浙赣交界地区上奥陶统红家坞组(O3h)   总被引：2，自引：0，他引：2  

汪隆武  许红根  齐岩辛  唐增才  俞国华 《地层学杂志》2004,28(1):52-55,58

红家坞组为 1/ 5万《球川镇幅》和《常山县幅》新建岩石地层单位。本组分布于浙皖盆地东南缘 ,系指江山、常山、玉山地区 (简称为“三山”地区 )出露的一套杂色砂岩—泥岩组合 ,层位与文昌组灰绿色砂岩、粉砂岩相当 ,在岩性、岩相上又与之有明显区别的海相红层 ,厚度 380— 4 83m ,典型剖面位于浙江省江山市大桥镇仕阳尾行政村红家坞村。该组的建立 ,丰富了浙赣“三山”地区岩石地层资料。  相似文献   

深基坑开挖对坑内基桩受力特性的影响分析   总被引：6，自引：1，他引：5  

胡琦  凌道盛  陈云敏  程泽海  冉龙 《岩土力学》2008,29(7):1965-1970

基坑开挖对基桩产生一定的侧摩阻力,如果处理不当,将危及地下结构与基桩的安全使用,同时也给基桩承载力与刚度的确定带来困难。根据应力路径与应力水平对土体刚度的影响,建立了受深基坑开挖影响的桩土界面荷载传递模型,通过应力路径试验确定了界面摩擦特性参数。对不同开挖深度的影响分析,得出了基坑开挖对桩周侧摩阻力的分布、基桩刚度与承载力的影响。分析结果表明,采用覆土条件下的基桩承载力与刚度值是偏于不安全的。  相似文献   

Preliminary stratigraphic and structural architecture of Bhutan: Implications for the along strike architecture of the Himalayan system   总被引：5，自引：0，他引：5  

Nadine McQuarrie  Delores Robinson  Sean Long  Tobgay Tobgay  Djordje Grujic  George Gehrels  Mihai Ducea 《Earth and Planetary Science Letters》2008,272(1-2):105-117

High-precision in-situ ion microprobe (SIMS) oxygen isotope analysis of zircons from two diorite intrusions associated with the late Caledonian Lochnagar pluton in Scotland has revealed large differences in the degree of heterogeneity in zircon δ¹⁸O between the diorites. Zircon crystals from the Cul nan Gad diorite (CnG) show a unimodal distribution of oxygen isotope values (δ¹⁸O = 6.0 ± 0.6‰ (2σ)) and no or only minor grain-scale variation. Those from the Allt Darrarie diorite (AD1) show a large range in δ¹⁸O and an apparent bimodal distribution with modes of 6.6 ± 0.4‰ and 7.3 ± 0.4‰. Variations of up to 1.2‰ occur between and within grains; both an increase and decrease in δ¹⁸O with zircon growth has been observed. The δ¹⁸O composition of growing zircon can only change if open-system processes affect the magma composition, i.e. if material of contrasting δ¹⁸O composition is added to the magma. The variability in AD1 is interpreted to represent a cryptic record of magma mixing. A ‘deep crustal hot zone’ is a likely site for generation of the dioritic magmas which developed by mixing of residual melts and crustal partial melts or by melting of mafic lower crustal rocks. The overall small number of zircons with mantle-like δ¹⁸O values (5.3 ± 0.6‰ (2σ)) in the Lochnagar diorites is largely the product of crustal differentiation rather than crustal growth.

The δ¹⁸O of quartz from the CnG and AD1 diorites shows only minor variation (CnG: 10.9 ± 0.5‰ (2σ), AD1: 11.7 ± 0.6‰ (2σ)) within single populations, with no evidence of mixing. Quartz–zircon isotopic disequilibrium is consistent with later crystallisation of quartz from late magmatic fluids, and in case of the AD1 diorite after the inferred magma mixing from a homogenised, higher δ¹⁸O melt.

High-precision SIMS oxygen isotope analysis of zircon provides a new approach to identifying and resolving previously undetected early-stage magma mixing and constraining the compositions and origins of the component magmas. A combination of zircon, quartz and whole-rock data has proven to be a powerful tool in reconstructing the petrogenetic evolution of diorite from early crystallisation to late alteration.  相似文献   

北天山地区中强地震震源机制解分析   总被引：3，自引：1，他引：2  

龙海英  高国英  聂晓红  李莹甄 《中国地震》2008,24(1):23-30

利用北天山地区历史上24次中强地震震源机制解,进行系统聚类及应力场反演分析.结果表明,北天山地区中强地震震源断错性质主要以倾滑逆断层为主.多数地震的主破裂面为NW向.与其附近地震构造走向基本一致.主压应力P轴方位近NS向,倾角较小;主张应力T轴倾角较大,显示出区域应力场主要受近NS向水平挤压作用.最大主应力方向从东到西呈现出NNE-Ns-NW的渐变过程.  相似文献   

基于TC35T模块在无人值守地震台站遥控电源开关的应用   总被引：1，自引：1，他引：0  

张茂军  张晋川  袁燕妮  龙文智  曾新元 《地震地磁观测与研究》2008,29(1):89-94

雷击是造成地震台站观测仪器损坏、影响观测数据连续率和可靠性的重要因素。基于应用TC35T手机模块的遥控电源开关可实现对市电电源遥控“拉闸”和开启,以起到对无人地震监测点的防雷作用。介绍了TC35T模块的应用工作方式,遥控电源开关的硬件组成、程序设计思路,以及该遥控装置在无人值守台站四川攀枝花川-05井水化观测站的应用情况。认为,该遥控装置对地震台站,特别是无人值守台站的地震观测仪器,及其他领域带电工作的仪器设备免遭雷击,减少损失,提高运转连续率和工作质量,具有较高的实用价值和推广前景。  相似文献   

龙滩水电工程数字遥测地震台网监测能力检验   总被引：12，自引：5，他引：7  

姚宏  陈鑫  黄树生  龙政强 《地震地磁观测与研究》2008,29(4):62-66

阐述了数字地震台网地震监测能力的计算方法,根据龙滩数字遥测地震台网监测要求与设计监测能力,采用该台网2006年1月至2007年11月期间记录到的833个ME1．5以下地震,检验和分析了台网的实际监测能力,结果表明,台网的实际监测能力达到设计要求。  相似文献   

四川盆地西北部新生代构造变形模式讨论——对认识青藏高原东北缘新生代变形机制的意义     

罗良  贾东  李海滨  邓飞  李一泉  武龙 《高校地质学报》2008,14(4):593-600

综合造山带内的构造热年代学及盆地内部进行的磷灰石裂变径迹研究,提出了四川盆地西北部的三个背斜（潼梓关背斜、九龙山背斜和南阳坝背斜）主要是新生代构造变形的产物。野外观察发现汉中盆地是一个第四纪的拉分盆地,其主控断层具左行走滑性质。新生代青藏高原东缘大型地块向东挤出,遭遇强硬的四川克拉通阻挡之后,沿着龙门山形成了一个右行的走滑挤压带,并且影响到邻近的四川盆地,形成北东向背斜。这期构造变形往北延伸进入米仓山,形成具有逆冲性质的北东向断层。四川盆地北面也存在向东的挤出作用,这和汉中盆地主控断层的左行走滑性质是匹配的。四川盆地北面的地块挤出影响了米仓山前缘的四川盆地,由于龙门山和米仓山构造变形的叠加,使得最东面的南阳坝背斜相对于其它两个背斜在褶皱轴上发生了偏转。  相似文献   

不同实验条件下GPS伪距定位精度分析     

原洪峰  杨龙  蒋德 《全球定位系统》2005,30(5):23-26

研究概括了在不同的实验条件下利用GPS伪距获得较高精度定位结果的方法。实验结果的精度表明,这些方法的定位结果都能比常规的GPS伪距定位法的结果精度高,而且定位效果稳定。同时该方法也可为后续高精度定位及定轨等研究工作打好基础。  相似文献   

A full-scale field experiment to study the thermal-deformation process of widening highway embankments in permafrost regions     

ShuangJie Wang  Long Jin  Kun Yuan  DongGen Chen  JinPing Li  Yi Song 《寒旱区科学》2021,13(2):123-132

As one of the widely used upgrading way in road engineering, the widening embankment(WE) has suffered evident differential deformation, which is even severer for highway in permafrost regions due to the temperature sensitivity of frozen soil and the heat absorption effect of the asphalt pavement. Given this issue, a full-scale experimental highway of WE was performed along the Qinghai-Tibet Highway(QTH) to investigate the differential deformation features and its developing law. The continuous three years' monitoring data taken from the experimental site, including the ground temperature and the layered deformation of WE and original embankment(OE), were used to analyze the thermal-deformation process. The results indicate that the widening part presented the remarkable thermal disturbance to the existing embankment(EE). The underlying permafrost was in a noteworthy degradation state, embodying the apparent decrease of the permafrost table and the increase of the ground temperature. Correspondingly, the heat disruption induced by widening led to a much higher deformation at the widening side compared to the original embankment, showing a periodic stepwise curve. Specifically, the deformation mainly occurred in the junction of the EE and the widening part, most of which was caused by the thawing consolidation near the original permafrost table. In contrast, the deformation of EE mainly attributed to the compression of the active layer. Furthermore, it was the deformation origination differences that resulted in the differential deformation of WE developed gradually during the monitoring period, the maximum of which reached up to 64 mm.  相似文献   

基于CNN和RF算法的ECMWF降水分级订正预报方法     

赵华生  金龙  黄小燕  黄颖 《气象科技》2021,49(3):419-426

利用卷积神经网络(CNN)和随机森林回归模型,提出了一种新的欧洲中期天气预报中心(ECMWF)降水订正预报方法.该方法首先根据ECMWF模式对站点雨量预报值所属的等级进行划分,再计算出不同等级相对应的高相关因子矩阵.进一步利用CNN模型对高相关矩阵进行综合特征提取的学习和训练.最后对CNN模型最终输出的特征因子中,选取...  相似文献