云南金平白马寨含矿镁铁-超镁铁岩体岩石地球化学   总被引：7，自引：0，他引：7       下载免费PDF全文

管涛  黄智龙  许德如  张振亮  严再飞  许成 《地质科学》2006,41(3):441-454

云南金平白马寨铜镍硫化物矿床含矿岩体为侵位在奥陶系砂页岩的镁铁-超镁铁环状杂岩体。从岩体核心到边缘依次出现橄榄岩—橄榄辉石岩—辉石岩—辉长岩的岩相分带。该岩体的主量元素显示拉斑玄武岩岩浆分异演化的趋势。REE显示富集LREE的配分模式,具明显的Eu异常。微量元素蛛网图显示明显的Ta、Nb、Ti及P的负异常。具有高(⁸⁷Sr/⁸⁶Sr)_i(0.710974~0.722667)和低ε_Nd(t)(-13.17~-12.09)的特征。微量元素和同位素地球化学证据表明,岩浆源于俯冲地壳物质改造的富集地幔,岩浆上升过程中遭受了一定的地壳物质混染。岩体可能是在弧后拉张的构造环境中形成。  相似文献   

Flat rare earth element patterns as an indicator of cumulate processes in the Lesser Qinling carbonatites, China   总被引：1，自引：0，他引：1  

Cheng Xu  Ian H. Campbell  Charlotte M. Allen  Zhilong Huang  Liang Qi  Huan Zhang  Guishan Zhang 《Lithos》2007,95(3-4):267-278

The Lesser Qinling carbonatite dykes are mainly composed of calcites. They are characterized by unusually high heavy rare earth element concentrations (HREE; e.g. Yb > 30 ppm) and flat to weakly light rare earth element (LREE) enriched chondrite-normalized patterns (La/Yb_n = 1.0–5.5), which is in marked contrast with all other published carbonatite data. The trace element contents of calcite crystals were measured in situ by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS). Some crystals show reduced LREE from core to rim, whereas their HREE compositions are relatively constant. The total REE contents and chondrite-normalized REE patterns from the cores of carbonate crystals are similar to those of the whole rock. The carbon and oxygen isotopic compositions of calcites fall within the range of primary, mantle-derived carbonatites. The initial Sr isotopic compositions (0.70480–0.70557) of calcites are consistent with an EM1 source or mixing between HIMU and EM1 mantle sources. However these sources cannot produce carbonatite parental magmas with a flat or slightly LREE enrichment pattern by low degrees of partial melting. Analyses of carbonates from other carbonatites show that carbonates have nearly flat REE pattern if they crystallize from a LREE enriched carbonatite melt. This implies that when carbonates crystallize from a carbonatite melt the calcite/melt partition coefficients (D) for HREE are much greater than the D for the LREE. The nearly flat REE patterns of the Lesser Qinling carbonatites can be explained if they are carbonate cumulates that contain little trapped carbonatite melt. Strong enrichment of HREE in the carbonatites may require their derivation by small degrees of melting from a garnet-poor source.  相似文献   

大陆、海洋分布的对称性及成因探讨     

随启发 《华南地质与矿产》2007,(3):75-78

通过观察地球表面偶然发现,大陆、海洋的分布有明显的对称特征,地球一侧如为大陆,与其对应的地球的另一侧一定为海洋。依大陆、海洋分布的对称特征为基本论据,从大陆、海洋形成所需物质、物质运移、物质运移能量三大要素入手,分析讨论了大陆、海洋的形成过程,指出大陆、海洋的形成是靠地球内能的作用,形成大陆的物质来自地球另一侧与其对称分布的海洋,软流层是物质运移通道。  相似文献   

Small-world characteristics on transportation networks: a perspective from network autocorrelation     

Zengwang Xu  Daniel Z. Sui 《Journal of Geographical Systems》2007,9(2):189-205

Studies on small-world networks have received intensive interdisciplinary attention during the past several years. It is well-known among researchers that a small-world network is often characterized by high connectivity and clustering, but so far there exist few effective approaches to evaluate small-world properties, especially for spatial networks. This paper proposes a method to examine the small-world properties of spatial networks from the perspective of network autocorrelation. Two network autocorrelation statistics, Moran’s I and Getis–Ord’s G, are used to monitor the structural properties of networks in a process of “rewiring” networks from a regular to a random network. We discovered that Moran’s I and Getis–Ord’s G tend to converge and have relatively low values when properties of small-world networks emerge. Three transportation networks at the national, metropolitan, and intra-city levels are analyzed using this approach. It is found that spatial networks at these three scales possess small-world properties when the correlation lag distances reach certain thresholds, implying that the manifestation of small-world phenomena result from the interplay between the network structure and the dynamics taking place on the network.   相似文献   

Application of RAPD in genetic diversity study onGracilaria lemaneiformis III. Phase and sex related markers     

Xiang-feng  Li  Zheng-hong  Sui  Xue-cheng  Zhang 《中国海洋湖沼学报》1998,16(1):147-151

Random amplification of polymorphic DNA (RAPD) was conducted by using 10 random primers (P-1 to P-10) inGracilaria lemaneiformis. Phase and sex specific bands were amplified by primers P-2, P-6, P-7 and P-8: for P-2 a 1.4 kb band was found in female gametophytes and tetrasporophytes, for P-6, a 0.6 kb band appeared in male gametophytes and tetrasporophytes; for P-7, a 0.76 kb band appeared in male gametophytes and tetrasporophytes; for P-7, a 0.72 kb band appeared in female gametophytes and tetrasporophytes; for P-8, a 0.73 kb band only appeared in male gametophytes.

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基于多分辨分析的滤波算法在SAR图像斑点噪声消除中的应用     

倪秀平  肖国超  万志龙 《测绘学院学报》1998,(2)

合成孔径雷达 (SAR)图像一般都存在相干噪声 ,对地物信息的提取及 SAR图像应用的干扰非常严重 ,对此许多人提出了不少处理方法 ,并分析对比了多种滤波算法 ,认为改良 K -均值自适应滤波效果最佳。本文中分析了改良 K -均值自适应滤波法的数学基础的局限性 ,并采用了一种基于多分辨分析的滤波算法 ,该算法通过将噪声 (或较小的结构特征 )与较大的结构特征相分离 ,然后滤出噪声 (或较小的结构特征 ) ,从而达到消除斑点噪声的目的。实验结果证明 ,基于多分辨分析的滤波算法在消除 SAR图像的斑点噪声方面优于改良 K -均值自适应滤波法。  相似文献   

塔里木盆地天然气运聚系统与运聚模式   总被引：7，自引：0，他引：7  

柳广弟  周兴熙 《沉积学报》1998,16(1):58-63

对塔里木盆地东部地层压力结构和天然气性质差异的研究表明,塔里木盆地东部具有多个独立的天然气运聚系统。这些运聚系统具有流体封存箱的特征。天然气只能在运聚系统内部进行短距离的运移,不能进行大规模侧向运移。因此天然气藏的形成具有近源的特点。由于不同运聚系统特征的差异,塔里木盆地大致有三种天然气运聚模式。  相似文献   

长白山望天鹅火山双峰式火山岩的成因演化   总被引：12，自引：7，他引：5  

樊祺诚  张国辉 《岩石学报》1998,14(3):305-317

望天鹅火山活动从早到晚分为三期：①长白期以粗面玄武岩为主,少量碱性玄武岩和玄武质粗安岩;②望天鹅期又分早晚两个亚期,早期玄武质粗安岩和粗面岩,晚期碱性流纹岩;③红头山期碱性流纹岩。望天鹅火山岩的岩石学、ＲＥＥ、不相容元素和Ｎｄ、Ｓｒ、Ｐｂ同位素（１４３Ｎｄ／１４４Ｎｄ、８７Ｓｒ／８６Ｓｒ、２０６Ｐｂ／２０４Ｐｂ分别变化于０．５１２５６７～０．５１２６４２、０．７０５１９８～０．７１６７４２和１７．４３４～１７．９３４）,揭示了岩浆源区明显受洋壳的俯冲和壳幔混合混染,三期火山岩具有共同的岩浆源区和紧密的成因演化关系,分离结晶作用控制了岩浆的演化过程。原始碱性系列玄武质岩浆经橄榄石、辉石的结晶分异,向粗面玄武岩演化;粗面玄武岩经斜长石强烈的结晶分离作用,还有辉石、钛铁氧化物和磷灰石的分离结晶作用形成具显著Ｅｕ、Ｓｒ、Ｂａ、Ｔｉ、Ｐ负异常的碱性流纹岩,导致本区火山岩缺失中性（ＳｉＯ２＝５７％～６３％）的安山岩和粗安岩,呈现双峰式火山岩组合的特点。  相似文献   

融合点云和多视图的车载激光点云路侧多目标识别     

方莉娜  沈贵熙  游志龙  郭迎亚  付化胜  赵志远  陈崇成 《测绘学报》2021,50(11):1558-1573

城市环境中的行道树、车辆、杆状交通设施是重要的交通地物,也是智能交通,导航与位置服务,自动驾驶和高精地图等行业应用的核心要素.为了准确识别这些路侧目标,本文提出一种融合点云和多视角图像的深度学习模型PGVNet(point-group-vi ew network),充分利用目标点云数据中空间几何信息及其多视角图像中高级全局特征提升路侧行道树、车辆和杆状设施的分类精度.为了减少视图间的冗余信息并增强显著视图特征,PGVNet模型利用预训练的VGG网络提取多视图特征,对其进行分组赋权获取最优视图特征;采用嵌入注意力机制的融合策略,利用最优视图特征动态调整PGVNet模型对点云不同局部关系的注意力度,学习不同路侧目标的多层次、多尺度显著特征,实现行道树、车辆和杆状交通设施的精确分类.试验采用5份不同车载激光扫描系统获取的不同城市场景数据验证本文方法的有效性,其中行道树、车辆及杆状交通设施分类结果中的准确率、召回率、精度和F1指数分别达(99.19％、94.27％、93.58％、96.63％);(94.20％、97.56％、92.02％、95.68％);(91.48％、98.61％、90.39％、94.87％).结果表明,本文方法融合多视图全局信息和点云局部结构特征可以有效区分城市场景中的行道树、车辆和杆状交通设施,可为高精度地图中要素构建与矢量化提供数据支撑.  相似文献   

滇西马厂箐铜钼多金属矿床成矿流体来源及演化过程——来自石榴子石原位微量元素及H- O同位素组成的限定     

吉彦冰  杜丽娟  陈军  黄智龙  李波  李鑫正  刘林林  杨再风 《地质学报》2023,97(4):1140-1156

滇西马厂箐铜钼多金属矿床位于三江特提斯成矿域,是一个与喜马拉雅期富碱斑岩侵入有关的多金属矿床。前人研究表明,马厂箐铜钼多金属矿床形成于斑岩-矽卡岩成矿系统,但由于缺乏系统矿物学研究,目前对矽卡岩矿化过程和成矿效应仍不清楚,限制了对该矿床成矿过程的全面认识。因此,本文以马厂箐矿床矽卡岩型矿化中的石榴子石为研究对象,利用H-O同位素、电子探针(EPMA)以及LA-ICP-MS原位微区技术开展了同位素及成分分析,限定成矿流体来源以及反演成矿流体演化过程。石榴子石可分为早期自形石榴子石(Grt I)和晚期他形石榴子石(Grt II)。Grt I与辉石共生,并伴有黄铁矿、黄铜矿等金属矿物组合,属于钙铝-钙铁榴石固溶体(And_{49.37～99.58}Gro_0～49.79);Grt II更富Fe,属钙铁榴石系列(And_{67.50～99.85}Gro_0～31.84)。两期石榴子石均富含Th、U、Nd,亏损Ba、Sr、Hf、Nb,富轻稀土。基于石榴子石矿物化学特征认为,Grt I可能是在弱酸性、氧化、低水岩比(W/R)条...  相似文献