玻纤、矿纤对钢渣/矿渣复合胶凝材料强度和膨胀性的影响

研究了玻纤、矿纤分别掺入钢渣/矿渣复合胶凝材料时对胶砂强度的影响,通过沸煮和压蒸试验研究两种纤维对胶凝材料体积膨胀的影响,通过SEM观察纤维与基体的界面粘结情况。强度实验结果表明,玻纤掺量(质量分数)不高于0.3%时,胶砂试件各龄期强度随着掺量的增加而提高,掺量高于0.3%,胶砂试件强度损失大;矿纤掺量对试件早期强度影响不大,后期抗压强度随掺量的增加持续下降,后期抗折强度先下降后上升。沸煮和压蒸试验结果表明,玻纤掺量0.3%的压蒸试件比不掺纤维时压蒸膨胀率下降26.60%,矿纤掺量0.3%的压蒸试件比不掺纤维时压蒸膨胀率下降29.36%。SEM结果显示,水化早期纤维表面附着少量C—S—H凝胶,纤维与基体相互分离,水化后期,纤维表面生长Ca(OH)2晶体,纤维与基体粘结紧密。     

膨胀剂和玄武岩纤维对含氯盐混凝土压拉性能的影响

研究了不同掺量的膨胀剂和玄武岩纤维对含氯盐混凝土抗压强度和劈裂抗拉强度的影响。结果表明:当膨胀剂掺量和玄武岩纤维掺量相同时,含氯盐混凝土压拉强度随氯盐掺量的增加而增加;当氯盐掺量和玄武岩纤维掺量相同时,含氯盐混凝土压拉强度随膨胀剂掺量的增加而降低。与素混凝土相比,当氯盐掺量、玄武岩纤维掺量和膨胀剂掺量分别为4 kg/m~3、3 kg/m~3和8%时,含氯盐混凝土抗压强度和抗压强度增长率的最大值分别为48.3 MPa和26.4%;劈裂抗拉强度和劈裂抗拉强度增长率的最大值分别为3.63 MPa和23.5%。结果同时表明:在含氯盐混凝土中掺入玄武岩纤维对劈裂抗拉强度比对抗压强度的改善更显著。     

玄武岩纤维掺砂水泥土压拉强度的试验分析

为研究玄武岩纤维和砂对水泥土强度的影响,进行不同配比玄武岩纤维掺砂水泥土的无侧限抗压强度试验和劈裂抗拉强度试验,探讨了玄武岩纤维掺量和掺砂量对水泥土强度及破坏形态的影响和作用机制。研究结果表明:玄武岩纤维掺量0.5%、1.0%、1.5%,掺砂量10%的水泥土无侧限抗压强度分别为3.58、3.40、3.31 MPa,较素水泥土分别提高了26.1%、19.7%、16.5%;水泥土的抗拉强度随玄武岩纤维掺量的增加呈先增大后减小的趋势,在玄武岩纤维掺量为1.5%时达到最大值;玄武岩纤维掺量1.5%、掺砂量为10%和15%的水泥土抗拉强度分别为0.52 MPa和0.60 MPa,较素水泥土分别提高了44.4%和66.7%;玄武岩纤维的掺入使水泥土在破坏时保持较好的整体性,表现出一定的塑性特征;玄武岩纤维和砂在各自工作的同时,在一定程度上相互协作,共同促进水泥土压拉强度的提高。     

云南个旧卡房铜矿玄武岩K-Ar年龄及其地质意义

云南个旧是全球最大的锡铜多金属矿区,包括马拉格、松树脚、高松、老厂和卡房五大矿田。卡房铜矿主要的矿床类型有两类:玄武岩层与大理岩层间的似层状矿床和花岗岩与围岩的接触带型矿床。以矿区内玄武岩型铜矿床为主要研究对象,对矿化玄武岩进行同位素K-Ar定年。热史信息揭示矿区内存在一期66～68 Ma的成矿作用,表明玄武岩的冷却时间与其喷发期次和顶板高程具有极高的一致性。     

苏皖嘉山一盱眙地区新生代晚第三纪玄武岩的岩石地球化学特征

本文通过对苏皖嘉山一盱眙地区新生代晚第三纪玄武岩的岩石学、岩石化学及岩石地球化学的研究表明该区玄武岩具有富钛、富碱和贫铝的特点、属大陆碱性玄武岩系列。富亲石元素及轻稀土。并据过渡金属和稀土元素的分配模式等地球化学特征讨论了玄武岩形成环境及成因。     

万岩基性火山-侵入杂岩的地球化学及其构造背景

万岩基性火山-侵入杂岩地处湖南省古丈县境内,江南古陆的西北缘,主要由超浅成的辉长-辉绿岩、基性熔岩和火山碎屑岩所组成。岩石化学和微量元素、稀土元素以及钕同位素地球化学研究表明,万岩基性火山-侵入杂岩属碱性-钙碱性系列的板块内部(即大陆内部)火山作用的产物,形成于雪峰期大陆拉张伸展构造背景之下。     

Mantle olivine xenocrysts entrained in Mesozoic basalts from the North China craton：Implication for replacement process of lithospheric mantle

Mesozoic (125 Ma) Fangcheng basalts fromShandong Province contain clearly zoned olivines that arerare in terrestrial samples and provide first evidence for thereplacement of lithospheric mantle from high-Mg peridotitesto Iow-Mg peridotites through peridotite-melt reaction.Zoned olivines have compositions in the core (Mg# = 87.2--90.7) similar to those olivines from the mantle peridotiticxenoliths entrained in Cenozoic basalts from the NorthChina craton and in the rim (Mg# = 76.8--83.9) close to oli-vine phenocrysts of the host basalts (75.7--79.0). Thesecompositional features as well as rounded crystal shapes andsmaller grain sizes (300—800 μm) demonstrate that thesezoned olivines are mantle xenocrysts, i.e. disaggregates ofmantle peridotites. Their core compositions can representthose of olivines of mantle peridotites. The zoned texture ofolivines was formed through rapid reaction between the oli-vine xenocryst and the host basalt. This olivine-basaltic meltreaction could have been ubiquitous in the Mesozoic litho-spheric mantle beneath the North China craton, i.e. an im-portant type of the replacement of lithospheric mantle. Thereaction resulted in the transformation of the Paleozoic re-fractory (high-Mg) peridotites to the late Mesozoic fertile(Iow-Mg) and radiogenic isotope-enriched peridotites, lead-ing to the loss of old lithospheric mantle.     

Origin of two differentiation trends in the Emeishan flood basalts

Both the Bowen and Fenner differentiation trends have been recognized in the Emeishan flood basalts.While the Longzhoushan laveas in Panxi paleorift evolved on a trend of silica enrichment (Bowen trend),the lavas from Guizhou evoled along the Fenner trend leading to the magmas with high Fe2O3 (23%) and low SiO2(44%) contents,This provides evidence for the existence of Fe-rich and Si-poor magmas in nature ,Such contrasting differentiation trends,marked by different timing of crystallization of Fe-Ti oxides,are correlated with the extent of crustal contamination of the magmas ,Linited crustal contamination in the Guizhou lavas is coupled with the low oxygen fugacity which delayed the onset of magnetite crystallization .In contrast,significant involvement of crustal components in the Long-Zhoushan lavas increased fo2 which in turn triggered early crystallization of magnetite.The close spatial association between the Longzhoushan lavs and the synchronous V-Fe-Ti deposit-bearing layered intrusions suggests a potential relationship between them.     

1650℃,1～3GPa下玄武岩熔体结构的实验研究

以玄武岩为初始物料,在１６５０℃,１－３ＧＰａ压力条件下进行了熔融实验,对实验产物中的玄武岩淬火玻璃进行了电子探针分析,折光率测定和ＣＩＰＷ标准矿物计算,并进行了拉曼光谱研究。     

新疆普鲁火山岩古地磁研究

塔里木地块堪称国际古地磁研究热点地区之一,但各家的研究范围都比较局限,基本上以塔里木盆地西北缘和北缘为主。截至目前为止,除个别作者在塔里木盆地南缘和西南缘进行过探索性研究外,迄今尚未见有其他作者公开报道过这些地区的古地磁研究动态和成果。本文简要介绍塔里木盆地南缘普鲁火山岩的研究成果。