线性连续变化非弹性介质中地震波射线轨迹与走时研究

地球内部非弹性介质广泛存在,垂向线性连续变化非弹性介质模型具有重要理论与实际意义,本文利用复速度概念推导得到了复速度随深度线性连续变化的非弹性介质中地震波射线轨迹与等时线方程.理论结果表明:在线性连续变化非弹性介质中,射线轨迹呈圆形,等时面的形状为椭圆.最后对射线轨迹与等时线方程的适用性条件进行了讨论.     

新疆塔城地区地震地质特征

托里活断层、达尔布特活断层、独山子—安集海活断层及霍尔果斯—卡子湾活断层是塔城地区主要的全新世活断层，均有过多次古地震活动。自１９７７年以来，４级以上地震活动的空区在裕民县西北。据活断层古地震活动复现期及地震活动围空特点分析，今后１０年北天山或塔城西北可能有发生６级左右地震的危险。     

前兆起伏加剧与短临地震预报

起伏加剧是相态突变前的一种临界现象,本文应用这一观点探讨了强地震前小震活动频次和地下流体、气体、地应力等前兆变化的起伏加剧现象,并得到以下初步结果: 1.临近强地震前较大范围内超过平均日活动水平的小震活动的空间分布具有有序性,即出现穿过未来大震区的小地震活动条带,条带的交汇区为未来大震区。2.强地震前的小震高频次活动日大多与外因出现时间同步,目前发现的外因有塑望、节气、中强以上磁暴以及大气压力下降等。这种小震的高频次活动一般出现在震前当天至一个月时间内。3.前兆的起伏时间和小震频次的起伏时间大致同步。它们在成因上有联系。     

K-Ar isotopic geochronology of Lianhuashan tungsten mining district,Guangdong Province

Reported in this paper are K-Ar ages of volcanic rocks, biotite-granite and greisen from the Lianhuashan tungsten mine in Guangdong Province. The isotopic dilution method was adopted in this work. Whole-rock isochron ages of the volcanic rocks are in the range 120.4±12.1 m.y. The petrogenetic age of biotite-granite and the minero genetic age of tungsten ore are close to those of the volcanic rocks. The apparent ages of various types of rock in the mining district generally bias towards younger values, which may be attributed to the effects of late thermal events which took place in the circum-Pacific metallogenetic belt.     

甘肃天水地区1654年罗家堡7(1)/(2)级地震构造背景的初步分析

本文从分析天水地区区域地质构造背景出发着重指出,1654年罗家堡7(1/2)级地震发生在天礼盆地中北东向构造与北北西向活动构造交汇所形成的新生代以来沉陷最深的部位。并对1936年天水镇6级地震发生的构造条件以及天礼盆地的成因进行了初步探讨。     

On the conditions of formation of Gushan iron ore deposit

On the basis of its geological characteristics, the Gushan iron deposit should be assigned to volcano-hydrothermal type with hematite-quartz as its principal mineral assemblage. Iron concentration of the ore solution has been estimated from the ratio of hematite to quartz in the ore. By using experimental and thermodynamic data, the solubility of ferro-minerals at elevated temperatures and pressures have been calculated in the system FeO?Fe₂O₃?NaCl?HCl?H₂O. The effects ofT, P, pH,f _{O 2} and total Cl concentration on the solubility of ferrominerals are discussed. Thermodynamic calculations based on presumed physico-chemical conditions for the ore solution are in good agreement with geological observations. The calculation shows that ferro-minerals were deposited at logf _{O 2}=?21～?25, log(m_HCl+m_H+)=?2.5～?3,P=1?0.75 (or 0.5) kb, andT=400°?350°C. It is believed that the original solution was an acid NaCl-bearing solution of magmatic derivation. However, iron in the solution was enriched with falling temperatures by dissolving pre-existing ferro-minerals in consolidated rocks rather than extracting directly from the magma. Either temperature (below 400°C) or pressure decrease may result in the precipitation of ferro-minerals from the solution, but the Fe/Si ratio in the ore is dependent mainly upon pH. The widespread siliceous veins of later stages are a reflection of decreasing acidity of the solution. An increase inf _{O 2} will also favor the deposition of ferro-minerals. The hypabyssal occurrence and the existence of the Huangmaqing sandy shale have contributed greatly to the formation of hematite.     

机载热红外扫描在岩溶水文地质中的应用

<正> 由地面资料评价一个地区地下水的排泄地段,已经有了一套比较成功的方法。然而,地面方法相对来说所需要的时间长,花钱多,尤其是在那些交通不便,人们难以到达的地区。四十年代以来,随着航空地质工作的发展,借助于航空摄影所提供的地形、植被类型、地层产状以及破裂等资料来分析地下水的补给和排泄关系。     

当代造山带研究中值得重视的若干前沿问题

当代造山带研究正从以往以阐明板块运动历史和板块边界相互作用为主，转向并进入到了阐明造山带岩石圈及其之下地幔系统中各层圈相互作用过程和动力学的新阶段，大陆动力学正成为造山带研究的主要指导思想。在这种形势下，造山带研究正围绕着下列前沿问题展开工作：（１）碰撞后的造山过程：拆沉作用、伸展垮塌和深变质岩剥露；（２）造山带之下地幔的结构和演化；（３）壳内软层的性质和动力学作用；（４）造山带地壳的精细构造和演化；（５）巨量花岗岩的成因和侵位动力学；（６）沉积作用与造山过程：根据沉积特征对造山过程、造山事件的恢复再造；（７）新元古代超大陆。     

A CASE OF MESOSCALE CONVECTIVE COMPLEX EVOLVING INTO A VORTEX

A case of mesoscale convective complex(MCC)which evolved into a vortex is documented in this paper.As theMCC entered into the dissipating phase,a well-defined spirally banded structure became visible in the satellite image.The blackbody temperature(TBB)of the residual cold-cloud-shield indicates the vortex existed in the layer from 400 to250 hPa.According to the upper air analysis,the upper level vortex was an anticyclone.The MCC-generated vortex wasvisualized in the satellite images because it was located in the subtropical high where the wind field was very weak.     

A CASE OF MESOSCALE CONVECTIVE COMPLEX EVOLVING INTO A VORTEX*

A case of mesoscale convective complex(MCC) which evolved into a vortex is documented in this paper.As the MCC entered into the dissipating phase,a well-defined spirally banded structure became visible in the satellite image.The blackbody temperature(TBB) of the residual cold-cloud-shield indicates the vortex existed in the layer from 400 to 250 hPa.According to the upper air analysis,the upper level vortex was an anticyclone.The MCC-generated vortex was visualized in the satellite images because it was located in the subtropical high where the wind field was very weak.