新疆库鲁克塔格震旦系冰碛岩的地球化学特征及其对物源区的指示

库鲁克塔格震旦系冰碛岩样品的常量元素、微量元素和稀土元素(REEs)特征表明,Na2O,Ba和HREE比太古代后页岩富集,Sr,Cr,Co,Ni和Sc则相对亏损;其他元素与NASC和PAAS特征相似.地球化学特征指示库鲁克塔格震旦系冰碛岩主要来源于以长英质岩石为主的物源区.K2O/Al2O3低的比值,表明源区物质中的碱性长石含量较低.库鲁克塔格震旦系冰碛岩的REE配分模式和负Eu异常特征表明它们的物源区中老地壳的组分占较大的比例,发生过壳内分异作用.高的Na2O的含量和(La/Yb)n>2的特征说明它们的成熟度低于PAAS和NASC.化学蚀变指数(CIA值)指示库鲁克塔格震旦系冰碛岩的物源区古风化程度较低.一些样品表现高K的特征,在Al2O3-(CaO* Na2O)-K2O(A-CN-K)三角图中表现为向K顶点方向上偏移,表明这些冰碛岩在沉积期后发生了不同程度的钾交代.     

辽西朝阳地区张家口组火山岩地球化学特征及构造背景

朝阳地区张家口火山旋回可分为3个亚旋回,火山岩主要为流纹岩类、粗面岩类和粗安岩类.地球化学特征表明,张家口旋回火山岩属高钾钙碱性岩石系列.火山岩具有高SiO2,Al2O3,K2O,Na2O和低MgO,TiO2的特征,里特曼指数均值为2.59.火山岩富集大离子亲石元素K,Rb,Sr,Zr,Ba,Pb,Li等,相容元素Ti,Co,Ni,Cr,V亏损.火山岩为轻稀土富集型,总体显示弱负铕异常、弱负铈异常.综合研究认为,张家口组火山岩成岩物质主要来源于地壳,火山岩的成因以部分熔融为主.火山岩形成于挤压造山与伸展构造的过渡环境,具有大陆板内造山带火山岩的基本特征.     

赤峰四家子盆地张家口组火山岩成因研究

根据最近几年开展的1∶5万区域地质调查获得的新资料,确认了内蒙古四家子盆地晚侏罗世张家口组的存在,并将张家口旋回火山岩划分为三个亚旋回.火山岩岩性为流纹岩类、粗面岩类和粗安岩类.对该地区火山岩的主量元素和微量元素进行了高精度分析测试,结果显示:火山岩具有高SiO2,Al2O3,K2O,Na2O含量和低MgO,TiO2含量的特征;里特曼指数σ(1.19~4.87)均值为2.47,属高钾钙碱性岩石系列.火山岩富集大离子亲石元素K,Rb,Sr,Zr,Ba,Pb,Li等,相容元素Ti,Co,Ni,Cr,V亏损.火山岩稀土总量较高,稀土配分模式呈右倾型,轻稀土分馏作用高于重稀土的分馏作用,总体显示弱负铕...     

党河南山乌里沟中酸性岩体锆石U-Pb年龄、地球化学特征及与金矿成矿关系

通过对南祁连山党河南山东段乌里沟金矿区中酸性侵入岩锆石U-Pb年龄测定及岩石地球化学分析,探讨了岩体形成的构造环境及其与金矿成矿的关系。矿区角闪石闪长岩体侵位年龄为457±6.3 Ma,岩石中各组分的质量分数:SiO2为48.98%~59.16%,Al2O3为14.51%~16.77%,K2O+Na2O为8.24%~9.47%,属准铝质、碱性-过碱性岩系列;DI为58~79,属I型花岗岩类;岩石Cr和Mg#值较低,Na2O和K2O含量接近,表明源岩含有较多的壳源成分;稀土总量中等,轻稀土富集,具弱Eu负异常;相对富集大离子亲石元素Rb、Ba、Th、K、U,亏损Nb、Ta、P、Ti。矿区二长花岗岩属碱性岩系列,比角闪石闪长岩稀土总量低、更加亏损Nb、Ta等,与角闪石闪长岩属同一岩浆源,分异程度比角闪石闪长岩高。两种岩石均具岛弧岩浆岩特征,是中晚奥陶世南祁连俯冲到较浅部位熔融形成。岩体金含量高,目前探明的矿体产于岩体内部及接触带,围岩蚀变强烈,显示岩体为金矿成矿提供物质来源和成矿热液。     

冀北崇礼红旗营子黑云斜长片麻岩的地质地球化学特征

基于当代红旗营子群是否应该解体这一观点,研究了崇礼红旗营子群中黑云斜长片麻岩的地质地球化学特征。研究表明原岩为泥质沉积岩,其特点为SiO2〉56％,Al2O3〉MgO,Na2O〉K2O,Na2O／（Na2O＋K2O）〉0．5,且其他氧化物与SiO2含量呈现出有规律的变化,随着岩石中SiO：含量的增加,TiO2,AL2O3,FeO,Fe2O3,MgO,CaO,Na2O和K2O呈明显下降趋势。稀土元素总量较低;轻重稀土分离程度较高,LREE／HREE的值为5．16～7．98,La。／Yb。的值为4．28～8．62,轻稀土富集,重稀土平坦分布,稀土配分曲线表现出中等程度的负Eu异常,δEu的值为0．73～0．83。稀土元素Ce基本无异常或略显负异常,表明其形成环境可能为一浅海相或边缘海或被陆地封闭海。     

辽西建平县义县组火山岩形成构造环境的地球化学鉴别

对辽西建平县平庄-马厂盆地的火山岩进行了岩石学、地球化学、同位素年代学研究.结果表明,火山岩属白垩纪.义县组火山作用可分为2个亚旋回.火山岩主要为流纹岩类、粗面岩类和粗安岩类.义县旋回火山岩属高钾钙碱性岩石系列.火山岩具有高SiO2,Al2O3,K2O,Na2O和低MgO,TiO2的特征.火山岩富集大离子亲石元素(LILE)K,Rb,Sr,Zr,Ba,Pb,Li等,高场强元素(HFSE)Nb,Ti,P及相容元素Co,Ni,Cr,V亏损.火山岩为轻稀土富集型,总体显示弱负铕异常、无铈异常.对火山岩形成的构造环境的地球化学判别,表明义县组火山岩成岩物质主要来源于下地壳的部分熔融,岩浆在上升过程中受到了一定程度的上地壳物质的混染.火山岩形成于板内岩石圈不均匀伸展作用环境,具有大陆板内造山带火山岩的基本特征.     

大厂凹陷MIS3阶段以来沉积物地球化学特征分析

深海氧同位素3-1阶段是指深海沉积物有孔虫氧同位素记录的第四纪末次冰期至冰后期的一个时期,期间气候表现为间冰阶、极端寒冷、多次千年尺度气候事件至最后转暖多个变化特征,相关气候变化沉积响应及影响因素等科学问题一直以来备受关注。然而,该时期相关千年尺度气候事件的记录及讨论在华北平原地区仍有争议,为探讨华北平原西北地区在该阶段的气候特征,本研究在大厂凹陷区天然剖面进行高密度碳14断代样品测试,并开展常量和微量元素地球化学含量分析,获得地球化学数据变化趋势特征,结果表明,该剖面年代从32.5ka至8.2 ka,处于深海氧同位素3阶段末期至深海氧同位素1阶段早期。在该时段,主量元素氧化物TFe2O3、Al2O3、SiO2、MgO、CaO、Na2O与K2O与微量元素Sr、V、Ni、Co、Ga、Cu、Ba、Cr和Zn均呈现一致的变化趋势;在MIS2末次冰盛期和MIS1早期中的B?lling-Aller?d暖期和新仙女木冷期,K/Na、Al/Na、化学蚀变指数 、化学风化指数 和古温度等指标与东亚季风区气候呈现一致的变化,同时与全球尺度的事件具有同步性,因此认为晚更新世晚期华北平原的气候变化可归因于全球气候系统下东亚季风区的演化。     

浙江省衢州市上方镇大理岩矿床矿物学、地球化学特征及其地质意义

衢州市上方镇位于钦杭结合带东段,是中国著名的重钙用大理岩产区,区内大理岩矿床均赋存于石炭系黄龙组碳酸盐岩地层.在野外地质调查的基础上,对上方镇大理岩矿床的碳酸盐岩进行了详细的岩相学、矿物学和地球化学研究.研究结果表明,上方大理岩矿床矿石主要为大理岩和大理岩化灰岩,具粒状变晶结构,大理岩方解石结晶较好,颗粒较大且规则,含杂质较少,大理岩化灰岩则含较多杂质,其方解石结晶较差,颗粒不规则且有溶蚀交代现象.地球化学特征显示两类碳酸盐岩化学组成相似,大离子亲石元素(Sr、Ba等)和高场强元素(Nb、Zr、U、Hf、Th等)明显富集,而Ti明显亏损.K2O/Na2O、100×MgO/Al2O3、Ga、Ba、Sr和U/Th等指标暗示碳酸盐岩原岩为沉积型碳酸盐岩,且沉积环境为受陆源碎屑物质影响较少的浅海海相沉积,显示为较强的贫氧-缺氧的还原环境特征.     

西藏朗县蛇绿混杂岩的地球化学特征及地质意义

在岩石学研究的基础上,对西藏东南部朗县蛇绿混杂岩的岩石地球化学进行了系统研究.朗县蛇绿混杂岩的变质橄榄岩和变辉绿岩具有低Na2O+K2O,且Na2OK2O,低P2O5以及MgO和TiO2变化较大等特点;稀土配分模式为轻稀土略微亏损或富集的平坦型;大离子亲石元素Rb和Sr强烈亏损,高场强元素变化较大.变玄武岩的TiO2,P2O5与N-MORB十分接近;稀土配分模式为轻稀土略微亏损或富集的平坦型,拉索村和白露村-朗县附近地区玄武岩具有E-MORB特征,而里龙地区的玄武岩具有N-MORB特点;与典型的洋中脊玄武岩比较,大离子亲石元素和高场强元素的丰度值普遍偏高,拉索地区的大离子亲石元素比较接近N-MORB,里龙地区的高场强元素十分接近N-MORB.体现具有典型洋中脊玄武岩的特征但又不完全相同,微量元素分布形式非常类似于阿曼蛇绿岩的特征,表明朗县蛇绿混杂岩可能形成于大洋中脊到岛弧的过渡环境.     

山西芦芽山早元古代紫苏花岗岩的成因：地球化学和Nd同位素证据

芦芽山紫苏花岗岩体主要由紫苏二长岩、紫苏石英二长岩、紫苏花岗岩和钾长花岗岩组成.这些花岗质岩石表现TiO2,P2O5,K2 O,Zr,Nb,Y,Pb,La,Ce和Ba富集以及高的K2O/Na2O比值,而MgO,CaO,Mg#,Th,U亏损和低的Sr/Ba、Rb/Ba比值.Zr,Nb和Ce与SiO2反相关,这与Ⅰ型花岗岩恰恰相反.这些岩石的Sm-Nd同位素特征比较均一,初始εNd值为-5.93到-6.97,亏损地幔模式年龄为2.67到2.78 Ga.这些特征说明紫苏花岗质岩浆起源于晚太古代下地壳的部分熔融,即铁镁质麻粒岩在富CO2流体存在和异常高温下的部分熔融,石榴石作为主要残余相.它们经历了干燥高温岩浆的结晶分异,辉石、斜长石、磷灰石和钛铁矿可能为早期结晶相.芦芽山紫苏花岗岩的岩浆作用形成于东部陆块和西部陆块(～1850 Ma)主碰撞期后的俯冲洋壳拆沉、地幔上隆导致的热松弛构造背景.     

Characterization of Ordovician carbonate reservoirs, southeastern Saskatchewan, Canada

The discovery of the prolific Ordovician Red River reservoirs in 1995 in southeastern Saskatchewan was the catalyst for extensive exploration activity which resulted in the discovery of more than 15 new Red River pools. The best yields of Red River production to date have been from dolomite reservoirs. Understanding the processes of dolomitization is, therefore, crucial for the prediction of the connectivity, spatial distribution and heterogeneity of dolomite reservoirs.The Red River reservoirs in the Midale area consist of 3～4 thin dolomitized zones, with a total thickness of about 20 m, which occur at the top of the Yeoman Formation. Two types of replacement dolomite were recognized in the Red River reservoir: dolomitized burrow infills and dolomitized host matrix. The spatial distribution of dolomite suggests that burrowing organisms played an important role in facilitating the fluid flow in the backfilled sediments. This resulted in penecontemporaneous dolomitization of burrow infills by normal seawater. The dolomite in the host matrix is interpreted as having occurred at shallow burial by evaporitic seawater during precipitation of Lake Almar anhydrite that immediately overlies the Yeoman Formation. However, the low δ18O values of dolomited burrow infills (-5.9‰～ -7.8‰, PDB) and matrix dolomites (-6.6‰～ -8.1‰, avg. -7.4‰ PDB) compared to the estimated values for the late Ordovician marine dolomite could be attributed to modification and alteration of dolomite at higher temperatures during deeper burial, which could also be responsible for its 87Sr/86Sr ratios (0.7084～0.7088) that are higher than suggested for the late Ordovician seawaters (0.7078～0.7080). The trace amounts of saddle dolomite cement in the Red River carbonates are probably related to "cannibalization" of earlier replacement dolomite during the chemical compaction.     

A computer generator for randomly layered structures

AcomputergeneratorforrandomlylayeredstructuresYUJia shun1,2,HEZhen hua2(1.TheInstituteofGeologicalandNuclearSciences,NewZealand;2.StateKeyLaboratoryofOilandGasReservoirGeologyandExploitation,ChengduUniversityofTechnology,China)Abstract:Analgorithmisintrod…     

海南岛地体及其毗邻陆缘晚中生代—新生代古地磁研究和构造演化

本文叙述了对海南岛及其毗邻大陆边缘白垩纪到第四纪地层岩石进行古地磁研究的全部工作过程。通过分析岩石中剩余磁矢量的磁偏角及磁倾角的变化,提出海南岛白垩纪以来经历的构造演化模式如下:早期伴随顺时针旋转而向南迁移,后期伴随逆时针转动并向北运移。联系该地区及邻区的地质、地球物理资料,对海南岛上述的构造地体运动提出以下认识:北部湾内早期有一拉张作用,主要是该作用使湾内地壳显著伸长减薄,形成北部湾盆地。从而导致了海南岛的早期构造运动,而海南岛后期的构造运动则主要是受南海海底扩张的影响。海南地体运动规律的阐明对于了解北部湾油气盆地的形成演化有重要的理论和实际意义。     

Exciton Seebeck in Molecular Systems

Various applications relevant to the exciton dynamics,such as the organic solar cell,the large-area organic light-emitting diodes and the thermoelectricity,are operating under temperature gradient.The potential abnormal behavior of the exicton dynamics driven by the temperature difference may affect the efficiency and performance of the corresponding devices.In the above situations,the exciton dynamics under temperature difference is mixed with     

Achieving Unusual States of Matter Under High Pressure

The elongation method,originally proposed by Imamura was further developed for many years in our group.As a method towards O(N)with high efficiency and high accuracy for any dimensional systems.This treatment designed for one-dimensional(ID)polymers is now available for three-dimensional(3D)systems,but geometry optimization is now possible only for 1D-systems.As an approach toward post-Hartree-Fock,it was also extended to     

《Chinese Science Bulletin》SUBJECT INDEX TO VOLUME 59(2014)

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An on-line scaling method for improving scalability of a database cluster

The explosive growth of the Internet and database applications has driven database to be more scalable and available, and able to support on-line scaling without interrupting service. To support more client's queries without downtime and degrading the response time, more nodes have to be scaled up while the database is running. This paper presents the overview of scalable and available database that satisfies the above characteristics. And we propose a novel on-line scaling method. Our method improves the existing on-line scaling method for fast response time and higher throughputs. Our proposed method reduces unnecessary network use, i.e. , we decrease the number of data copy by reusing the backup data. Also, our on-line scaling operation can be processed parallel by selecting adequate nodes as new node. Our performance study shows that our method results in significant reduction in data copy time.     

An improved R-tree based on childnode''s probability

R-Tree is a good structure for spatial searching. But in this indexing structure,either the sequence of nodes in the same level or sequence of traveling these nodes when queries are made is random. Since the possibility that the object appears in different MBR which have the same parents node is different, if we make the subnode who has the most possibility be traveled first, the time cost will be decreased in most of the cases. In some case, the possibility of a point belong to a rectangle will shows direct proportion with the size of the rectangle. But this conclusion is based on an assumption that the objects are symmetrically distributing in the area and this assumption is not always coming into existence. Now we found a more direct parameter to scale the possibility and made a little change on the structure of R-tree, to increase the possibility of founding the satisfying answer in the front sub trees. We names this structure probability based arranged R-tree (PBAR-tree).     

Integrating GIS Web services based on mediating architecture

The geographic information service is enabled by the advancements in general Web service technology and the focused efforts of the OGC in defining XML-based Web GIS service. Based on these models, this paper addresses the issue of services chaining,the process of combining or pipelining results from several interoperable GIS Web Services to create a customized solution. This paper presents a mediated chaining architecture in which a specific service takes responsibility for performing the process that describes a service chain. We designed the Spatial Information Process Language (SIPL) for dynamic modeling and describing the service chain, also a prototype of the Spatial Information Process Execution Engine (SIPEE) is implemented for executing processes written in SIPL. Discussion of measures to improve the functionality and performance of such system will be included.     

Tracking data management using topology of moving object database system for moving object constrained trajectory in LBS application

Advances in wireless technologies and positioning technologies and spread of wireless devices, an interest in LBS (Location Based Service) is arising. To provide location based service, tracking data should have been stored in moving object database management system (called MODBMS) with proper policies and managed efficiently. So the methods which acquire the location information at regular time intervals then, store and manage have been studied. In this paper, we suggest tracking data management techniques using topology that is corresponding to the moving path of moving object. In our techniques, we update the MODBMS when moving object arrived at a street intersection or a curved road which is represented as the node in topology and predict the location at past and future with attribute of topology and linear function. In this technique, location data that are corresponding to the node in topology are stored, thus reduce the number of update and amount of data. Also in case predicting the location,because topology are used as well as existing location information, accuracy for prediction is increased than applying linear function or spline function.