贵州省地勘局工勘施工业（岩土钻掘工程业）“十五”期间主要成果及“十一五”规划

一、“十五”期间取得的主要成绩 “十五”期间，全局工勘施工业坚持以市场为导向，从实际出发，大胆创新，加强实践，及时调整不合时宜、束缚和阻碍生产力发展的一些制度、观念和作法，通过不断深化改革，调整队伍结构和产业结构、提升资质、改善装备水平、加强管理等措施，较好地拓宽了市场服务领域，创收能力逐年提高，其作为地勘经济骨干产业的地位和作用日益凸显。     

Indium Enrichment in the Meng'entaolegai Ag-Pb-Zn Deposit, Inner Mongolia, China

Abstract. The Meng'entaolegai In-rich Ag-Pb-Zn deposit is located in the eastern part of Inner Mongolia. It is one of the In-richest deposits in China. Large amounts of quartz and sulfide minerals constitute a hydrothermal quartz-sulfide vein deposit within a Hercynian acidic granite massif, which occupies an area of about 400 km². Thirty-six orebodies, controlled strictly by the E-W trend faults, are found in the orefield of 6 km in length from east to west and 200 to 1,000 m in width from south to north. The ore minerals are mainly galena, sphalerite and pyrite, and subordinate chalcopyrite, arsenopyrite, cassiterite and stannite with many Ag-minerals. The gangue minerals are mainly quartz, calcite, sericite and chlorite. Economic components of the deposit are dominated by Pb andZn (reserves of Pb and Zn are 0.17 Mt and 0.37 Mt, and their grades are 1 % and 2.3 %, respectively), with Ag, Sn, In and Cd (1,800 t Ag, >2,000 t Sn, >500 t In and 1,800 t Cd) as by-products. Indium is highly enriched in ores and its contents are 9 to 295 ppm in ores and 85 to 2,660 ppm in sphalerite. Analytical results show that the ore-forming fluid of this deposit contains 0.8–3.5 ppm In and 4–36 ppm Sn, and the two elements show a very good positive correlation with a correlation coefficient of 0.8672, while the correlation between In and Zn in the ore-forming fluids, with a correlation coefficient of 0.5723, is not as good as that between In and Sn. This indicates that indium has an affinity with tin in the ore-forming fluids. The authors think that this is probably the main reason why those In-rich deposits spread over the world are simultaneously enriched in tin.     

大变形有限元法分析边坡稳定性

边坡稳定性分析的重要任务是确定边坡潜在滑面的位置及相应的安全系数,鉴于坡体位移可在现场监测中直接得到,提出边坡潜在滑面确定的位移判据,采用大变形有限元首先计算出边坡的位移场,然后在开挖面的不同高度作塑性区内的水平位移参考线,依次连接参考线上的位移突变点即得到边坡失稳的潜在滑面位置,分析滑面上的应力以及岩体抗剪强度即得到边坡的整体安全系数。     

长白山圆池泥炭氮元素分布特征及其影响因素分析

通过对长白山圆池4个泥炭剖面样品的分析,揭示了其氮元素分布规律。在圆池选取4个具有代表性的采样点,利用泥炭采样器采取新鲜泥炭样品。分析结果表明,4个泥炭剖面氮元素含量在0.014%~3.353%之间;剖面间相比较,其中贫营养泥炭整体含氮量较低;4个泥炭剖面的氮元素分布呈现明显规律,受泥炭上层不同植物、泥炭水分和有机质含量等因素的影响,泥炭剖面中氮元素累积峰可能出现在剖面的表层(0~5cm)或中间层(10~20cm);泥炭剖面氮元素与有机质呈极显著的正相关;泥炭剖面C/N比值变化在9.51~66.98之间,部分剖面层位C/N比值异常高,表明该层位碳的累积速度显著高于氮元素。     

福建省山仔水库浮游植物特征与水体富营养状况分析

采用浮游植物指示法评价了福州省山仔水库2005年不同季节水体的富营养状况,结果表明:冬、春季库区水体处于中—富营养水平,夏季发生水华微囊藻(Microcystis flos-aquae)“水华”,水体处于富营养水平,秋季水体处于中营养水平.由于浮游植物的生长状况受到多因素的影响,有必要进一步结合其他评价方法对整个水体的富营养状态做出综合判断.     

REE characteristics of the Fanshan alunite deposit in Zhejiang Province, China

1 Introduction Alunite [KAl3(SO4)2(OH)6] is a very important non-ferrous metal resource, so many countries throughout the world have made great investments in research on the mechanism of its formation, its geological characteristics and applications. O…     

Evolution from Oceanic Subduction to Continental Collision: a Case Study from the Northern Tibetan Plateau Based on Geochemical and Geochronological Data

Two apparently distinct, sub-parallel, paleo-subduction zonescan be recognized along the northern margin of the Tibetan Plateau:the North Qilian Suture Zone (oceanic-type) with ophioliticmélanges and high-pressure eclogites and blueschistsin the north, and the North Qaidam Belt (continental-type) inthe south, an ultrahigh-pressure (UHP) metamorphic terrane comprisingpelitic and granitic gneisses, eclogites and garnet peridotites.Eclogites from both belts have protoliths broadly similar tomid-ocean ridge basalts (MORB) or oceanic island basalts (OIB)in composition with overlapping metamorphic ages (480–440Ma, with weighted mean ages of 464 ± 6 Ma for North Qilianand 457 ± 7 Ma for North Qaidam), determined by zirconU–Pb sensitive high-resolution ion microprobe dating.Coesite-bearing zircon grains in pelitic gneisses from the NorthQaidam UHP Belt yield a peak metamorphic age of 423 ±6 Ma, 40 Myr younger than the age of eclogite formation, anda retrograde age of 403 ± 9 Ma. These data, combinedwith regional relationships, allow us to infer that these twoparallel belts may represent an evolutionary sequence from oceanicsubduction to continental collision, and continental underthrusting,to final exhumation. The Qilian–Qaidam Craton was probablya fragment of the Rodinia supercontinent with a passive marginand extended oceanic lithosphere in the north, which was subductedbeneath the North China Craton to depths >100 km at c. 423Ma and exhumed at c. 403 Ma (zircon rim ages in pelitic gneiss). KEY WORDS: HP and UHP rocks; subduction belts; zircon SHRIMP ages; Northern Tibetan Plateau     

RTK在大比例尺地形图航测数字化测图中的应用

结合某开发区1：2000地形图航测数字化测图工程，探讨了采用GPSRTK的自由基站二步法拟合方式测量航外像控点（平高点），实施大比例尺地形图野外检测的可行性。对比测量实验表明，该方式在像控点要求的特定位置不仅能保证平面精度，也可以保证高程精度；与常规的RTK相比，该方式具有基站设置位置灵活、不需单独提前解算基准转换参数，以及显著提高工效等优点。     

内蒙古巴特敖包地区早古生代洋壳消减的岩石证据

内蒙古白云鄂博北部巴特敖包、查干呼绍一带分布着一系列岛弧型侵入岩,其岩石地球化学特征与典型的埃达克岩(adakite)一致:SiO2 多≥56 %,Al2O3 >15 %,MgO<3 %(很少大于 6 %),Yb(0.726 ~ 2.789)×10-6,La/Yb>10 ~ 20,Y(6.842 ~ 28.734)×10-6,Sr>400×10-6,Sr/Y≥20 ~ 40;Mg#值在0.51 ~ 0.58之间,多大于0.40;稀土元素分析,显示为轻稀土富集、重稀土亏损型,具正铕异常或微弱负铕异常;微量元素蛛网图中具明显的Sr峰和Nb、Ti低谷。9组锆石 U Pb同位素年龄值(206 Pb/238 U)范围在 345.06 ~ 552.671 Ma间,反映了本区大洋板块消减事件的年龄。构造环境判别证明它们是在岛弧环境下形成,为早古生代期间南蒙古洋板块向宝音图微陆块发生强烈斜向俯冲(oblique subduction),古洋壳板块发生部分熔融、消减而形成的产物。     

美国坦帕湾地区供水策略介析

世界范围内的水资源和水环境问题越来越突出。首先系统介绍了美国弗罗里达州坦帕湾地区的水资源利用现状和供水管理策略,对该地区的地表水、地下水、海水淡化和废水利用的情况作了详细分析。该地区从以地下水为主的供水方式,改变为地表水、地下水、海水淡化各占1/3的供水方式的规划思想、经济分析以及管理措施具有积极的参考意义。针对我国的客观背景,进一步探讨了城市供水的挖潜途径,雨水直接回收和中水利用是城市节水的两个有效方式,沿海地区则应对海水淡化予以重视;对于广大的农村乡镇,雨水集水塘和小型平原水库则是提高农村供水条件和改善水环境的一种有效措施。