Alpine tectono‐metamorphic history of the continental units from Vardar zone: the Kopaonik Metamorphic Complex (Dinaric‐Hellenic belt,Serbia)     

Mario Zelic  Nicola Levi  Alessandro Malasoma  Michele Marroni  Luca Pandolfi  Branislav Trivic 《Geological Journal》2010,45(1):59-77

The easternmost zone of the Dinaric‐Hellenic belt is represented by the Vardar Zone, in which the Kopaonik Metamorphic Complex (KMC) is regarded as the lowermost unit. This complex is topped by the unmetamorphosed Brzece unit and is intruded by the Oligocene Kopaonik Intrusive complex. The KMC is characterized by a stratigraphy that includes metapelites and meta‐carbonates of Late Triassic age, associated with metabasites. It is characterized by a complex deformation history that comprises four phases: D1 to D4. The D1 phase structures occur only as relict structures, whereas the D2 phase structures are represented by isoclinal F2 folds, associated with a well‐developed S2 foliation. The estimated P‐T conditions for the D1 and D2 metamorphism are consistent with the upper greenschist facies. The D3 phase is characterized by west‐verging thrusts associated with upright folds. In contrast, the D4 phase is characterized by open folds (F4) associated with low‐angle normal faults. The D1 and D2 deformation phases developed during the shortening related to continental collision, whereas the subsequent D3 and D4 phases can be related to the progressive exhumation of the KMC. The D4 phase probably developed during extensional tectonics during and after emplacement of the Kopaonik Intrusive Complex. The data show that the continental units belonging to the Vardar zone had a long‐lived deformation history that was more complex that previously thought. Copyright © 2009 John Wiley & Sons, Ltd.  相似文献   

Vegetation development in the Middle Euphrates and Upper Jazirah (Syria/Turkey) during the Bronze Age     

Katleen Deckers  Hugues Pessin 《Quaternary Research》2010,74(2):216-226

Vegetation changes are reconstructed based on more than 51,000 charcoal fragments of more than 380 samples from nine Bronze Age sites in northern Syria and southern Turkey. In addition to fragment proportions, special attention was paid to the frequency of Pistacia relative to Quercus and Populus/Salix relative to Tamarix, fruit-tree ubiquity, and riverine diversity in order to gain an improved understanding of the human versus climatic impact on the vegetation. The results indicate that human impacts first took place within the riverine forest. This phase was followed by land clearing within the woodland steppe, especially in the northern portion of the study area. In the south near Emar, the woodland steppe probably disappeared by the Late Bronze Age. It is uncertain whether this was caused by aridification and/or human clearing. The northward shift of the Pistacia-woodland steppe is very likely a result of climatic drying that occurred throughout the entire period under investigation. Although increased deforestation is evident through time, the small proportions of imported wood indicate that local resources were still available.  相似文献   

氯化法钛白粉生产项目放射性环境影响评价     

邱国华 《铀矿地质》2010,26(3):178-186

在放射性核素走向分析和环境现状调查的基础上,对某氯化法钛白粉生产项目的放射性环境影响进行了分析、预测与评价。放射性环境现状调查表明,评价因子总体在区域环境本底范围内,经分析确定了放射性敏感点。经放射性环境影响预测,工作人员和公众所受的附加剂量分别为0.59mSv/a和9.28×10-4mSv/a,均低于年有效剂量管理限值。在落实辐射防护和环境保护措施并加强放射性环境监测后,该项目的放射性环境影响符合国家有关法规和标准限值要求。  相似文献   

SH25H型液压风动冲击钻机在大口径硬岩钻孔灌注桩施工中的试验研究          下载免费PDF全文

何龙飞  林坚  孙亚军  王宇清 《探矿工程》2010,37(8):41-43,46

根据京沪高速铁路徐州东站大口径嵌岩灌注桩工程,试制SH25H型液压风动冲击钻机？采用气动潜孔锤空气正循环组合钻进工艺,结合捞砂桶排渣,摸索总结出一套针对硬岩地层的干式成孔新方法,钻进效率及钻孔质量显著提高,为大直径成孔施工增添了一种新的方法。  相似文献   

农田排水沟渠的环境效应与生态功能综述   总被引：9，自引：0，他引：9       下载免费PDF全文

陆海明  孙金华  邹鹰  朱乾德  丰华丽 《水科学进展》2010,21(5):719-725

农田排水沟渠作为农业景观中重要的景观单元,能够调节农田生态系统水分平衡,改变流域水文情势。农田养分可以随排水过程迅速流失,也可以通过沉淀与吸附机制被农田沟渠所截留或者通过植物吸收后收割与反硝化去除等机制脱离农田生态系统。作为农田生态系统边缘的交错带,农田排水沟渠较高的植物多样性可以提供动物栖息地和避难场所,增加农田生态系统生物多样性。清淤、收割和控制排水等管理措施对于农田排水沟渠的环境效应和生态服务功能有着不同的影响。今后应加强从多个学科研究农田排水沟渠的环境效应和生态功能,探索生态排水沟渠的构建和管理技术,实现农田排水沟渠水利功能和生态功能的"双赢"。  相似文献   

桐柏北部宽坪群变泥质岩的变质作用研究   总被引：1，自引：0，他引：1       下载免费PDF全文

胡娟  刘晓春  曲玮 《地学前缘》2010,17(1)

桐柏北部宽坪群发育一套由斜长角闪岩、变泥质岩、大理岩以及石英岩夹层组成的中级变质岩石。本文选取4个含石榴变泥质岩样品进行了详细的岩石学研究,其中回龙寺组的一个样品含有特征的十字石+蓝晶石组合,而左老庄组的一个样品则含有夕线石。回龙寺组样品中的石榴石均具有明显的进变质成分环带,而左老庄组样品中的石榴石均遭受到晚期低温扩散的影响,所以在计算其形成条件时选取了生长于峰期变质阶段的特定部位。运用传统的石榴石-黑云母-白云母-斜长石-石英地质温压计估算回龙寺组的变质p-T区间为590～610℃、0.95～1.14GPa,左老庄组为630～650℃、0.65～0.89GPa,分别相当于低角闪岩相和高角闪岩相。这一结果与变质反应曲线所限定的温压范围基本一致,并且后者中还存在由蓝晶石区域向相对高温低压的夕线石区域转变的过程。低-高角闪岩相的宽坪群与低角闪岩相的二郎坪群和麻粒岩相的秦岭群紧密伴生,且变质时代近于一致(440～400Ma),说明华北南缘在志留纪—早泥盆世发生了岛弧、微陆块与华北板块大陆边缘的碰撞造山作用。  相似文献   

成矿环境中的高密度碳质流体:以阿尔泰南缘为例   总被引：1，自引：0，他引：1       下载免费PDF全文

徐九华  丁汝福  林龙华  褚海霞  王琳琳  卫晓峰 《地学前缘》2010,17(1):202

碳质流体(CO2-CH4-N2体系流体)常见于地幔橄榄岩和下地壳麻粒岩中。近期研究表明,阿尔泰南缘晚古生代成矿环境中的碳质流体极为丰富,不仅在造山型金矿中赋存大量与成矿有关的碳质流体,而且在VMS型矿床中也存在同造山期的变质碳质流体。由共生的富CO2包裹体(LCO2-LH2O型)和H2O-CO2包裹体(LH2O-LCO2型)的均一温度推测,造山型金矿的碳质流体捕获温度大于254～394.5℃,压力大于150～320MPa;VMS矿床的变质碳质流体捕获温度大于209～430℃,压力大于180～300MPa,两者具相似的捕获温度压力条件。碳质流体的捕获温度压力条件与变质相带相平衡计算的变质温度、压力范围相当。碳质流体源于区域变质作用,并参与了与造山型金矿有关的构造-变质-流体-成矿作用和对VMS型矿床的变质改造作用。  相似文献   

谈液动冲击回转钻进技术在破碎岩层中运用     

吴志强  王廷睿 《安徽地质》2010,20(2):131-134

简要说明液动冲击回转钻进是一项投资少,见效快的先进适用的钻探技术,可大幅度提高钻探效率和经济效益,增加回次长度和岩矿芯采取率,并能减少孔内事故。  相似文献   

Petrology, Mineralogy and Geochemisty of Antarctic Mesosiderite GRV 020175: Implications for Its Complex Formation History     

WANG Linyan  HSU Weibiao  and MA Changqian 《《地质学报》英文版》2010,84(3):528-542

<正>GRV 020175 is an Antarctic mesosiderite,containing about 43 vol%silicates and 57 vol% metal.Metal occurs in a variety of textures from irregular large masses,to veins penetrating silicates, and to matrix fine grains.The metallic portion contains kamacite,troilite and minor taenite.Terrestrial weathering is evident as partial replacement of the metal and troilite veins by Fe oxides.Silicate phases exhibit a porphyritic texture with pyroxene,plagioclase,minor silica and rare olivine phenocrysts embedded in a fine-grained groundmass.The matrix is ophitic and consists mainly of pyroxene and plagioclase grains.Some orthopyroxene phenocrysts occur as euhedral crystals with chemical zoning from a magnesian core to a ferroan overgrowth;others are characterized by many fine inclusions of plagioclase composition.Pigeonite has almost inverted to its orthopyroxene host with augite lamellae, enclosed by more magnesian rims.Olivine occurs as subhedral crystals,surrounded by a necklace of tiny chromite grains(about 2-3μm).Plagioclase has a heterogeneous composition without zoning. Pyroxene geothermometry of GRV 020175 gives a peak metamorphic temperature(～1000℃) and a closure temperature(～875℃).Molar Fe/Mn ratios(19-32) of pyroxenes are consistent with mesosiderite pyroxenes(16-35) and most plagioclase compositions(An_(87.5_96.6)) are within the range of mesosiderite plagioclase grains(An_(88-95)).Olivine composition(Fo_(53.8)) is only slightly lower than the range of olivine compositions in mesosiderites(Fo_(55-90)).All petrographic characteristics and chemical compositions of GRV 020175 are consistent with those of mesosiderite and based on its matrix texture and relatively abundant plagioclase,it can be further classified as a type 3A mesosiderite.Mineralogical, penological,and geochemical studies of GRV 020175 imply a complex formation history starting as rapid crystallization from a magma in a lava flow on the surface or as a shallow intrusion.Following primary igneous crystallization,the silicate underwent varying degrees of reheating.It was reheated to 1000℃,followed by rapid cooling to 875℃.Subsequently,metal mixed with silicate,during or after which,reduction of silicates occurred;the reducing agent is likely to have been sulfur.After redox reaction,the sample underwent thermal metamorphism,which produced the corona on the olivine, rims on the inverted pigeonite phenocrysts and overgrowths on the orthopyroxene phenocrysts,and homogenized matrix pyroxenes.Nevertheless,metamorphism was not extensive enough to completely reequilibrate the GRV 020175 materials.  相似文献   

佳木斯地块南缘牡丹江地区高压变质作用：黑龙江杂岩的岩石学和地质年代学   总被引：6，自引：0，他引：6  

赵英利  刘永江  李伟民  温泉波  韩国卿 《地质通报》2010,29(203):243-253

牡丹江地区出露的黑龙江杂岩是由变质基性岩、泥质片岩、大理岩和变硅质岩系列组成的类似于蛇绿岩层序的构造混杂岩,代表了佳木斯地块西南缘碰撞增生的产物。钠长石和绿帘石变斑晶中共生的矿物组合(钠云母+蓝闪石+多硅白云母+绿帘石)的地质温压计估算结果表明,黑龙江杂岩的峰期变质的温压条件为 T=320~480℃, p=800~1600MPa,为典型的绿帘-蓝片岩相高压变质作用。黑龙江杂岩带中泥质片岩所含的多硅白云母单矿物给出的40Ar/39Ar坪年龄为164.9Ma±0.5Ma。根据白云母中K-Ar同位素体系的封闭温度(350~430℃)接近于得到的黑龙江杂岩的峰期变质温度,可以认为40Ar/39Ar坪年龄指示了这期高压变质事件的年龄,也证实了黑龙江杂岩带中普遍存在一期中侏罗世末期的变质-热事件。  相似文献