云南个旧似长石正长岩类及其岩石成因     

王宇菲  董国臣  陈薇  苏麟  殷国栋  朱红运  李华伟 《地学前缘》2019,26(4):209-220

云南个旧碱性岩体主要的岩石类型有碱性正长岩和似长石正长岩,其中,似长石正长岩中出现大量似长石矿物霞石、方钠石和碱性暗色矿物。本文根据矿物成分及特征,将这些似长石正长岩进一步划分为黑榴霞石方钠正长岩、霞石方钠正长岩、霞石正长岩及方钠霞石正长岩4类。岩石地球化学结果表明,4类岩石的地球化学行为整体表现出过碱质岩的特征,K2O+Na2O含量很高,为钾玄岩系列,同时表现出钾质的特点。分异指数高,呈现高度分异演化特点。稀土元素变化大,轻重稀土元素分异明显,富集轻稀土元素,亏损重稀土元素。微量元素富集大离子亲石元素Th、U及Zr、Hf等高场强元素,亏损Ba、Sr大离子亲石元素,而P和高场强元素Ta、Ti亏损,同时Cr、Co、Ni含量非常低,具有中等的负Eu异常和微弱的负Ce异常。研究表明,似长石正长岩在岩浆演化过程中表现出明显的分离结晶作用特征,且岩浆起源温度较高,约为835℃,起源较深。个旧似长石正长岩为A型岩套A1亚型,结合构造判别图解,认为其可能来自角闪石或者金云母相矿物存在的富集地幔,形成于燕山晚期伸展的构造背景,岩浆在较高温度下高度结晶分异,并在侵位过程中伴随陆壳成分的混染。  相似文献   

层间隔震结构工作机理研究   总被引：17，自引：2，他引：15  

祁皑  林云腾  郑国琛 《地震工程与工程振动》2006,26(4):239-243

本文建立了层间隔震结构动力分析模型,对层间隔震结构地震反应的主要影响系数进行了分析。结果表明:在一定的频率比范围内,当隔震层的位置较高时,隔震结构下部位移和上部加速度均显著减小,表现出与TMD相似的工作机理;当隔震层的位置较低时,隔震结构下部位移和上部加速度均变化不明显,其工作机理与基础隔震相似。隔震层的阻尼比对层间隔震结构的减震效果也有较大影响,阻尼比越大,减震效果越好。  相似文献   

西藏过铝花岗岩的岩石化学特征及成因探讨   总被引：7，自引：1，他引：6  

廖忠礼  莫宣学  潘桂棠  朱弟成  王立全  耿全如  赵志丹  熊兴国  董国臣 《地质学报》2006,80(9):1329-1341

西藏班公湖—改则—安多—怒江带一线以南分布有61个主要过铝花岗岩体,其岩石类型主要有电气石花岗岩、白云母花岗岩和二云母花岗岩,它们的主量元素组成为SiO2=65.70%~79.52%、K2O Na2O=2.20%~12.51%、K2O/Na2O=0.49~1.04及A/CNK=1.04~1.38。随着SiO2的增加,岩石中Al2O3逐渐下降,而其他的氧化物较离散。岩石系列主要为含钾较高的钙碱性系列,具典型的(强)过铝花岗岩特征。铝饱和指数图解、QAP图解投点大多数落在CCG区,表明其为大陆碰撞构造环境。Ab-Or-Q-H2O相图表明过铝花岗岩形成的压力为0.05~0.2GPa,推断温度低于700℃。根据岩石化学分析,可以得出这样的推论,西藏过铝花岗岩类发生在两个大陆地壳板块的碰撞阶段,源岩来源于上地壳的重熔,成因为S型花岗岩。其中南冈底斯带和拉轨岗日带具有许多相似的性质,这些相似的性质可能暗示二者有相同的岩浆源区或(和)相同的构造环境。  相似文献   

Mantle Input to the Crust in Southern Gangdese, Tibet, during the Cenozoic: Zircon Hf Isotopic Evidence     

Mo Xuanxue  Dong Guochen  Zhao Zhidan  Zhu Dicheng  Zhou Su  Yaoling Niu 《中国地质大学学报(英文版)》2009,20(2)

The Quxu (曲水) complex is a typical Intrusive among the Gangdese batholiths. Two sets of samples collected from the Mianjiang (棉将) and Niedang (聂当) villages in Quxu County, Including gabbro, mafic micro-enclaves (MME), and granodiorites in each set, were well dated in a previous SHRIMP zircon U-Pb analysis (47-51 Ma). In this article, the same zircons of the 6 samples were ap-plied for LA ICP-MS Hf isotopic analysis. The total of 6 samples yields 176Hf/177Hf ratio ranging from 0.282 921 to 0.283 159, corresponding to εHf(t) values of 6.3-14.7. Their Hf depleted-mantle modal ages (TDM) are in the range of 137-555 Ma, and the zircon Hf isotope crustal model ages (TDMC) range from 178 to 718 Ma. The mantle-like high and positive εHf(t) values in these samples suggest a mantle-dominated input of the juvenile source regions from which the bathollth originated. The large varia-tions in εHf(t) values, up to 5-e unit among zircons within a single rock and up to 15-e unit among zir-cons from the 6 samples, further suggest the presence of a magma mixing event during the time of magma generation. We suggest that the crustal end-member involved in the magma mixing is likely from the ancient basement within the Lhasa terrane itself. The zircon Hf isotopic compositions further suggest that magma mixing and magma underplating at about 50 Ma may have played an important role in creating the crust of the southern Tibetan plateau.  相似文献   

热红外港口图像特征的评估器提取与选择     

马兰  陈筱勇  邓国臣 《测绘科学》2017,42(5)

针对低对比度、条纹噪声、低空间分辨率等特点而导致的热红外图像识别效果不佳问题,提出了一种港口目标热红外遥感图像特征提取与选择方法,实现了一定情况下港口目标的高精度分类。采用纹理、几何等29个特征,通过评估器选择最佳特征组合,并根据识别精度选择最佳分类器,能生成热红外图像港口目标22个最佳分类特征,且具有一定的鲁棒性。经过参数优化后的libSVM(一种支持向量机)分类器分类精度较高;白天图像比夜间图像分类精度更高;像素值、灰度直方图相关的一维和二维统计特征、局部二进制模式特征、边缘方向直方图特征等与灰度和纹理相关的特征对港口目标热红外图像识别影响较大。  相似文献   

果蝇算法优化的广义回归神经网络在变形监测预报中的应用     

范良  赵国忱  苏运强 《测绘通报》2013,(11):87-89,92

简要介绍广义回归神经网络,基于果蝇优化算法,对广义回归神经网络的平滑因子进行优化。利用神经网络工具箱,对某煤仓的沉降变形观测数据进行分析和计算,采用优化后的网络建立变形预测模型,使用相关数据来训练和测试该模型的可靠性和可行性。结果表明,果蝇算法优化的广义回归神经网络能很快找到合适的平滑因子并对变形数据进行有效预报。  相似文献   

Petrogenesis of the earliest Early Cretaceous mafic rocks from the Cona area of the eastern Tethyan Himalaya in south Tibet: Interaction between the incubating Kerguelen plume and the eastern Greater India lithosphere?     

Dicheng Zhu  Xuanxue Mo  Guitang Pan  Zhidan Zhao  Guochen Dong  Yuruo Shi  Zhongli Liao  Liquan Wang  Changyong Zhou 《Lithos》2008,100(1-4):147-173

The relationship between the breakup of eastern Gondwanaland and the Kerguelen plume activity is a subject of debate. The Cona mafic rocks are widely exposed in the Cona area of the eastern Himalaya of south Tibet, and are studied in order to evaluate this relationship. Cona mafic rocks consist predominantly of massive basaltic flows and diabase sills or dikes, and are divided into three groups. Group 1 is composed of basaltic flows and diabase sills or dikes and is characterized by higher TiO₂ and P₂O₅ content and OIB-like trace element patterns with a relatively large range of Nd(T) values (+ 1.84 to + 4.67). A Group 1 diabase sill has been dated at 144.7 ± 2.4 Ma. Group 2 consists of gabbroic sills or crosscutting gabbroic intrusions characterized by lower TiO₂ and P₂O₅ content and “depleted” N-MORB-like trace element patterns with relatively higher, homogeneous Nd(T) values (+ 5.68 to + 6.37). A Group 2 gabbroic diabase dike has been dated at 131.1 ± 6.1 Ma. Group 3 basaltic lavas are interbedded with the Late Jurassic–Early Cretaceous pelitic sediments; they have compositions transitional between Groups 1 and 2 and flat to slightly enriched trace element patterns. Sr–Nd isotopic data and REE modeling indicate that variable degrees of partial melting of distinct mantle source compositions (enriched garnet–clinopyroxene peridotite for Group 1 and spinel-lherzolite for Group 2, respectively) could account for the chemical diversity of the Cona mafic rocks. Geochemical similarities between the Cona mafic rocks and the basalts probably created by the Kerguelen plume based on spatial–temporal constraints seem to indicate that an incubating Kerguelen plume model is more plausible than a model of normal rifting (nonplume) for the generation of the Cona mafic rocks. Group 1 is interpreted as being related to the incubating Kerguelen plume–lithosphere interaction; Group 2 is likely related to an interaction between anhydrous lithosphere and rising depleted asthenosphere enriched by a “droplet” originating from the Kerguelen plume, while Group 3 may be attributed to thermal erosion resulting in the partial melting of lithosphere during the long-term incubation of a magma chamber/pond at a shallow crustal level. The Cona mafic rocks are probably related to a progressively lithospheric thinning beneath eastern Gondwanaland from 150–145 Ma to 130 Ma. Our new observations seem to indicate that the Kerguelen plume may have started its incubation as early as the latest Jurassic or earliest Cretaceous period and that the incubating Kerguelen plume may play an active role in the breakup of Greater India, eastern India, and northwestern Australia.  相似文献   

某油田地下水污染特征及其机理分析   总被引：1，自引：0，他引：1  

陈鸿汉  任仲宇  刘荣芳  刘菲  张国臣 《地学前缘》2008,15(4):178-185

在对某油田石油类污染物分布特征研究的基础上,对其进入地下水的途径进行分析。研究表明,除石油类外,CODMn、Cl-、NO3-N和TDS具异常变化,这些异常变化已成为石油类污染的参考指标。含水层污染程度主要以严重污染和中度污染为主,下段含水层中的石油类污染物的浓度明显高于上段含水层。地下水遭受污染的途径类型分为地表渗透型和优势通道渗漏型,但地表渗透型污染对研究区地下水的威胁性相对来说较小。由构造活动、地下水开采引发的地裂缝形成的优势通道渗漏型污染是地下水污染的主要途径。  相似文献   

公路涎流冰的成冰机理与新型防治措施研究     

张浩  折学森  鲁中举 《冰川冻土》2015,37(6):1571-1578

建立了粗、细粒土冻结模型, 分析了扰动三层体内部的析冰原理, 提出密闭水体的冻结-压力循环, 该循环是涎流冰发育的机理. 对饱水粗颗粒土与饱水细颗粒土的冻结模型比较表明, 饱水粗粒土在密闭体系中的冻结; 就其产生的水压力而言, 实质上就是密闭水体的冻结, 也就是水冻结成冰体积膨胀受限而产生力的问题. 这种体积膨胀产生的力导致约束结构(如薄弱层)的整体性破坏. 在公路边坡数值模拟分析的基础上, 提出边坡薄弱层破坏导致渗水是形成坡积冰的主要原因之一, 薄弱层破坏处是病害最严重的位置. 根据病害形成原理和成因分析, 并提出渗井与仰斜式排水管相结合的复合防治措施, 工后效果良好.  相似文献   

Geofluid Discrimination Incorporating Poroelasticity and Seismic Reflection Inversion   总被引：4，自引：0，他引：4  

Zhaoyun Zong  Xingyao Yin  Guochen Wu 《Surveys in Geophysics》2015,36(5):659-681

  相似文献