge damage even in the sheltered shoreline of the island. That all waves propagating into the topography and finally reaching the coastline are called perfect trapped modes, while any waves escaping from the topography are called leaky modes. Whether these long waves can be trapped is dependent on the depth profile of the island. This paper presents analytic solutions of the ray path for waves propagating into the circular island with power function profiles. Wave height distributions over the island are further investigated based on the principia that crowded rays correspond to large wave height and sparse rays correspond to small wave height. The trapped mechanism for water waves over the island is revealed based on their ray paths. Furthermore, the perfectly trapped criterion is derived, that is, when the slope gradient at the topography toe is greater than twice the ratio of the water depth to the radial distances, all wave rays propagating on the island will finally reach the coastline, and the waves are perfectly trapped.     

山东省沂水县下儒林钛铁矿矿床地质特征

下儒林钛铁矿位于沂沭断裂带内汞丹山凸起的东部边缘,浮来山白粉子断裂的西侧。含矿岩石(矿化体)为侵入于新太古代泰山岩群中的新太古代晚期含钛磁铁矿角闪石岩,其呈透镜状或带状发育于泰山岩群中或被捕虏(残留)于古元古代吕梁期傲徕山弱片麻状中粗粒二长花岗岩内,其产状与新太古代变质地层基本一致。矿区内圈定矿体5个,矿体长240~1000m,宽14~140m。矿石TFe含量一般为15%~16%,最高为21.84%,矿床平均为15.55%;TiO2含量一般为5%~8%,最高为10.13%,矿床平均为6.54%。矿石中TiO2与TFe含量变化呈正相关关系。     

可可西里北缘中新世火山活动带的基本特征

可可西里北缘火山活动带为可可西里中新世火山活动区数条火山活动带之一,其特征十分典型。本文以火山地质、同位素、岩石化学以及稀土元素地球化学为基础对其岩浆来源、演化、火山活动规律进行了研究。该火山带粗安岩-粗面岩-亚碱性流纹岩组合与世界高原溢流玄武岩类似,同时反映大陆伸展的构造环境。     

GPS�ⶨ���Ĵ�«ɽMw6.6����ͬ���α�

??????????????Χ??GPS??????????????з?????????t???????λ?????????α?????50 km??Χ????GPS????α???????????????????70 mm????????????30 s???????λ??????????????????α????????λ???????????У???С?????о???????????????29 km????????λ???21 mm????????150 km???λ???1??2 mm????GPS???????α????????????????????????????????????????????λ?????и???20 km????????廬?????0.6 m??GPS????????α??о????????????????????????????????ε?????????????????     

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?????????????????????????????α?????????????????????????????????????????????????????????????????ж?????б????????????ν????????1989??2000???λ???????????в????′??????????????3???????????????????仯??????????????????????С??????′????????????μ?????????????????????????α????????GPS??????????????????????????NW??????????????????????????????????????????п?????     

2021年阿拉斯加MW8.2地震震源破裂过程反演

基于GPS近场形变和远场P波,利用有限断层方法反演2021-07-29阿拉斯加M_W8.2地震的震源破裂过程。结果显示,此次地震持续时间约100 s,释放的地震矩约为1.59×10²¹ Nm。断层破裂滑移自震中沿断层向NEE延伸,震中东北侧的断层滑动量较大。基于GPS数据和位错理论模型分析地震的地表形变,同震形变整体上符合海沟特大地震的逆冲断层弹性回跳理论模式。受到断层闭锁的影响,太平洋板块俯冲北美板块,使得上盘北美板块受到长时间持续挤压,地震发生瞬间北美板块转变为拉张松弛状态。     

南北地震带北段南瑞现代地壳运动特征与地震

本文对南北地震带北段南端近十五年来大面积垂直形变观测资料及跨断层短水准观测资料进行了系统的分析处理。认为本地区七十年代以来以继承性构造运动为主。八十年代以来有加强的趋势;孕震区附近存在高梯度形变带,且高梯度带在断裂带附近发生偏转;形变速率等值线在其偏转处的切线几乎与断裂线正交。随着观测点的震中距及观测点与发震构造的位置关系不同,断层形变表现出不同的特征。另外,还对地壳形变与莫霍面深度及地壳应力场之间的关系作了初步分析。     

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