长乐—南澳断裂带东山段剪切变形与剪切加热作用

本文在系统的有限应变测量的基础上,对闽东南长乐—南澳断裂带东山段剪切变形特征进行了分析:利用变形石英显微亚结构。(动态重结晶颗粒)估算了剪切带内古应力并(σ—σ_3):通过对剪切变形能密度分布W(x)格离散化计算,采用有限差分数值近方法,获得了剪切热数值解:最后总结了研究地区剪切变形,剪切加热与动热成岩成矿作用的相对时空关系以及长乐—南澳断裂域构造意义     

海南戈枕韧性剪切带微观构造研究

韧性剪切带的定性－定量分析。能更清晰、直接地揭示构造运动生发发展过程应力、应变的状况。作者对海南戈枕韧性剪切带从显微构造角度作了系统研究工作。通过矿物粒度、形态比统计，在纵横方向上更明确了内部的复杂分带性；通过显微批向构造、矿物组权及变形变晶分析了探讨了构造活动的方式、方向；通过古应力值、剪应变、总位移量、弗林系数的测算，定量表述了该带变形机制及应力、应变速率大小。     

Blockage of regional seismic waves by the Teisseyre-Tornquist zone

During the Group of Scientific Experts Technical Test (GSETT, second experiment, 22 April-2 June 1991), several hundred seismic events were located in Europe. Associating these events with the detecting stations-altogether 28 European stations including seven arrays participated in the GSETT-2 experiment-clearly shows that the Teisseyre-Tornquist Zone (TTZ) influences the propagation of regional seismic phases. Large explosions in the Bay of Gdańsk, for example, were observed by the well-established Scandinavian arrays'NORSAR (Δ 830km) and ARCESS (Δ 1650km), but not by the Polish station KSP (Δ 470km) nor by the new highly sensitive GERESS array (Δ 750km), both situated south-west of the TTZ. For events in central Europe with comparable magnitudes, we observe a similar increase of the detection threshold at stations located north-east of the TTZ in Scandinavia. to explain these observations, the wave propagation of P_n and P_g perpendicular to the TTZ was modelled for a profile from the Estonian/Russian border region to GERESS with Gaussian-beam seismograms. Published crustal and uppermost mantle models for Poland and for Europe were used as a starting point for developing a model of the TTZ. the observations cannot be explained only by a graben-like crustal structure with a jump in Moho depth from 30km to 50km. to defocus the seismic energy, the TTZ as a structural anomaly between eastern and western Europe must reach down into the upper mantle to a depth of at least about 200 km. the proposed model has such a deep-reaching root of the TTZ.     

A hypothesis for the seismogenesis of a double seismic zone

The seismogenesis of a double seismic zone, in particular the lower layer of a double seismic zone, has not been adequately explained in the literature. On the basis of seismic data and geothermal structures along three well-studied cross-sections in the Kuril-Kamchatka and Japan subduction zones, we investigate the temperature/pressure conditions associated with seismogenic structures of the double seismic zones. the corresponding T/P loci seem to suggest that earthquakes observed in the lower layer and in the lower part (below approximately 130 ± 20 km) of the top layer of a double seismic zone were caused by metastable phase transition-a mechanism similar to that responsible for deep-focus earthquakes only at lower temperature/pressure conditions. Under this hypothesis, the wedge-shaped configuration of a double seismic zone is interpreted to represent the loci of the kinetic boundary of the phase transition. According to theoretical/experimental studies and the constraints imposed by our observations, a likely candidate for such a phase transition is the metastable Al-rich enstatite decomposing into the assemblage of Al-poor enstatite plus garnet. Earthquakes in the upper part of the top layer were most probably due to conventional mechanisms such as dehydration of subducted materials and/or facies change from basalt to eclogite. That the top layer involves more than one seismogenic mechanism is also implied by the distinct behaviour of seismicity in the vicinity of 130 ± 20 km. Because the presence of deviatoric stress is critical to the reaction rate of a metastable phase transition, it is inferred that single seismic zones are also caused by the same mechanisms, except that the implicit layer of a supposed double seismic zone is missing, due to the insufficient amount of appropriate metastable minerals or to the lack of appropriate deviatoric stresses in the source region.     

内蒙古苏尼特左旗交其尔推覆构造带的发现及其地质意义

内蒙古苏尼特左旗中部交其尔一带发现一条近ＥＷ向延伸的推覆构造带。上元古界－下古生界浅变质岩以低角度向北推覆于晚古生代花岗岩基之上．推覆构造上盘的浅变质岩中发育有一套轴面向南倾的同斜倒转褶皱系，并伴有一系列向南倾的叠瓦状逆冲断面。下盘花岗岩中发育有较宽的糜棱岩带．沿推覆构造带分布有一系列的飞来峰及构造窗。这一构造带的发现，为纬向构造带的存在提供了有力证据，并显示了晚古生代末期以来地壳沿经线方向的强烈缩短。     

论民俗旅游资源的基本特征及其开发原则

富有民族特色的民俗旅游是一项具有广阔前景的旅游项目。民俗旅游资源具有世界性、地域性、集体性、增智性和封闭性等基本特征。开发利用民俗旅游资源要严格掌握和妥善运用有关的民族政策，保护民族利益；要注重发挥民俗资源特色和保护当地社会文化环境，避免盲目仿效、随意移樾和粗制滥造；要区分主次，重点开发，切忌一拥而上；要注意把当地民俗资源优势与其它景观优势结合配置，增强吸引力，提高效益。     

澜沧江中下游斜坡稳定性评价预测的理论与方法探讨

本文以澜沧江下游流域边坡稳定性评价为实例，对模糊评判模型的应用问题和处理技术进行了论述。认为该模型简便实用、效果稳健、适应性强，是边坡稳定性评价工作中适宜推广的一个实用模型。此外，文中还提出了用于模糊评判模型的信息检验法，讨论了这一方法在遴选有效评价因子和优化模型效能中的作用。     

河流污染带的随机模拟方法

根据随机理论，推导了一个描述污染带变化的概率模型，并采用Ｍｏｎｔｅ－Ｃａｒｌｏ抽样法对其求数值解。该随机模型的解是一个随机物，实例计算表明，它的解能够反映任一计算点的浓度变化趋势及范围，并能够给浓度等值线附加上概率的意义，表现了在不确定因素的影响下，污染带随机变化的情况。