福建省洋源地区镁钠闪石的发现及成因探讨

根据电子探针分析成果结合矿物光性特征，在洋源南部万全岩群中浅变质岩中新发现蓝闪石类矿物－镁钠闪石，它产于闽西北与闽西南两大构造单元交接部位之南平－宁化构造岩浆岩带上，它的出现与四堡期－晋宁期构造作用密切相关，镁钠闪石的发现对于探讨该地区用至福建大地构造演化，具有一定意义。     

离子质谱计测定地质样品中镁同位素组成方法学研究

应用信通公司研制的离子质谱计（ＳＴ－ＩＭＳ），建立了地质样品镁同位素分析的实验流程和误差分析方法，为进一步分析微量地质样品中镁同位素组成和分布奠定了基础。     

攀枝花地区辛阶含钛铬铁矿的层状超镁铁-镁铁岩岩体的矿化特征

Recently, the Xin Jie layered intrusive body has been recognized in the Trap Province of SW China, which can be divided into three igneous cumulate cycles. It shows considerable similarities with the Hong Ge titanmagnetitebearing layered intrusive body in petrography and mineralization although the ore beddings near the footwall are much higher in the grade of chromium and platinum. It is suggested that the Lu Ku Intrusive Crowd, to which the Hong Ge and Xin Jie intrusives belong, in the Trap Province of SW China is probably formed in;such an environment as Palaeozoic An Ning River rift.     

http://www.sciencedirect.com/science/article/pii/S1674987111000429

The three most crucial factors for the formation of large and super-large magmatic sulfide deposits are: (1) a large volume of mantle-derived mafic-ultramafic magmas that participated in the formation of the deposits; (2) fractional crystallization and crustal contamination, particularly the input of sulfur from crustal rocks, resulting in sulfide immiscibility and segregation; and (3) the timing of sulfide concentration in the intrusion. The super-large magmatic Ni-Cu sulfide deposits around the world have been found in small mafic-ultramafic intrusions, except for the Sudbury deposit. Studies in the past decade indicated that the intrusions hosting large and super-large magmatic sulfide deposits occur in magma conduits, such as those in China, including Jinchuan (Gansu), Yangliuping (Sichuan), Kalatongke (Xinjiang), and Hongqiling (Jilin). Magma conduits as open magma systems provide a perfect environment for extensive concentration of immiscible sulfide melts, which have been found to occur along deep regional faults. The origin of many mantle-derived magmas is closely associated with mantle plumes, intracontinental rifts, or post-collisional extension. Although it has been confirmed that sulfide immiscibility results from crustal contamination, grades of sulfide ores are also related to the nature of the parental magmas, the ratio between silicate magma and immiscible sulfide melt, the reaction between the sulfide melts and newly injected silicate magmas, and fractionation of the sulfide melt. The field relationships of the ore-bearing intrusion and the sulfide ore body are controlled by the geological features of the wall rocks. In this paper, we attempt to demonstrate the general characteristics, formation mechanism,tectonic settings, and indicators of magmatic sulfide deposits occurring in magmatic conduits which would provide guidelines for further exploration.     

花岗质岩石中铜铁锌的化学分离方法

过渡族元素同位素研究是近几年才发展起来的研究领域,随着研究的范围日趋广泛,问题日渐深入,需要对更多的地质样品进行同位素组成测定和研究.尽管文献报道的有关用于多接收器等离子体质谱过渡族元素同位素分析的化学分离方法能将Cu、Fe、Zn等元素很好地分离开来,但并未对地质样品中复杂地质基体元素的分离情况进行报道.因此,笔者对花岗岩中Cu、Fe、Zn分离进行了研究.     

胶东海阳所超镁铁岩中强亲铁元素的地球化学特征及其构造环境探讨

强亲铁元素与亲石元素具有不同的地球化学行为,因此能够从不同的角度为造山带中超镁铁岩的成因及演化提供重要信息。位于苏鲁造山带东北端的胶东海阳所超镁铁岩主要由橄榄岩和辉石岩组成,它们常以团块状赋存于花岗质片麻岩中。虽然前人对这些超镁铁岩已经开展大量岩石学研究,但关于其成因及构造属性仍存在较大争议。本文开展了海阳所超镁铁岩的全岩主微量元素、强亲铁元素及Re-Os同位素的分析工作,结果显示蛇纹石化橄榄岩具有较高的MgO和Fe₂O₃^T含量,较低的Al₂O₃、TiO₂和CaO含量,明显富集流体迁移元素（U、Pb）,亏损高场强元素（Zr、Hf）,强亲铁元素没有发生明显分异,但Ru显示正异常,表明海阳所蛇纹石化橄榄岩是经历了低-中等程度部分熔融及熔/流体交代作用影响的残余地幔橄榄岩。海阳所辉石岩的主量元素表现出明显的结晶分异特征,稀土元素较原始地幔富集,铂族元素（PGEs）含量较低且发生了明显的分异,表明辉石岩的地幔源区经历过高程度的部分熔融和硫化物的分离。海阳所蛇纹石化橄榄岩的Os同位素地球化学特征表现出大洋亲和性,与辉石岩不具有熔体-残留体的关系。由于该地区发育较深层次的韧性剪切带,蛇纹石化橄榄岩中的橄榄石与辉石表现出韧性变形的特征,同时有辉石岩侵入到橄榄岩的现象,表明该地区的蛇纹石化地幔橄榄岩与辉石岩既不同时,也不同源,因此,暗示了该套岩石组合可能形成于大洋核杂岩（OCC）与洋脊型蛇绿岩（MOR）堆晶岩交互发育环境。