调压积时式悬沙采样器进口流速特性的研究

进口流速应接近于天然流速,这是设计调压积时式悬沙采样器的重要技术要求。如何才能使研制的仪器符合这一要求?重要的问题是,应从理论上进行研究,分析影响进口流速的主要因素及其相互关系,在此基础上,进行仪器的设计和试制,并通过反复的试验和改进,使仪器性能达到预期的要求。现对调压积     

Study on relationship between deep and shallow structures along north boundary fault of Yanqing-Fanshan basin

IntroductionTheYanqing-Huailaibasin,whichconsistsoftheYanqing-FanshanandHuailai-Zhuolusub-basins,ismainlycontrolledbythenorthboundaryfaultsofthesub-basins.AsabasictectonicunitattheintersectionofthenortheasternendoftheNNE-trendingShanxigrabensystemandtheNW-trendingZhangjiakou-Penglaifaultzone,ithaskepttheintensivetectonicactivityintheQuaternary(YANG,1982;XU,DENG,1988;XU,MA,1992;FANG,etal,1993;Pavlides,etal,1999).Overthepastdecade,manyresearchershaveconductedstudiesonthedetailedstr…     

云南省旅游资源开发的SWOT分析及对策研究

旅游资源是旅游业发展的基础，旅游资源开发在一定区域存在一定的优势、劣势、机遇和挑战，优势和劣势、机遇和挑战之间存在相互转化的互动关系。在区域旅游资源开发中科学分析资源开发中的SWOT因素，制定适宜的开发战略，可以变劣势为优势，以机遇迎接挑战，从而实现资源持续开发。用SWOT分析方法对云南旅游资源开发的优势、劣势、机遇和挑战进行了具体的分析，面对异常激烈的竞争市场，云南省应立足资源和市场，加大力度，以生态旅游为特色，全方位、深层次的开发，实现旅游业的可持续发展，从而把云南省打造成旅游大省和强省。     

大别山北麓石炭系杨山组沉积体系及聚煤规律

大别山北麓石炭系杨山组是本区唯一的含煤地层,通过分析杨山组野外剖面及钻孔的沉积特点,详述了该区冲积扇、扇三角洲沉积体系的发育特点及其演化规律;探讨了沼泽发育的有利地区,沼泽的形成与沉积体系演化之间的关系;认为杨山组的可采煤层一般都形成在退积型扇三角洲的平原相。     

长江三峡工程区微震的观测与研究

通过长江三峡库首区沿江段、盐关和仙女山断裂带３个小孔径台网近３年的地震强化观测，发现该地区同时存在着天然地震和矿山地震。其中黄陵背斜轴部结晶花岗岩体内没有观测到极微震活动；西缘秭归香溪至龙马溪一带存在着百余次微震，最高震级为ＭＬ２．５级盐关地震，与这一带的矿山开采有关；东缘宜昌石门附近也分布有数次微震；在黄陵背斜外围区域分布着若干３～４级（ＭＬ）弱震。这些地震的发生基本上反映了该地区的弱活动构造格局     

喀拉通克铜镍矿床中的金属矿物珠滴构造及成因

作为岩浆初期熔离作用形成的典型代表一珠滴状构造,在喀拉通克硫化铜镍矿床中有广泛地发育。其中,不仅有金属硫化物组成的珠滴,而且还出现少见的金属氧化物珠滴。作者对珠滴构造的形态特征、分布规律等所作的研究,以及成因探讨,在成矿理论与找矿实践中均有一定意义。     

新技术开拓了我队钻探工作新局面

自1981年地质队按专业化组建队后，我队成为单一的探矿工程专业队——河南省地矿局第五探矿工程队。现有职工670人，各类专业技术干部80多人，开动钻机8台。1982年以来我队生产形势喜人，这一年提前40天超额完成省局下达的9125米任务。1983年提前72天超额完成省局下达的10，000米任务。1984年提前95天超额完成地矿局下达的13，000米任务。工程质量逐年提高，优质孔率1981年为12％，1982年为78％，1983年和1984年均达到94％以上，钻探成本逐年下降。为什么会出现这样好的生产形势呢？     

我国在新疆首次发现富镍硫铁铜钾矿(Ni-rich djerfisherite)K_5(Fe,Ni)_(24)S_(26)Cl

Djerfisherite(俄文名:ДЖЕРФИШЕРИТ)是一种成分可变动的含钾、铁、铜、镍硫化物(有时含氯),在我国为首次发现。它的中文译名通常叫做硫铁铜钾矿,也有译作陨硫铁钾矿或硫铜钾矿的。我们1983年在新疆富蕴县某硫化铜镍矿床1号岩体金属矿物鉴定中发现一种罕见矿物,经深入系统研究,曾认为是富蕴矿K_5(Fe,Ni)_(24)S_(26)Cl。后来呈报中国新矿物及矿物命名委员会,经审查后确认该矿物为Djerfisherite的富镍变种。本文就是根据上述意见将该矿物重新厘定的结果。     

Pattern of latest tectonic motion and its dynamics for active blocks in Sichuan-Yunnan region, China

Based on the concept of "active blocks" and spatial distribution of historical earthquakes with surface ruptures as well as major and subordinate active faults. The Sichuan-Yunnan region can be divided into four first-order blocks. They are the Markam block (I), the Sichuan-Yunnan rhombic block (II), Baoshan-Pu'er block (III), and Mizhina-Ximeng block (IV). Cut by sub-ordinate NE-trending active faults, the Sichuan-Yunnan rhombic block (II) can be further divided into two sub-blocks: the northwestern Sichuan sub-block (II1) and the middle Yunnan sub-block (II2), while the Baoshan- Pu'er block (III) can be further divided into three sub-blocks: Baoshan sub-block (III1), Jinggu sub-block (III2), and Mengla sub-block (III3). A quantitative study of offset landforms is carried out and the basic types of active faults and their long-term slip rates along the major boundaries of active blocks of different orders in the Sichuan-Yunnan region are determined, through slip vector analysis, the motion states of the active blocks are clarified and the deformation coordination on the block margins is discussed. It is suggested that the tectonic motion of the blocks in this region is a complex or superimposition of three basic types of motions: southeastward sliding, rotating on vertical axis, and uplifting. The Markam block (I), the northwestern Sichuan sub-block (II1), and middle Yunnan sub-block (II2) have a southeastward horizontal sliding rate of 1-5 mm/a, clockwise rotating angular rate of 1.4-4(/Ma, and uplifting rate of about 1 mm/a. The Baoshan-Pu'er (III) and Mizhina-Ximeng (IV) blocks have also been extensively clockwise rotated. This pattern of motion is a strain response to the collision between the Indian and Eurasian plates and the localized deformation and differential slip on the block margins associated with the northward motion of the Indian Plate. Because a set of transverse thrusts between the blocks absorbs and transforms some components of eastward or southeastward sliding motion, the eastward escape or extrusion of the Tibetan Plateau is limited as "imbricated thrusting transformation-limited extrusion model".