川滇地区活动地块现今地壳形变特征     

乔学军  王琪  杜瑞林 《国际地震动态》2004,(Z1):10

位于青藏高原东南缘的川滇菱形块体的地壳运动主要以鲜水河、安宁河、则木河、小江、红河、澜沧江、龙门山等深大断裂的强烈构造活动为特征,新生代以来受青藏高原物质向东侧流动及阿萨姆顶点楔入的作用,使该地区构造活动复杂,地震活动强烈而频繁,是研究地壳形变与地震的有利地区之一.但由于形变观测资料时空分布的制约,以前很多学者对川滇地区活动断裂的GPS形变研究主要以大尺度为主,主要反映川滇块体的整体运动特征,而对于利用GPS研究各个块体间的相互作用及其对边界带的活动构造的作用缺少深入的分析,本文正是基于1998～2002年间该地区200多GPS点位的三期GPS复测资料(网络工程和973项目),将川滇地区分为9个次级活动块体,计算了各个活动块体的欧拉旋转矢量和主要活动断裂的运动速度,并分析了该地区的应变场特征和地震危险性.结果表明川滇地区活动块体的运动有以下特点:  相似文献   

纬度圈上的大地震带     

王泽皋  边庆凯  乔子云  马凤霞  赵明淳 《国际地震动态》2004,(Z1):50

根据Ms≥6.0大地震活动的空间分布,有地震带和地震区之分.中国境内既有纵贯南北缘经度分布并把我国地震活动分隔成东西两部分的南北地震带,也有横穿北纬40左右呈东西向分布的阴山、燕山地震带,以及呈片状展布的东北深震区等.  相似文献   

Aerosol polarized phase function and single-scattering albedo retrieved from ground-based measurements     

Zhengqiang Li  Philippe Goloub  Claude Devaux  Xingfa Gu  Yanli Qiao  Fengsheng Zhao  Hongbin Chen 《Atmospheric Research》2004,71(4):233-241

Aerosol optical parameters, polarized phase function and single-scattering albdeo, have been retrieved from ground-based sun photometer measurements in Beijing 2003. The measured aerosol optical thickness varies from 0.12 to 0.77 with an average value of 0.39. The measured Ångström coefficient ranges from 0.75 to 1.47 with an average value of 1.21. The retrieved single-scattering albedo at 870 nm is within the 0.76–0.94 range and the average value is 0.85, suggests there are considerable aerosol absorptions in Beijing. The maximum value of retrieved polarized phase function at 870 nm ranges from 0.068 to 0.225 with an average value of 0.16, and it illustrates good correlations with the Ångström coefficient, i.e. the relative size of aerosol particles. Analyses of measurements and theoretical calculations show the polarized phase function is sensitive to aerosol size distribution and complex refractive index, especially the imaginary part of the refractive index which denotes aerosol light absorbing effects. These results suggest that the polarized phase function is an effective and unique aerosol optical parameter and is able to improve the retrieval of aerosol physical properties.  相似文献   

桥梁气象专题研究与服务   总被引：2，自引：0，他引：2  

刘聪张忠义  黄世成 《气象科技》2004,32(6):399-403

根据实际开展的桥梁气象专题研究，分析桥梁气象研究与服务如何面对国内大型桥梁建设发展趋势所带来的机遇和挑战，提出开展桥梁气象研究与服务的必要性，并从桥位气候背景、桥位气象参数取值、桥梁气象研究方法以及桥梁施工及营运期气象服务与保障等方面介绍桥梁气象专题研究及服务应开展的主要内容，同时，给出一个已投入实际使用的桥梁施工期气象环境监测与预警系统的建设思路。  相似文献   

基于GPRS的远程气象观测数据实时采集传输系统及其应用   总被引：9，自引：1，他引：9       下载免费PDF全文

刘聪 顾建吴国平  袁成松黄世成 《应用气象学报》2004,15(6):712-718

通过对远程自动气象站数据实时采集传输通讯方式的比较，提出基于通用分组无线业务（GPRS）的远程自动气象站数据实时采集和传输系统的技术方案，以小数据流方式，实现野外自动气象站观测数据的实时采集、传输和对观测设备运行的监控，达到节约经费，提高数据传输时效的目的，并将此系统成功地用于苏通长江公路大桥施工期气象环境监测与预警系统中。  相似文献   

Crustal structure of the southern Dabie ultrahigh-pressure orogen and Yangtze foreland from deep seismic reflection profiling   总被引：8，自引：0，他引：8  

Shuwen Dong  Rui Gao  Bolin Cong †  Zhongyan Zhao  Xiaochun Liu  Sanzhong Li  Qiusheng Li  Dongding Huang 《地学学报》2004,16(6):319-324

A new 140‐km‐long seismic reflection profile provides a high‐resolution crustal‐scale image of the southern Dabieshan high‐pressure (HP) metamorphic belt and the Yangtze foreland fold‐and‐thrust belt. The seismic image of the stacked section shows that the southern Dabieshan metamorphic terrane and Yangtze foreland belt are separated by a large north‐dipping fault. In the foreland the upper crust is dominated by a series of folds and thrusts formed during the collisional stage in the mid‐Triassic; it was reworked by crustal extension resulting in the formation of a late Jurassic and Cretaceous red‐bed basin. The southern Dabieshan profile shows stacked crustal slabs developed along the margin of the collisional orogenic belt. The Moho reflectors at 10–11 s (～30–33 km) are seismically prominent and segmented by a number of south‐verging thrusts that were probably developed by foreland‐directed thrusting of the deeply subducted continental crust during exhumation. The seismic reflection profile suggests that structures related to the Triassic–Jurassic subduction and exhumation of the Yangtze plate are preserved despite the severe crustal extension superimposed during the late Mesozoic and Cenozoic.  相似文献   

铁路缓和曲线的等间隔放样方法     

姜晨光  姜祖彬  严立明  蔡伟  乔元昌 《现代测绘》2004,27(1):28-30

介绍了铁路缓和曲线设置的目的、作用、基本原则和重要意义，阐述了等间隔放样缓和曲线的基本原理，给出了等间隔放样缓和曲线放样要素采集的基本方法，叙述了缓和曲线等间隔放样的工作过程。  相似文献   

The spectacular fossils of the ‘water margin’: the Cambrian biota of Chengjiang,Yunnan, China          下载免费PDF全文

Mark Williams  David J. Siveter  Derek J. Siveter  Sarah E. Gabbott  Xiaoya Ma  Mark A. Purnell  Peiyun Cong 《Geology Today》2016,32(6):233-237

Shi Nai'an's fourteenth century Chinese epic ‘Water Margin’ tells of the release of 36 heavenly spirits and 72 baleful stars from their captivity beneath a tablet of stone at Mount Longhu in Jiangxi Province. They are reincarnated as the 108 heroes of the Liangshan marsh in Shandong Province, who rise against an unjust world. The virtuous exploits of the ‘108’ were brought to life through the cathode‐ray screens of 1970s television sets, as the TV series The Water Margin introduced heroes like Lin Chong battling his evil nemesis Gao Qiu. Far to the west of Jiangxi Province and several hundred years after the Water Margin during the summer of 1984, a young scientist from Nanjing was working amongst the hills and lakes of southern Yunnan Province. He too overturned a stone slab, releasing from their half‐billion year captivity a cornucopia of new Chinese legends. His name was Xianguang Hou and he had made one of the most momentous fossil discoveries in history, uncovering the exceptionally preserved marine fossils of the Chengjiang biota from the ancient water margin of Cambrian seas.  相似文献   

大兴安岭北部伊图里河地区二长花岗岩的成因及构造背景   总被引：1，自引：0，他引：1  

吴涛涛  陈聪  刘凯  鲍庆中  周永恒  宋万兵 《地质学报》2016,90(10):2637-2647

本文对大兴安岭北段伊图里河地区黑云二长花岗岩进行了系统的地球化学及锆石U-Pb同位素年代学研究,旨在查明其成岩时代及岩石成因,并探讨其构造意义。研究结果表明,该黑云二长花岗岩的LA-ICP-MS锆石U-Pb年龄为123.3±0.8Ma,表明其形成时代为早白垩世晚期。岩石具有具有高硅、富钾、富铝的特征,A/CNK比值较大(0.96~0.99),痕量元素具有轻稀土富集、重稀土亏损、富集Rb、K等大离子亲石元素和Th、Ce、Zr、Hf等高场强元素,贫Sr、P、Ti、Ba的特征。以上特征表明伊图里河地区花岗岩为具钾玄质系列岩石特征的铝质A型花岗岩,为中下地壳岩石部分熔融的产物,该期岩浆侵位活动可能发生在早白垩世晚期东部古太平洋板块向欧亚板块俯冲作用下的弧后伸展环境。  相似文献   

松辽盆地西缘早白垩世伸展事件：流纹岩锆石U Pb年龄、地球化学研究   总被引：4，自引：0，他引：4  

程银行  李影  刘永顺  滕学建  李艳锋  杨俊泉  奥琮 《地质学报》2016,90(12):3492-3507

为研究松辽盆地西缘大兴安岭早白垩世火山岩的构造属性,对研究区内流纹岩开展锆石U-Pb测年和地球化学测定。锆石U-Pb定年结果显示,流纹岩形成于131.6±0.6~123.9±1.7Ma,属早白垩世。主量元素分析表明,流纹岩具高硅(SiO_2=69.08%~79.58%)、富碱(K_2O+Na_2O=5.93%~9.76%,平均为8.14),富钾(K_2O/Na_2O大于1.0,平均为2.14)、贫钙镁(平均CaO为0.60、MgO为0.27)和高FeOT/MgO(平均为6.77)比值的特征,属过铝质(A/CNK=1.35~1.78)高钾钙碱性—钾玄武岩系列岩石。据微量元素地球化学特征将其划分为两组:Ⅰ组流纹岩稀土元素总量较高(∑REE介于149.04×10~(-6)~213.18×10~(-6)之间,平均为172.35×10~(-6)),轻稀土元素(LREE)富集、轻重稀土元素分馏较强[(La/Yb)_N=4.89~11.87,平均为7.75)],中等—弱负铕异常(δEu=0.54~0.88,平均为0.70),配分曲线右倾模式,强烈富集大离子亲石元素(LILE)Rb,Ba,Th,K和亏损高场强元素(HFSE)_Nb,Ta,P和Ti;Ⅱ组流纹岩以稀土总量(∑REE平均为142.60×10~(-6))相对较低,具相对较强的负铕异常(δEu=0.05~0.46,平均为0.27),配分曲线相对较平缓以及Ba,Sr,P,Ti元素的强烈亏损与Ⅰ组流纹岩相区别,两组流纹岩地球化学成分相关性较好,二者均有低的Sr(206×10~(-6))和高Yb(大于2)含量,具壳源和造山后花岗岩的特征。结合最新资料及本文研究成果,初步认为研究区流纹岩为地壳部分熔融的产物,之后经历强烈的矿物分离结晶作用,与蒙古—鄂霍次克造山后伸展作用有关。  相似文献