P-Ⅲ型分布混合权函数估计法的研究

为克服传统的马秀峰权函数法所存在的缺陷，提出了一种可考虑线性矩法优点的新的权函数估计法即混合权函数法，经过统计试验验证，该法对传统的马秀峰权函数法有较大改进，是一种统计性能较优秀的参数估计方法。     

自然电场法在寻找层间氧化带型砂岩铀矿中的应用

介绍了自然电场形成的原理及在寻找层间氧化带砂岩型铀矿中的应用.根据氧化带与还原带的自然电位变化特征,利用自然电场法可以确定盆地层间氧化带前锋线,由此推测层间氧化带砂岩型铀矿大体空间位置.     

2003年新疆石河子5.4级地震前地震活动异常分析

分析了2003年2月14日石河子5．4级地震前北天山地震活动图像和地震学参数异常过程。5．4级地震发生在2002年北天山4级地震集中活动区空段，震前12项地震学参数时间进程存在中、短期异常，3项地震波参数出现短期异常。震前3个月乌鲁木齐震情窗出现超警戒线异常。震前10天震中附近地区地震和震群活动显著。     

岫岩-海城5.4级地震前小震震源机制解与记录特征分析

采用Pn、Pg初始波初动符号，利用乌尔夫网上半球投影，用作图方法求解了岫岩－海城震区（1999年1月－1999年11月29日）主震前辽宁数字地震台网记录（ML≥2.5)的41个小震的震源机制参数。结合前震记录的某些特征，对主震前应力方向的时空变化，震源错动性质进行分析和讨论。     

1995年日本新泻北部M6.0地震及其由地震烈度和地下水地热异常分布所揭示的隐伏地震断层

1995年日本新泻北部M6.0地震发生在新泻地震空区的东部边缘.由于此次地震震源较浅(10 km),造成了55栋房屋倒塌、165栋房屋半倒.通过计算倾倒墓碑的地震矩,对本区地震烈度进行了分析,发现烈度6度区(据日本JMA度)为一覆盖面积6.1×1 km2,呈NNE-SSW向分布的条带,表明震中区的冲积平原下存在一条隐伏断层.震中区地下水的温度、电导率和Cl-浓度等异常区与呈线性分布的6度烈度区大致吻合,也有力地证明了震中区下面存在一条隐伏断层.这次地震可能是由高压型热水系沿隐伏活动断层喷溢引起.带着高温的高压热水降低了岩石的断裂强度,从而触发了地震.     

俯冲-增生型造山带增生楔流体研究进展

俯冲－增生型造山带弧前增生楔流体的特点为：盐度低、氯化物含量异常低，并含有丰富的CO2和CH4。流体以扩散式或沿断层带渠道式活动；泥火山、张裂隙充填脉、碳酸盐壳、深海生物群是流体活动的直接体现；流体活动影响着增生楔的内部结构和构造样式；增生楔中流体活动特征的研究对研究造山带的地质演化及矿床成因具有重要意义。     

湖南郴州南风坳银矿床银的赋存状态及分布规律

南风坳银矿是产于震旦系浅变质碎屑岩中受北北东—北东向断裂控制的热液充填交代型矿床。矿床中银主要以银矿物存在，次为类质同像。银的载体矿物主要为方铅矿，次为铁闪锌矿、黄铜矿、黄铁矿、毒砂等。已查明的银矿物15种，常见的10种，主要的银矿物为银黝铜矿和黝锑银矿，它们多呈显微包体分布在载银矿物中。银在矿区中部(03-17线)980m～1036m标高范围内富集。银与铅关系密切，银在富铅矿体中富集。     

Study of crustal structure with S—wave data from Maqen—Jingbian profile

2-D crustal velocity structure and vp/vs are obtained by processing and interpretation of S-wave data from Maqen-Jingbian deep seismic sounding(DSS)profile.The result shows that there exist obvious differences in 2-D S-wave velocity structure and vp/vs ratio structure along the profile.The S-wave velocities are low and vp/vs ration is high for the westem section of the profile and Haiyuan region,while they are normal for the middle and eastern sections.The changes in lithologic characters of two major anomalous zones are discussed according to lateral variation of S-wave velocity structure and vp/vs ratio structure.It is concluded that the development and occurrence of the Haiyuan strong earthquake is not only related to tectonic activities,but also to lithologic characters of the region.     

Crustal structure beneath the Songpan—Garze orogenic belt

The Benzilan-Tangke deepseismic sounding profile in the western Sichuan region passes through the Song-pan-Garze orogenic belt with trend of NNE.Based on the travel times and the related amplitudes of phases in the record sections,the 2-D P-wave crustal structure was ascertained in this paper.The velocity structure has quite strong lateral variation along the profile.The crust is divided into 5layers,where the first,second and third layer belong to the upper crust,the forth and fifth layer belong to the lower crust.The low velocity anomaly zone gener-ally exists in the central part of the upper crust on the profile,and it integrates into the overlying low velocity basement in the area to the north of Ma‘erkang.The crustal structure in the section can be divided into 4parts:in the south of Garze-litang fault,between Garze-Litang fault and Xianshuihe fault,between Xianshuihe fault and Longriba fault and in the north of Longriba fault,which are basically coincided with the regional tectonics division.The crustal thickness decreases from southwest to northeast along the profile,that is ,from62km in the region of the Jinshajiang River to 52km in the region of the Yellow River.The Moho discontinuity does not obviously change across the Xianshuihe fault basesd on the PmP phase analysis.The crustal average velocity along the profile is lower,about 6.30 km/s.The Benzilan-Tangke profile reveals that the crust in the study area is orogenic.The Xianshuihe fault belt is located in the central part of the profile,and the velocity is positive anomaly on the upper crust,and negative anomaly on the lower crust and upper mantle.It is considered as a deep tectonhic setting in favor of strong earthquake‘s accumulation and occurrence.     

俄罗斯贝加尔湖-日本石卷地学断面西段地质-地球物理基本特征

对于贝加尔湖-石卷地学断面(BAMSIP)的西段俄罗斯贝加尔湖-中国满洲里断面城内的地质构造背景、地震剖面波类型和基本特征等研究发现：(1)断面域中贝加尔裂谷带地震波速度结构存在异常地幔带；结晶地壳物质成分基性程度较高；基底顶面和Moho界面未观察到明显的镜象关系；(2)西伯利亚南部的复杂相故基底由古生代和前寒武纪岩层所组构；区域构造由古褶皱系、中生代沉积盆地、裂谷带构成。