甘肃典型夯土民房承重墙体加固试验研究

武都是甘肃省典型夯土民房使用地区,研究其夯土民房的抗震性能对于防灾减灾具有重要意义。在试验中,使用武都当地常用土料,完全按照其施工工艺夯筑4片夯土墙体试件,利用伪静力方法研究了素土墙体与使用铁丝网加固墙体的抗剪强度。结果显示：①在竖向荷载10 kN条件下,加固墙体试件较素土墙体试件的水平开裂荷载和极限荷载分别增长了73%和38%,在竖向荷载18 kN条件下,加固墙体试件素土墙体试件的水平开裂荷载和极限荷载分别增长了76%和5%;②随着竖向荷载从10 kN增加到18 kN,素土墙体试件的水平开裂荷载与极限荷载分别增长了217%和359%,加固墙体试件的水平开裂荷载与极限荷载则增长了223%和249%;③在水平往复荷载的作用下,夯土墙体始终沿着夯土层间的水平和垂直接触裂缝产生破坏,最终碎裂成块体。     

重要海-气-天文事件与新德里季风降水中δ18O的关系

通过分析西南季风区印度新德里站夏季降水资料发现, 降水中δ18O变化趋势大致与太阳黑子变化趋势一致, 是温度效应的具体体现. 温度和降水的耦合导致温度和降水量的比值(T/P)与δ18O具有显著的正相关关系; ENSO与δ18O的遥相关关系是热带印度洋和太平洋海气耦合作用的结果, 是降水量效应的反映. 在500 hPa高度, 云滴的蒸发以及与下层向上层传输的季风水汽之间发生稳定同位素交换, 可能是导致500 hPa高度风的速率与δ18O正相关的主要原因, 温度效应及降水量效应对这一关系的形成起促进作用.     

GIS支持下的煤田大地测量控制点成果信息管理系统的设计与实现

建立控制测量成果管理系统是实现煤田资料数字化管理的发展方向,本文介绍了基于GIS的煤田大地测量控制成果信息管理系统的设计和控制点符号的绘制,并以河南省煤田大地测量控制点成果管理系统为例,验证了该系统的可行性与正确性。该系统的实现能够使煤田大地测量成果在规范化管理、信息处理与共享、安全性等方面得到有效改善,具有较强的实用价值。     

Tectonic Evolution of the Tianhuan Depression and the Western Margin of the Late Triassic Ordos

Abstract: The Ordos Basin is one of the most important oil and gas basins in China. Based on surface outcrop, key exploratory wells and seismic reflection data and by using the technology of “prototype basin recovery”, seismic profile “layer flattening” and “restoration of balanced section”,and other methods, the sedimentary boundary, structure and the evolution history of the Tianhuan depression on the western margin of the Ordos Basin are reestablished. The following results have been obtained. (1) The west boundary of the Late Triassic Ordos Basin was far beyond the scope of the current basin. The basin is connected with the Late Triassic Hexi Corridor Basin, and its western margin did not have tectonic characteristics of a foreland basin. (2) The Tianhuan depression was first formed in the Late Jurassic. At the late stage it was impacted by the late Yanshanian and Himalayan tectonic movement and the depression axis gradually moved eastwards to the present location with a cumulative migration distance of ~30 km. (3) Eastward migration of the depression axis caused adjustment and even destruction of the originally formed oil and gas reservoirs, so that oil and gas remigrated and aggregated, resulting in secondary structural reservoirs formed at high positions on the western flank of the depression.     

穿云飞机电磁噪声的实验分析

利用高灵敏度和高时空精度的三维雷电观测系统LMA(Lightning Mapping Array)分析穿云飞机的观测资料,发现这一系统在地面可探测到穿云飞机产生的60～66MHz带宽内的电磁辐射,其强度在1W～10kW之间,甚至更高,且与所探测到的辐射源数成线性反比,辐射是由飞机上的尖端放电产生的. 穿云飞机在10～12km高度上产生的辐射最强,且在靠近发生闪电的对流区比远离这一区域强. 飞机穿过不同云系时,辐射强度不同,其中穿过层状云系时,辐射最弱.     

Metallogenic Systems on the Paleocontinental Margin of the North China Craton

The North China Craton (NCC) is one of the largest blocks composing the continent. Different types of continental margins well developed around the NCC, along with lots of metallogenic systems of different metals and different times. Based on the study on the structural evolution of the NCC, the authors made a new division of tectonic units of the NCC. Through an analysis of the data of 1:25000 geochemical survey on stream sediments, regional geochemical features of main ore-forming elements including Au, Ag, Cu, Pb, Zn, W, Ni, Co and Mo of the NCC are discussed in the paper. Then different metallogenic systems and their forming processes and geodynamics are discussed in detail. At last, temporal and spatial distribution regularities are summarized and ten favorable ore-control factors on the paleocontinental margins are put forward, including (1) abundance of ore sources; (2) rendezvous of ore-forming fluids; (3) high thermo-dynamic anomaly; (4) remarkable Earth crust-mantle interaction; (5) cluster of     

Geochronology and Geochemistry of the Middle Proterozoic Aoyougou Ophiolite in the North Qilian Mountains,Northwestern China

The Aoyougou ophiolite lies in an early Palaeozoic orogenic belt of the western North Qilian Mountains, near the Aoyougou valley in Gansu Province, northwestern China. It consists of serpentinite, a cumulate sequence of gabbro and diorite, pillow and massive lavas, diabase and chert. Ages of 1840±2 Ma, 1783±2 Ma and 1784±2 Ma on three zircons from diabase, indicate an early Middle Proterozoic age. The diabases and basalts show light rare-earth element enrichment and have relatively high TiO2 contents, characteristic of ocean island basalts. All of the lavas have low MgO, Cr, Ni contents and Mg numbers indicating a more evolved character. They are believed to have been derived from a more mafic parental magma by fractionation of olivine, Cr-spinel and minor plagioclase. Based on the lava geochemistry and regional geology, the Aoyougou ophiolite was probably believed to have formed at a spreading centre in a small marginal basin. Subduction of the newly formed oceanic lithosphere in the Middle Proteroz     

ZD8T地电阻率观测装置稳定性检测仪

介绍了96－913重中之重课题研制的ZD8T装置稳定性检测仪的工作原理和所采用的几项关键技术，对指导地电观测台站使用该仪器进行地电阻率观测装置系统的稳定性检查有一定意义。     

中国东北地区中新生代岩浆岩中氮及其同位素组成

通过真空热解法分析中国东北地区中新生代以来形成的碱性玄武岩和基性侵入岩中氮含量及其同位素组成的差异，结果表明喷出岩和侵入岩中流体组分在岩浆的上升侵入过程中有不同的表现形式，喷出岩与围岩有较少的混染作用发生。碱性玄武岩包裹体中氮含量较低，为1．91－14．01μL/ g，δ^15N为－22．6‰～-1.8‰。侵入岩包裹体中氮含量为25．39－731.30μL/g,δ^15N为＋0．7‰～ 20.9‰。碱性玄武岩中N2含量和氮同位素组成可能部分代表了上地幔流体的特征，脱气作用造成同位素值有较大变化；而侵入岩中的N2含量和氮同位素组成更多地反映了地壳中含氮物质浓度及同位素组成特征。     

A PRELIMINARY STUDY OF SNOW MASS VARIATIONS IN CHINA OVER THE PAST 30 YEARS

Daily snow data for 2300 climate stations covering the period from 1951 through 1980 have been used to monitorand diagnose secular variations,year-to-year fluctuations,and the spatial characteristics of snow variation trends inChina.An examination of time series reveals that there is a strong teleconnction to ENSO,to major volcanic eruptions,as well as to the CO_2-induced warming.The country-wide snow mass variations are positively correlated with globalmean temperature,increasing during the current warming period and decreasing during the recent cooling period priorto the mid 1960s.A synchronous relationship exists between El Nino/Southern Oscillation and snowy winter in China.The year-to-year snow fluctuations seem to be generally out of phase with volcanic activity.The anomaly map showsthat snow mass increased in high altitudes and moist regions,while it decreased in arid lowland and the southern bounda-ry zone during the warming period.The potential CO_2-induced changes in snow mass will further aggravate the regionaldifferentiation between high mountains and lowlands,between moist and arid regions.The number of snow cover dayswill decrease in the northern lowlands,and snowfall will increase in the Qinghai-Xizang Plateau,high mountains,andthe lower reaches of the Changjiang(Yangtze)River.