钦杭成矿带东段燕山期中酸性岩浆活动时空演化与成矿规律

钦杭成矿带东段处于华夏地块与扬子地块的交接部位,其特殊的构造背景造就了其独特的岩浆事件与成矿作用。本文详细总结了燕山期中酸性岩浆时空演化与成矿规律,认为钦杭成矿带东段燕山期岩浆活动是连续的,可分为"两期四阶段":早期早阶段(180~160Ma)主要形成I型花岗岩,早期晚阶段(160~145Ma)形成I型、S型花岗岩,晚期早阶段(145~125Ma)以形成S型花岗岩为主(136Ma之后开始形成A型花岗岩),晚期晚阶段(125~100Ma)主要形成A型花岗岩。以东乡-德兴I型花岗岩带为岩浆活动中心,总体经历了从西往东,从I型→S型→A型的演化过程。按成矿专属性,将I型花岗岩分为两种类型:I_1型花岗岩以形成铜(金)铅锌铁多金属矿床为特色,I_2型花岗岩主要形成钨钼矿;将S型花岗岩分为三类:S_1型花岗岩主要形成钨锡钼矿床,高分异的S_2型花岗岩形成铌钽矿,S_3型花岗岩主要形成铅锌银铀矿床;A型花岗岩则具备I型、S型两种花岗岩的成矿特征。与岩浆作用一致,成矿作用也是连续的,可分为相应的"两期四阶段"。成岩成矿的时空演化过程主要受太平洋板块俯冲过程中动力条件变化的控制,导致不同部位的基底地层发生熔融,发生不同程度的壳幔相互作用。     

基于MGS探测器掩星观测的火星电离层数据初步分析

该文简要介绍了行星无线电掩星技术的意义、历史和原理.利用MGS探测器无线电科学掩星实验得到的火星电离层电子浓度EDS数据,可研究火星电离层的结构.文中分析了MSG电子浓度廓线的峰值高度随经度的变化特性,并结合火星电离层的Chapman模型和实测的电子浓度廓线,探讨了火星电离层的双层或多层结构的可能性及其物理机制.分析了峰值电子浓度和峰值高度同太阳天顶角的关系和TEC在各数据集中的分布.     

重力卫星检测到的全球陆地水储量变化

利用GRACE时变重力位模型反演了2004年至2008年共60个月的全球陆地水存储量变化,并采用滑动年平均,对全球陆地水储量的长期性变化情况进行了分析,同时也推求了全球陆地水储量的季节性变化。研究表明,使用滑动年平均对GRACE重力位模型数据进行处理,可以较好地揭示全球陆地水储量的长期和季节性变化情况,其监测能力足以揭示几cm的等效水高变化。     

国外规划实施评价理论与方法及其在国内应用的研究进展

在我国,修编土地利用总体规划、城市总体规划之前,开展对现行规划实施情况的评价,已经纳入规范的工作程序,与之相应,规划实施评价研究逐渐成为关注的焦点。该文首先对国外规划实施评价理论与方法进行简要的介绍,再对国内开展的实证研究进行归纳分类,并做出简要评述,以期为今后的规划实施评价研究提供一些新的视角和参考。     

The quiescence of earthquakes with ML34.0 as an important precursory characteristic prior to strong shocks in North China region

Before a strong earthquake, there is often a process of quiescence or 2absence2 of regional seismic activity, which is a phenomenon that has attracted the attention of many scholars in China and other countries (LU, et al, 1985; Wesson, 1973). In the past ten-odd years, some Chinese seismologists made, earlier or later, special studies on the quiescence anomaly of seismicity in some specified areas from different angles. Taking the converted annual frequency of M=5.0 earthquakes in North China region as a characteristic quantity, JIANG and FENG (1989) analyzed the quiescence anomaly of seismic activity by fuzzy recognition.     

Current crustal motion and deformation in the Chinese mainland and its surrounding area determined from GPS data

Based on the geodetic data taken from the National GPS Network established by China Climbing Program "Investigation of Crust Motion and Geodynamics in Modern Time",we derived the movement velocities of the GPS sites. In terms of the power series expansion of a rotation function for horizontal velocities on a spherical surface proposed by Haines and Holt (1993), we computed the horizontal velocity and strain-rate field. We preliminarily studied the appearances and characteristics of the present-day crustal movement and deformation in the Chinese mainland with the computed results. The researches demonstrated: ① The present-day crustal movement and deformation in the Chinese mainland are being jointly controlled by Indian, Pacific and Philippines Ocean Plates and Siberia-Mongolia block, and these three large plates and block form a situation of tripartite confrontation, but Indian Plate seems to play a leading role; ② The North-South Earthquake Zone plays an important adjustment role in the present-day crustal movement and deformation process, displaying clear characteristics of demarcation line of tectonics in large areas; ③ There seems to be another adjustment zone along the latitude line approximate N35°, but its characteristics are less obvious than that of the former; ④ Dynamic actions of these three large plates and block on the Chinese mainland are dynamic stable; appearing in stable push-press velocities. These results are generally accorded with the results determined from geology, geophysics, and seismology. By the contrast with seismicities, it appears preliminarily that there is some corresponding relation between intense shear strain zone and future strong seismicity area, but this problem needs further examination of earthquake examples.     

增厚大陆岩石层热边界层对流剥离的数值模拟

用数值模拟方法模拟了增厚大陆岩石层热边界层被对流地幔剥离并为软流层物质替代的动力学过程．结果表明,在初始温度分层分布、侧向均匀但存在微小热扰动的流场中,80km厚的增厚岩石层热边界层约需60Ma才能被完全剥离,剥离的速率微弱地依赖扰动的强度;在已建立好的流场中,同样厚度的增厚热边界层只需约10Ma就可被剥离．模拟结果暗示青藏高原地壳及岩石层在岩石层增厚和剥离以前就很热,其下伏地馒中可能已存在建立好的上地幔小尺度对流系统,而该尺度的对流系统很可能是由特提斯海洋岩石圈俯冲和消减诱发的     

点力源在横向各向同性介质中激发的弹性波

点力源在均匀横向各向同性介质中激发的弹性波可以用透射-反射矩阵法进行求解。假定点力源位于一假想的各向同性层中,并利用各向同性介质中等效于势函数的过源面间断,从而易于求出介质中各个点上的弹性波场;再令假想的各向同性层的厚度趋近于0,则可求出原始问题的解,即横向各向同性介质中的格林函数。最后得出的结果和假想的各向同性层的性质无关,表明这一方法用于求解点力源在各向异性介质中激发的弹性波场是可行的。     

用图像质量评价量实现的真实图像和计算机生成图像的鉴别方法

真实图像和计算机生成图像的鉴别是数字图像盲取证中的一个重要问题。提出了一种真实图像和计算机生成图像的鉴别方法。借用模式识别中的二分类概念,采用图像质量评价量来建立模型,以捕获真实图像和计算机生成图像的统计差异,选用支持向量机作为分类器进行训练和测试。实验结果表明,该方法计算方便、实用性强、可靠性高。     

地震前兆多尺度综合信息函数及其初步应用

本文基于经验模态分解技术,构造多尺度地震前兆异常提取的综合信息函数,获得多尺度信息量。首先介绍了该方法的技术思路,然后通过对前兆时间序列进行经验模态分解,在各阶IMF和重构时序基础上计算其信息量,最后通过震例分析表明,该方法是有效的,思路是可行的,处理结果也是有意义的。