黑龙江东安金矿床锆石U-Pb年龄及其地质意义

通过LA-ICPMS锆石原位定年方法,对黑龙江东安金矿成矿期脉岩流纹斑岩进行了年龄测定.结果显示,与矿化关系极为密切的流纹斑岩的U和Th含量分别为269.1×10-6~956.0×10-6和202.2×10-6~1276.8×10-6,Th/U比值介于0.43~1.80之间.流纹斑岩206Pb/238U年龄的加权平均值为109.6±1.7 Ma,与区内浅成低温热液金矿的成矿年龄相近,共同记录了本区早白垩世晚期的一次重要成岩成矿事件,反映了早白垩世晚期岩石圈大规模伸展减薄的动力学背景.     

北秦岭四方台基性-超基性杂岩锆石 LA-ICP-MS年代学研究

四方台杂岩体是北秦岭沿商-丹带出露的基性-超基性杂岩体中最大的一个,出露面积约40 km2,由超基性-基性-中性岩石组成,侵入到丹凤群中。对四方台杂岩体中辉长岩锆石进行LA-ICP-MS微区定年研究,获得岩体的成岩时代为460±29 Ma。获得的32个测点可明显地分为400~500 Ma、700~900 Ma、1 800~2 600 Ma和2 700~2 918 Ma这4个时段,可能分别代表了北秦岭造山带不同地质时期的构造-岩浆事件的时代信息。其中400~500Ma与北秦岭地区表现强烈的加里东运动时限一致,而700~900 Ma则可能与830~740 Ma中国中西部地区响应积极的、造成Rodinia超大陆裂解的地幔柱活动有关。     

东昆仑查干尕诺地区中三叠世中酸性侵入岩地球化学特征及地质意义

查干尕诺地区位于东昆仑西段祁漫塔格中东部,该区中酸性侵入岩主要岩性为花岗闪长岩和二长花岗岩,侵入于白沙河组中,且从花岗闪长岩到二长花岗岩,岩石中SiO2(65.22%~72.42%)含量逐渐增高,Al2O3(14.90%~16.79%)、CaO(1.97%~4.20%)和MgO(0.61%~2.00%)逐渐降低;里特曼指数介于1.41~2.02,K2O+Na2O全碱含量为5.04%~8.8%,属高钾钙碱性系列;稀土总量中等(∑REE=69.78×10-6~148.9×10-6),稀土元素标准化曲线右倾,为轻稀土富集型,基本无Eu异常;岩石中Rb、Th等强烈富集,Nb、Zr、Ce、Ta、Hf等富集一般,Y弱亏损。LA-ICP-MS锆石U-Pb测年表明,其形成年龄为(246.8±1.7)Ma,时代为中三叠世。以上特征表明,本区的中酸性侵入岩属I型花岗岩,结合区域地质特征,该期花岗岩类含大量暗色微粒包体,具有明显的岩浆混合的证据。说明中三叠世该区构造处于洋壳俯冲结束-碰撞开始的转变期。该套侵入岩的发现对东昆仑西段祁漫塔格地区的构造岩浆带研究及发展演化史研究具有重要意义。     

金矿测年方法讨论及定年中存在的问题

准确的成岩成矿年代测定是矿床研究和对比的基础。然而近几年来 ,不同的研究者对同一矿床采用不同的定年方法得出了相差十分悬殊的成岩成矿年龄的报道屡见不鲜。为此笔者在分析了不同定年方法适用性的同时 ,强调了在金矿定年中要加强对金矿成岩成矿地质背景的研究 ,重视不同地质体与成矿的先后关系 ,确定标志性地质体 ,选择合适的定年方法 ,测定标志性地质体和矿体的成岩成矿年代 ,使成岩成矿年代互为限定 ,得到高质量的年代学数据。     

电子探针化学测年方法

介绍含Th U Pb矿物电子探针化学测年方法的基本原理 ,并利用应用实例说明该方法在研究岩石形成年龄、构造热事件年代等方面的重要作用 ,最后简要评价该方法的优、缺点 ,并指出它的应用前景 ,认为电子探针化学测年方法将有可能在深源岩石包体年龄研究、含放射性元素矿床形成年代研究等方面大有作为 ,并使地质年代学研究更加精细化 ,有助于深入探讨复杂地质事件及其演化历程。     

塔中地区志留系碎屑锆石测年及其地质意义

志留系是塔里木盆地第一套砂岩储层广泛分布的沉积盖层,其沉积来源与成因对志留纪构造演化及周边造山带的研究具有重要意义。塔中地区3个志留系样品的碎屑锆石LA?ICP?MS U?Pb定年研究表明,志留系具有比较集中的二期物源年龄：南华纪中期、古元古代中期。碎屑锆石测定的年龄表明塔中志留系物源均来自前寒武纪,塔中东部源区方向的塔南隆起基底在奥陶纪已隆升成为蚀源区。大量的新元古代中期锆石年龄表明塔里木板块在新元古代时期可能与Rodinia超大陆具有相似的聚合与裂解演化史。     

Polymetamorphism, zircon growth and retention of early assemblages through the dynamic evolution of a continental arc in Fiordland, New Zealand

The Marguerite Amphibolite and associated rocks in northern Fiordland, New Zealand, contain evidence for retention of Carboniferous metamorphic assemblages through Cretaceous collision of an arc, emplacement of large volumes of mafic magma, high‐P metamorphism and then extensional exhumation. The amphibolite occurs as five dismembered aluminous meta‐gabbroic xenoliths up to 2 km wide that are enclosed within meta‐leucotonalite of the Lake Hankinson Complex. A first metamorphic event (M1) is manifest in the amphibolite as a pervasively lineated pargasite–anorthite–kyanite or corundum ± rutile assemblage, and as diffusion‐zoned garnet in pelitic schist xenoliths within the amphibolite. Thin zones of metasomatically Al‐enriched leucotonalite directly at the margins of each amphibolite xenolith indicate element redistribution during M1 and equilibration at 6.6 ± 0.8 kbar and 618 ± 25 °C. A second phase of recrystallization (M2) formed patchy and static margarite ± kyanite–staurolite–chlorite–plagioclase–epidote assemblages in the amphibolite, pseudomorphs of coronas in gabbronorite, and thin high‐grossular garnet rims in the pelitic schists. Conditions of M2, 8.8 ± 0.6 kbar and 643 ± 27 °C, are recorded from the rims of garnet in the pelitic schists. Cathodoluminescence imaging and simultaneous acquisition of U‐Th‐Pb isotopes and trace elements by depth‐profiling zircon grains from one pelitic schist reveals four stages of growth, two of which are metamorphic. The first metamorphic stage, dated as 340.2 ± 2.2 Ma, is correlated with M1 on the basis that the unusual zircon trace element compositions indicate growth from a metasomatic fluid derived from the surrounding amphibolite during penetrative deformation. A second phase of zircon overgrowth coupled with crosscutting relationships date M2 to between 119 and 117 Ma. The Early Carboniferous event has not previously been recognized in northern Fiordland, whereas the latter event, which has been identified in Early Cretaceous batholiths, their xenoliths, and rocks directly at batholith margins, is here shown to have also affected the country rock. However, the effects of M2 are fragmentary due to limited element mobility, lack of deformation, distance from a heat source and short residence time in the lower crust during peak P and T. It is possible that many parts of the Fiordland continental arc achieved high‐P conditions in the Early Cretaceous but retain earlier metamorphic or igneous assemblages.     

塔里木盆地东南缘阿克塔什塔格地区新太古代陆壳增生:米兰岩群和TTG片麻岩的地球化学及年代学约束

塔里木盆地东南缘的阿克塔什塔格地区,保存有较为完好的早前寒武纪基底变质岩——阿克塔什塔格杂岩,主要由米兰岩群、新太古代TTG花岗片麻岩和侵入其中的各类古元古代花岗片麻岩构成。其中米兰岩群和TTG片麻岩发育塑性流变褶皱和高角闪岩相-麻粒岩相变质,具有强烈的混合岩化,并遭受后期的角闪岩相变质改造。米兰岩群中的长英质片麻岩和TTG岩系的锆石SHRIMP U-Pb年龄分别为(2 567±32)Ma和(2 592±15)Ma,二者普遍低Si高Al、富Na贫K、富Sr贫Mg、富集LILE和LREE,亏损HSFE和HREE、轻重稀土分馏强烈、Eu异常不明显,具有类似于埃达克岩的岩石地球化学特征,表明它们形成于俯冲带的岛弧环境,为岛弧玄武岩俯冲至下地壳部分熔融的产物,指示了塔里木盆地东南缘新太古代晚期古老克拉通的大陆地壳水平增生。在此基础上,文章还探讨了塔里木盆地周缘早前寒武纪基底岩系的年代格架问题,认为塔里木盆地具有统一的早前寒武纪变质基底。