寿昌-临浦火山带基底构造特征及其对铀成矿的控制

中国东部中生代陆缘寿昌-临浦火山带叠置于基底和下伏地幔的隆起带上。岩石圈的薄弱、地幔软流层传递的岩浆和热流、基底富铀地层及其深熔产物提供的铀源、北北东向挤压-拉张断裂系统、幔源中基性熔浆析出的CO_2,构成完整的火山洼地铀成矿机制。     

论陕西省饮用天然矿泉水形成机理

饮用天然矿泉水是一种宝贵的地下矿产资源,它具有医疗保健作用,是补充人体必需的微量元素的主要途径之一。陕西饮用天然矿泉水的形成受深大断裂带、盆地中相对隆起带以及岩体所控制。     

Application of intervention analysis to a road fatality series in ontario

Effect of an intervention on a road fatality time series is studied using (i) the usual intervention analysis of Box and Tiao (1975), and (ii) CUSUM charts for the one-step-ahead forecast errors. It is shown that the seat belt and speed limit legislations of the Ontario Government had some impact in bringing down the road toll level.     

带式无级变速传动分析

本文对南京爱德印刷有限公司的从意大利等国进口的装订机械中的带式无级变速传动装置进行了结构分析,运动分析和力分析;对于其零部件,在失效分析的基础上,提出了改进的措施。     

深槽胶带输送机过渡段的成形分析

对深槽胶带输送机过渡段的成形曲线方程进行推导，使之用作合理布置托辊的理论依据。     

郯庐断裂带的基本特征及其对沉积盆地的控制

郯庐断裂带是我国东部的一条巨型断裂带。在山东境内是不同大地构造单元的分界线,使东西两侧的深部、基底和盖层在地质和地球物理方面,都有很大的差异。该断裂成生于太古代中期,并开始对两侧的沉积与剥蚀起控制作用。在长期的活动中,表现出间歇性、继承性和差异性。运动特点则主要以差异升降为主,没有发生大规模的水平运动。     

35 ka BP climate simulations in East Asia and probing the mechanisms of climate changes

Interglacial or postglacial climates are all of charac-teristic of warmer conditions. However, if condition asso-ciated with the warm feature is wetter or drier than today,it would produce different impacts on natural environ-ments and human society. Quaternary studies found thatclimate with warm-dry or warm-wet conditions had oc-curred in China during the last 40—30 ka BP[1]. For ex-ample, it was warmer than the present during themid-Holocene (3—8 ka BP) and the late phases of MarineIsot…     

略论带传动的包角系数

文中通过对单根V带的额定功率和V带传动所需带的根数的计算公式进行分析,提出了包角系数的定义及其数学表达式,给出了不同材科配偶的带和带轮在不同包角时的包角系数值,并对带传动的设计问题提出了新的见解。     

Eocene high grade metamorphism and crustal anatexis in the North Himalaya Gneiss Domes,Southern Tibet

Determination of the timing and geochemical nature of early metamorphic and anatectic events in the Himalayan orogen may provide key insights into the physical and chemical behavior of lower crustal materials during the early stage of tectonic evolution in large-scale collisional belts.The Yardoi gneiss dome is the easternmost dome of the North Himalayan Gneiss Domes(NHGD),and contains three types of amphibolites with distinct mineral assemblage,elemental and radiogenic isotope geochemistry,as well as various types of gneisses.SHRIMP zircon U/Pb analyses on the garnet amphibolite and garnet-bearing biotite granitic gneiss yield ages of nearly peak metamorphism at 45.0±1.0 Ma and 47.6±1.8 Ma,respectively,which are 2 to 4 Ma older than the age for partial melting in migmatitic garnet amphibolite(43.5±1.3 Ma).Available data have demonstrated that ultra-high pressure metamorphism in the Tethyan Himalaya occurred at ～55 Ma,and high amphibolite facies to granulite facies metamorphism at 45 to 47 Ma.In addition,partial melting at thickened crustal conditions occurred at 43.5±1.3 Ma,which led to the formation of high Sr/Y ratios two-mica granites.The high-grade metamorphic rocks in the NHGD may represent the subducted front of the Indian continental lithosphere.In large collisional belts,fertile components in crustal materials could melt and form granitic melts with relatively high Na/K and Sr/Y ratios under thickened crustal conditions,significantly different from those formed by decompressional melting during rapid exhumation.     

钢丝磨削试验研究

砂带磨削作为一种新工艺,在机械加工领域发挥着越来越大的作用,满足了各种加工要求。本文简单介绍了砂带磨削的概念,阐述了一个针对钢丝表面除锈的新型砂带磨削设备的工作原理及其机床的主要机构,并通过试验研究磨削压力、金属去除率、砂带磨损、磨削比、磨削深度、钢丝走速之间的关系,为砂带修磨线材生产线提供了合理的磨削工艺参数。