郯庐断裂带莒县地区早白垩世中酸性火山岩成因及其地质意义

莒县早白垩世火山岩沿郯庐断裂带分布,由粗安岩、粗面岩和流纹岩组成,属高钾钙碱性-钾玄岩系列.岩石富集Rb、K、Ba等大离子亲石元素和轻稀土元素,相对亏损Nb、Ta、Ti等高场强元素和重稀土元素,Sr-Nd同位素组成((87Sr/86Sr)t=0.7082～0.7095,ENd(t)=-16.4～-19.8)与区内基性岩的相类似,而Pb同位素组成((206pb/204Pb)t=16.523～17.038,(207pb/204Pb)t=15.414～15.468,(208pb/204Pb)t=37.058～37.427)类似于EM1型富集地幔.(87Sr/86Sr)t和εNd(t)与SiO2没有明显的相关性,且较高的Th/U、Ce/Pb值和较低的Nb/La、Nb/U值均暗示岩浆在上升过程中未遭受明显的地壳混染.粗安岩具有高的Cr、Ni、MgO含量及Mg#值和古老Nd同位素模式年龄,暗示其起源于富集的岩石圈地幔.粗面岩与粗安岩的主要氧化物、微量元素与SiO2呈明显的相关性,这暗示可能为同源岩浆结晶分异而来.研究表明,莒县地区中酸性火山岩形成于岩石圈伸展减薄背景下,由曾遭受俯冲扬子陆壳熔体改造的华北岩石圈地幔部分熔融形成的岩浆分离结晶作用而成.郯庐断裂带的伸展活动控制着火山岩的分布,为岩浆的形成和运移提供了有利的场所,在华北克拉通破坏中可能起到了重要的作用.     

云南思茅三叠纪弧后前陆盆地的沉积特征

思茅盆地位于古特提斯构造域的东段,西侧为澜沧江造山带,东侧为哀牢山造山带.三叠纪沉积盆地建立在晚古生代褶皱基底之上,形成于古特提斯洋闭合后,造山早期的弧陆碰撞阶段.前人提出过后陆盆地、滞后型弧后盆地、裂谷盆地和前陆盆地等多种认识.本文通过对盆地形成的地球动力学背景及盆地内沉积体的性质、结构、时空叠置关系、古流向、特殊沉积体的时空展布及其所表现出的盆地沉降中心的迁移规律等方面的系统研究,认为思茅三叠纪盆地属弧后前陆盆地,其演化阶段始于中三叠统安尼期以前,盆地主要受控于澜沧江造山带,晚三叠世晚期受哀牢山造山带影响,具有复合式前陆盆地特点,三叠纪末过渡为陆内拗陷盆地。     

江苏省1∶25万、1∶100万基础数据修测与建库

1∶25万、1∶100万基础数据是江苏省地理空间信息基础框架的重要组成部分,本文根据江苏省地理空间信息基础框架的要求,结合全省现有的基础地理数据库建设的现状,叙述了对全省范围内的17幅1∶25万DLG、DOM,4幅1∶100万DLG数据如何进行修测、更新和入库,并建立相应的元数据库的过程和方法。     

基于Boussinesq水波模型的聚焦波模拟

基于最高导数为3阶的单层Boussinesq方程,建立了聚焦波的时域波浪计算模型。数值模型求解采用了预报−校正的有限差分法。对于时间差分格式,预报和校正分别采用3阶Adams-Bashforth格式和4阶Adams-Moulton格式。首先,针对不同水深条件下水槽中传播的强非线性波进行模拟,并将数值结果与流函数的数值解析解进行了比较,结果表明无论是波面位移、波面处的水平速度和垂向速度均与解析解符合较好,最大波峰面的速度分布伴随水深的增加与解析解吻合程度变差,非线性速度分布的适用范围与线性解析解适应范围kh<3.5基本一致。其次,对深水聚焦波演化进行了模拟研究,研究中聚焦波的生成采用在边界点累加不同频率线性规则波的方法。应用聚焦波物理模型实验结果验证模型,计算聚焦位置处的波面位移和沿水深的速度分布与实验结果的对比表明,波面位移吻合程度较好,垂向的水平速度分布基本吻合。最后,保持中心频率(周期)不变,数值模拟了周期范围变化下最大聚焦波峰面以及波峰面水平速度的变化趋势,结果表明波峰面值和波峰面水平速度随着周期范围缩小而增大。     

南岭金鸡岭岩体锆石U-Pb年龄、地球化学特征及地质意义

对南岭九嶷山地区金鸡岭岩体开展LA-ICP-MS锆石U-Pb年代学研究,结果显示主体粗中粒似斑状正长花岗岩和补体细粒斑状二长花岗岩的成岩年龄分别为156.40±0.66 Ma、153.00±2.20 Ma;结合已有资料将二者的形成时代约束在(156.40±0.66)～(159.00±0.45)Ma与(146.00±0.86)～(153.0±2.2)Ma之间;确定其成岩年代同为燕山早期,也明确了两者的形成顺序.岩石地球化学研究表明,金鸡岭岩体整体具有富硅、碱,贫钙、镁,准铝-过铝质(A/KNC=0.97～1.14)等特点;主体岩性稀土含量较补体明显偏高,分别为488.63×10^-6～571.67×10^-6和166.33×10^-6～275.51×10^-6,(La/Yb)_N分别为10.27～15.84、0.38～1.13;前者稀土元素配分曲线呈右倾轻稀土富集型,而后者则无明显轻、重稀土分馏;两类花岗岩的δEu值都很低,分别为0.049～0.063、0.003～0.007,为铕亏损型;...     

基于MicroStation环境的图形编辑系统的开发

研究了利用MicroStation95开发图形编辑系统、定制用户界面和自动建立地形图符号库的方法和技术。介绍了具体操作中的一些经验和技巧。     

Three-Dimensional Refined Modelling of Deep Structures by Using the Level Set Method: Application to the Zhaoping Detachment Fault,Jiaodong Peninsula,China

Mathematical Geosciences - The construction of fine-scale three-dimensional models of deep structures at a regional scale remains challenging. These models can be significantly benefitted by...     

THE STATISTICAL DISTRIBUTION OF THE SPATIAL MAXIMA OF A WAVY SEA SURFACE

A statistical distribution of the maxima of a random function in two space variables is suggested to fit with stereo observations of the sea surface. The presented distribution is a complicated mix of Gaussian, Rayleighian and Maxwellian distributions and determined by three parameters of the directional spectrum, According to the changes of the three parameters it may approach the above three distributions respectively in special cases so that it has more probability of fitting stereo data better In addition, the fact that these parameters can be directly estimated from observed data is briefly in the paper.     

Period of Light Variability in BL Lac ON 231

In this paper, the authors have compiled the data of about 100 years in B-band of the BL Lac ON 231 and used this database to analyze periodicity signals in the optical light curve. Two different methods were applied: the wavelet analysis and the Discrete Correlation Function (DCF) method. We revealed the existence of periods of 13.5 years in the source variability.     

Unusual Zebra Patterns in the Decimeter Wave Band

An analysis of new observations showing fine structures consisting of narrowband fiber bursts as substructures of large-scale zebra-pattern stripes is carried out. We study four events using spectral observations taken with a newly built spectrometer located at the Huairou station, China, in the frequency range of 1.1 – 2.0 GHz with extremely high frequency and time resolutions (5 MHz and 1.25 ms). All the radio events were analyzed by using the available satellite data (SOHO LASCO, EIT, and MDI, TRACE, and RHESSI). Small-scale fibers always drift to lower frequencies. They may belong to a family of ropelike fibers and can also be regarded as fine structures of type III bursts and broadband pulsations. The radio emission was moderately or strongly polarized in the ordinary wave mode. In three main events fiber structure appeared as a forerunner of the entire event. All four events were small decimeter bursts. We assume that for small-scale fiber bursts the usual mechanism of coalescence of whistler waves with plasma waves can be applied, and the large-scale zebra pattern can be explained in the conventional double plasma resonance (DPR) model. The appearance of an uncommon fine structure is connected with the following special features of the plasma wave excitation in the radio source: Both whistler and plasma wave instabilities are too weak at the very beginning of the events (i.e., the continuum was absent), and the fine structure is almost invisible. Then, whistlers generated directly at DPR levels “highlight” the radio emission only from these levels owing to their interaction with plasma waves.