西藏南木林县阿木雄北花岗闪长岩LA-ICP-MS锆石U-Pb年龄、岩石成因及构造意义

对冈底斯带中段阿木雄北花岗闪长岩进行LA-ICP-MS锆石U-Pb定年,主量和微量元素地球化学分析表明,花岗闪长岩的结晶年龄为61.8±1.2 Ma。花岗闪长岩为高钾钙碱性强过铝质花岗岩,Si O2含量为58.65%~73.5%,A/CNK值介于1.01~1.10之间,A/NK值介于1.34~2.19之间,稀土元素总量(∑REE)在99.96~201.42之间,在稀土元素配分模式图上,表现为倾斜下凹的浅"V"字型,轻、重稀土分馏明显;在微量元素蛛网图上,表现出相对富集Rb、Th、La、Pr、Hf、Nd、Dy,而亏损Ta、Nb、Ce、P、Zr、Ti的特征。花岗闪长岩显示出壳幔混源的特性,母源岩浆来自地幔,而后经AFC过程所形成的分异型I花岗岩,新特提斯洋板片回撤是其形成的深部地球动力学背景。     

MC-ICP-MS标样-样品交叉测试法测定石笋样品的230Th/U年龄

借鉴国际上已经建立的方法,本研究设计了一套便捷的UTEVA树脂分离纯化U与Th的化学流程,以及多接收电感耦合等离子体质谱测量U/Th同位素的方法,用于精确测定石笋样品的²³⁰Th/U年代。U/Th同位素的测量采用标样-样品交叉测试法（standard-sample bracketing）,即在测量未知样品之前和之后分别测量标准样品的同位素,通过外部归一化和线性内插法估算测量未知样品时仪器的校正因子,如质量歧视和二次电子倍增器相对于法拉第杯的增益。为检验该方法的可靠性,本研究分析了国际U标准样品Harwell uraninite-1（HU-1）、U/Th内用标准样品MFT和已知年代石笋样品的U/Th同位素。结果显示：HU-1的δ²³⁴U=（-1.27±2.14）‰（±2σ,n=29）,该结果与国际上不同实验室的测量值在误差范围内一致。U/Th内用标准样品MFT（±2σ,n=22）的δ²³⁴U、²³⁰Th/²³⁸U放射性活度比和年代平均值分别为（408.2±3.2）‰、1.002±0.003和(124.3±0.5) ka,具有较好的重现性。47个石笋样品的²³⁴U/²³⁸U、²³⁰Th/²³⁸U放射性活度比和²³⁰Th/U校正年代的相对误差（±2σ）分别约为0.6‰、2.4‰和0.5%,与已发表数据在误差范围内吻合。     

Mind-set and close relationships: When bias leads to (in)accurate predictions.

The authors investigated whether mind-set influences the accuracy of relationship predictions. Because people are more biased in their information processing when thinking about implementing an important goal, relationship predictions made in an implemental mind-set were expected to be less accurate than those made in a more impartial deliberative mind-set. In Study 1, open-ended thoughts of students about to leave for university were coded for mind-set. In Study 2, mind-set about a major life goal was assessed using a self-report measure. In Study 3, mind-set was experimentally manipulated. Overall, mind-set interacted with forecasts to predict relationship survival. Forecasts were more accurate in a deliberative mind-set than in an implemental mind-set. This effect was more pronounced for long-term than for short-term relationship survival. Finally, deliberatives were not pessimistic; implementals were unduly optimistic. (PsycINFO Database Record (c) 2010 APA, all rights reserved)     

一种基于协同过滤技术的在线交友推荐系统的设计与实现

为了满足年轻人在交友择偶方面需求,越来越多的征友网站应运而生.随着网站用户不断增加,根据用户提交的交友要求来进行推荐,往往结果数以千计或万计,要从这里面发现用户感兴趣的对象变得非常困难,我们将协同过滤算法引入交友推荐系统,并设计了一个个性化相似项目的协同过滤算法,根据用户的兴趣进行项目最近邻居查找,大大提高了用户对搜索结果的满意度.     

辽宁省凌源县牛河梁出土的炉壁研究

在牛河梁的一座人工建造的金字塔顶部发现的，被认定是从其它地方迁移过去的炉壁残片及其粘附的炉渣是辽西地区年代最早的冶铜遗物，热释光测定其年代为距今３００～３５００年，属夏家店下层化，炉渣含镁较高，夹杂有各种粒度的纯铜颗粒财质广场 河梁附近有多处古代开采遗迹的铜矿点，其脉石矿物也含有较高的镁，这些事实表明这些炉壁残片及其粘附的炉渣是冶炼当地氧化矿石的遗物，炉壁残片结果显示，炼炉上部内径约２５ｃｍ，有     

Two new measures of attitudes about the acceptability of teen dating aggression.

Aggression in dating relationships is associated with attitudes that justify its use. Attitudes about dating aggression are targeted by prevention efforts, contributing to a need to measure these attitudes sensitively, accurately, and multidimensionally. We describe two new measures of attitudes about aggression, each tapping different attitudinal components, and compare their psychometric properties with an existing scale. The 1st assesses attitudes about physical aggression in provocative situations. The 2nd taps attitudes about verbally aggressive, controlling, and jealous tactics against a dating partner. Data from 2,313 high school students were factor analyzed and cross-validated for each new scale. Compared with an existing measure, the scales had comparable levels of reliability and validity and improved response distributions. A 2nd-order factor analysis lends support to a multidimensional view of attitudes about dating aggression. (PsycINFO Database Record (c) 2010 APA, all rights reserved)     

The impact of a sewage treatment plant's effluent on sediment quality in a small bay in Lake Geneva (Switzerland–France). Part 2: Temporal evolution of heavy metals

The Bay of Vidy is the most contaminated area of Lake Geneva, Switzerland, as a result of the release of treated and untreated waste water from the municipal sewage treatment plant of the city of Lausanne and its surroundings. The reconstruction of the historical deposition of heavy metals in the sediment of the bay has been performed by the analysis of several dated (radiocaesium) sediment cores. The presence of sewage‐derived contaminants in the Bay of Vidy since the beginning of the sewage treatment plant's operations in 1964 is clearly observed, when a sharp increase in heavy metal contents is recorded, with maximum concentrations of cadmium, copper, zinc and lead occurring between the late 1960s and early 1970s. Despite considerable improvement in recent times, the present concentrations of the investigated heavy metals in sediments of the Bay of Vidy are still higher than concentrations measured at the centre of the lake, the latter close to Lake Geneva's natural background values. It is concluded that the quantity of heavy metals deposited in the bay is considerable and, because of sediment instability, will constitute a potential hazard for biota.     

大兴安岭塔源地区中生代火山岩锆石U-Pb年代学、地球化学及构造环境

大兴安岭塔源地区广泛出露一套中生代中酸性火山岩,文章在详细的野外调查基础上对其进行岩石地球化学、U-Pb年代学研究。确定塔源地区中生代火山岩为钙碱性过铝质的中酸性火山岩,稀土配分曲线呈现轻稀土元素相对富集的右倾分布特征,具有较弱的Eu负异常,富集Rb、Th、K等大离子亲石元素,亏损Sr、P、Ti等高场强元素,初步认为火山岩主要来源于地壳的部分熔融。通过锆石LA-ICP-MS U-Pb定年获得火山岩底部英安岩~(206)Pb/~(238)U加权平均年龄为154.6 Ma,结合前人获得顶部流纹岩~(206)Pb/~(238)U加权平均年龄128.7 Ma,表明火山岩形成于晚侏罗世-早白垩世。结合区域地质资料,认为其可能是蒙古-鄂霍茨克洋闭合之后的后造山阶段产物。     

粤东金坑锡铜多金属矿区花岗岩锆石U-Pb年龄和辉钼矿Re-Os年龄及其地质意义

广东揭西县金坑铜锡多金属矿床位于粤东地区西北部莲花山断裂带南西段,是粤东锡铜多金属成矿带近年来发现的一处中—大型铜锡铅锌多金属矿床。采用LA-ICP-MS锆石U-Pb法和辉钼矿Re-Os法对矿区与成矿有关的细粒花岗岩及与锡石共生的辉钼矿进行定年,获得该矿床成岩年龄为(141.0±0.3)Ma,辉钼矿Re-Os同位素年龄为(141.3±1.0)Ma,两者年龄接近,表明成岩成矿关系最为密切。并结合细粒花岗岩主微量元素分析结果表明细粒花岗岩具有高硅富碱特点,属于高分异的I型花岗岩,这种岩浆演化末端产物细粒花岗岩有利于成矿金属元素富集,为本区成矿提供巨量的物源与热源。结合成岩成矿年龄研究与主微量分析,初步认为成矿地质体为早白垩世细粒花岗岩,并探讨该矿床的成因及其成矿动力学背景。     

东昆仑那更康切尔沟银多金属矿床晚二叠世流纹斑岩年代学和地球化学特征研究

位于东昆仑造山带的那更康切尔沟银多金属矿床是近年来发现的一大型热液脉型矿床。本文研究发现矿区深部流纹斑岩中存在斑岩型Cu矿化,且获得该流纹斑岩LA-ICP-MS锆石U-Pb年龄为253.2±1.7 Ma,形成于晚二叠世。赋矿流纹斑岩SiO_2含量为75.56%～76.01%,Na_2O+K_2O含量为4.09%～7.68%,K_2O/Na_2O为0.92～11.78,A/CNK为1.05～2.41,属高硅、高钾钙碱性过铝质岩石。该流纹斑岩明显富集Rb、K等大离子亲石元素(LILE),亏损Nb、Ti、P等高场强元素(HFSE);稀土总量(∑REE)为245×10~(-6)～265×10~(-6),轻重稀土元素分馏明显((La/Yb)_N=7.76～9.96),并表现出Eu负异常(δEu=0.03～0.38)。综合分析认为那更康切尔沟矿区可能存在多期岩浆活动,形成斑岩型和热液脉型叠加成矿,该认识对本矿区乃至区域上寻找与火山-次火山热液有关的多金属矿床,尤其是深部找矿工作具有重要的指导意义。