U-Pb age of detrital zircons from neoproterozoic placers of the Erementau-Niyaz massif as a reflection of stages of Precambrian tectono-magmatic evolution of northern Kazakhstan

A typical feature of the Precambrian complexes of the Kokshetau, Ishkeolmess, Erementau-Niyaz, and Aktau-Dzhungaria massifs of Northern and Central Kazakhstan is the presence of the end Mesoproterozoic-beginning of the Neoproterozoic quartzite-schist sequences in these sections. The lower and upper parts of these sequences are mostly composed of schists with interlayers of quartzites and marbles and of quartzitic sandstones, respectively. It is suggested that the quartzite-schist sequences represent the sub-platform cover of a large continental block and were formed in the regressive basin with widely abundant facies of submarine deltas and a littoral shoal. The presence of horizons and the lenses enriched in zircon-rutile heavy concentrate with the amount of accessory minerals of 10-70% characterizes the quartzite-schist sections of the Kokshetau and Erementau-Niyaz massifs. The U-Pb age of zircons from one such locality in the central part of the Erementau-Niyaz massif was analyzed by LA-ICP-MS. The Concordia ages of zircons are in the intervals 1041 ± 13-1519 ± 14, 1623 ± 14-1931 ± 14, and 2691 ± 14-2746 ± 14 Ma. One age was 2850 ± 14 Ma. The age distribution is characterized by clear peaks of 1.08, 1.20. 1.34, 1.46, 1.65, 1.89, and 2.70 Ga and weak peaks of 1.13 and 1.68 Ga. The age of the majority of zircons ranges from 1309 ± 14 to 1519 ± 14 Ma. Our data indicate that mostly Neoproterozoic rocks with a subordinate role of Paleoproterozoic and Neoarchean complexes served the feeding sources for the quartzite-schist sequence of the Erementau-Niyaz massif. The Mesoproterozoic and Paleoproterozoic events identified for the detrital zircons of the Erementau-Niyaz massif are completely manifested only in Laurentia. In the first approximation, these events coincide with the assembly and breakup of the Columbia/Nuna supercontinent (～1650–1580 and 1450–1380 Ma) and assembly of the Rodinia supercontinent (1300–900 Ma).     

汶川县居民地要素空间分布特征分析

文章运用GIS空间分析技术,以四川省汶川县为研究区域,对居民地的空间分布特征及其影响因素进行分析.研究结果表明:汶川县居民地大体呈条带状分布,具有强烈的低海拔取向,其分布的优势地形区段为海拔2000m以下,居民地分布具有明显的沿河分布特征;在乡镇层面上汶川县居民地呈现一定的集聚分布特征,主要分布在海拔较低的水磨镇、漩口镇及县城所在地威州镇.研究成果可为汶川县居民地的整治规划提供参考.     

重庆万州区山地分类定量化研究

文章在GIS技术支持下,基于水文分析模型,通过DEM数据,结合山地综合分类模型,以重庆市万州区为例,对山地进行定量化分类研究,结果表明:以负地形洼地贡献区域作为山地相对高程的起算面,完全摆脱了人为因素的影响,解决了一直以来难以确定山地相对高度起算范围的难题;以负地形洼地深度作为山地相对高程是正确可行的,且能快速获取山地的相对高程;以山地表面积代替投影面积计算山地率更切合实际.     

TGR-2050型自动验潮仪的使用

剖析了TGR-2050自动验潮仪的工作原理,分析了影响测量精度的各种误差因素,指出该仪器设计上的缺陷,并给出实例,介绍了进行大气压改正的方法,得出了有益结论。     

复合蛋白源替代鱼粉对大菱鲆生长、体组成和表观消化率的影响

本实验旨在研究谷朊粉、宠物级鸡肉粉、脱脂肉骨粉、豆粕和玉米蛋白粉复合替代0%(对照组,CON)、35%(FM35)、50%(FM50)、65%(FM65)、80%(FM80)鱼粉对大菱鲆(Scophthalmus maximus)生长、体组成和表观消化率的影响。设计5组等氮等能(粗蛋白52%,总能19kJ/g)的饲料,养殖鱼初重(8.63±0.01)g,养殖周期9周。结果显示,替代组体末重、增重率和特定生长率显著低于CON(P0.05),而摄食率和成活率各处理组之间没有显著变化(P0.05)。替代组饲料效率和蛋白质效率随着替代水平的升高而降低,FM65和FM80饲料效率和FM80蛋白质效率显著低于CON(P0.05)。复合蛋白替代鱼粉对鱼体水分、粗蛋白和粗脂肪没有显著影响(P0.05),但替代组鱼体灰分显著高于CON(P0.05)。除FM35干物质表观消化率与CON没有显著差异(P0.05),其他替代组的干物质和粗蛋白表观消化率均显著低于CON(P0.05)。研究表明,该比例复合蛋白源替代鱼粉水平应不超过35%。     

Changes in record-breaking temperature events in China and projections for the future

Theoretical and Applied Climatology - As global warming intensifies, more record-breaking (RB) temperature events are reported in many places around the world where temperatures are higher than...     

X荧光光谱分析技术在测定安徽月山矿床铁铜矿石中Fe、Cu的应用研究

为建立符合安徽月山矿区的X荧光光谱(XRF)分析方法,针对矿区铁矿、铜矿的特点,用铁、铜矿石的国家标准物质制作系列校准样片,通过粉末压片和玻璃熔融两种制样方法,波长色散X荧光光谱法测定主矿体样品中的Fe、Cu等主量元素,并将测定结果与传统化学方法分析结果进行比较。结果显示,熔片法-XRF的测定结果与化学容量法测定结果一致,试样在850℃灼烧,按40∶1大稀释比熔融制样,解决了样品在高温熔融过程中对铂黄坩埚的腐蚀,适用于月山矿区铁铜矿样品中Fe、Cu的测定。粉末压片法不能克服矿物效应和粒度效应的影响,测定结果与化学容量法结果比对偏差较大,不适用于月山地区铁铜矿中Fe、Cu的测定。     

洋脊和年轻洋壳俯冲与埃达克岩生成的热模拟

新生代以来 ,环太平洋周边分布的埃达克岩 (Adakite)主要与年轻洋壳俯冲时在 70～ 90km深处的部分熔融有关。利用数值方法 ,模拟了洋壳俯冲的热演化过程并讨论了脱水、熔融对埃达克岩浆活动的影响。结果表明 :仅在活动海岭俯冲前后约 10Ma内 ,年轻的、热的俯冲海洋板片在 75～85km深度范围内 ,温度升高至 82 5～ 10 0 0℃脱水 ,导致年轻洋壳中角闪岩部分熔融 ,形成埃达克岩(Adakite)。而一般洋壳俯冲在 10 0km以下深度才脱水 ,由于脱水区压力较高洋壳自身不能熔融 ,水进入上覆地幔楔状体导致部分熔融 ,形成安山岩 (Andesite     

高密度电法在江西吉安某地区地热勘查中的应用

高密度电法具有点采集效率高,探测精度高等优点,广泛应用于工程地质和水文地质勘查。本文将高密度电法应用于某工区的地热勘察,通过圈定地热的供热通道断层,验证了高密度电法在地热勘探中的可行性。本次工作采用温纳装置,反演结果清晰地反映出地下的电性分布情况,为地热勘探提供了地球物理依据。