断层气氡测量技术对石棉断裂的初步探测研究

石棉断裂是大凉山断裂带的重要组成部分,其空间展布与活动性特征对于区域构造稳定性研究有重要的理论意义,且对该地区的城市建设与危险性评价有重要的应用价值。通过对石棉隐伏断裂进行断层气氡地球化学探测,并结合地质勘察、前人探槽、浅层人工地震等资料综合分析,结果表明：(1)断层气氡探测揭示的断裂空间位置与物探、探槽解译的空间位置吻合度较高,断裂位于断层气氡浓度最高峰峰值附近且都分布在主峰的异常区间内;(2)断层气氡探测确定的石棉隐伏断裂的倾向与物探、探槽揭示结果具有一致性,断裂产状为N38°～45°W/SW∠70°～80°;(3)利用断层气Rn浓度衬度值对石棉断裂不同段的相对活动性进行判定,断裂南段(南桠河流域)的活动性要强于北段(大渡河流域)。     

基于 BDS 利用海洋上冰山为人类服务的设想

海洋上冰山虽然被人们称为“海洋杀手”,但是如果人类能够在远航之前做好充分的准备,亦可以利用冰山为人类服务。本文阐述了海洋上冰山的特点,而且研讨了基于北斗卫星导航系统（BDS ）利用海洋上冰山为人类服务的设想。本文研讨的结论也可以为以后数字海洋的建设提供参考。     

滹沱河中游河道带150 ka以来沉积环境演化及其对气候变化的响应

古河道记载了地质历史时期区域水系结构和沉积环境的演变信息,对复原古环境、水系变迁规律等具有重要理论意义。依托滹沱河冲洪积扇扇中古河道带上的一个第四纪钻孔（L2）,基于详细的岩性特征、粒度参数和光释光年龄数据,文章深入分析了古河道发育的期次和时段,探讨了滹沱河中游古河道带150 ka以来的沉积环境演变过程及其对气候变化的响应。结果表明：研究区150 ka以来的沉积环境演化主要表现为三期古河道发育期与两期河流稳定期的交替,与深海氧同位素阶段及其指示的气候冷暖变化有很好的对应关系。其中三期古河道发育期分别对应于深海氧同位素第2、4、6阶段及其指示的气候冷期,两期河流稳定期对应于深海氧同位素第3、5阶段及其指示的气候暖期。第三期古河道（118~151 ka）是由距今150 ka的共和运动引起的构造抬升与倒数第二次冰期冷干气候的共同作用形成;第二期古河道（36~76 ka）是区域间歇性构造抬升与气候变化共同作用的结果;而第一期古河道（5~26 ka）则是末次盛冰期气候变化的产物。     

REE Characteristics of a New Uranium Mineral from the Xianshi Uranium Deposit,South China

正Objective Galuskin et al.(2011)firstly discovered that vorlanite(CaU~(6+/4+))O_4 is a rare Ca-rich mineral with a fluorite-type structure,which is isostructural with uraninite(U~(4+)O_2).Previous studies of the Xianshi granite-related uranium deposit reported that uraninite and pyrite are the major ore minerals whereas galena,clausthalite(PbSe),and pyrite are minor phases in the ores.A more detailed petrographic     

热带平流层水汽的准两年周期振荡

分析了1993年到2002年10年间HALOE卫星资料的热带平流层水汽年际变率,结果表明：热带平流层水汽混合比在2~5 hPa、10~30 hPa、30~100 hPa有三组显著的准两年周期振荡（QBO）现象;其中2~5 hPa和10~30 hPa水汽QBO呈反位相循环;30~100 hPa水汽QBO有显著上传特性.SOCRATES3模式模拟和诊断结果表明,热带平流层水汽QBO是在纬向风QBO强迫下产生的次级动力、热力因子和化学作用耦合后的结果：上层主要是环流输送引起,中层是环流输送和温度扰动驱动下的化学作用引起,下层是对流层顶水汽冻结层的温度扰动和环流输送引起.     

周围型肺错构瘤的多层螺旋CT表现

目的:探讨肺错构瘤的多层螺旋CT(MSCT)表现,以提高CT诊断水平.方法:回顾性分析经手术病理证实的32例肺错构瘤的MSCT平扫及22例MSCT动态增强扫描的特点.结果:MSCT上所有结节边缘光滑.结节内含有脂肪密度(无钙化)的12例,占37.5%,既有脂肪又有钙化的8例,占25.0%,只有钙化的2例,占6.3%.增强扫描(22例)强化值<20HU的20例,占90.9%,强化形态呈间隔状强化16例,占72.7%.结论:肺错构瘤的MSCT表现有一定的特征性,边缘光滑、结节内含有脂肪和钙化有助于诊断,动态MSCT增强扫描有助于与周围型肺癌的鉴别诊断.     

胃肠道间质瘤的CT诊断与临床病理分析

目的:探讨胃肠道间质瘤(GIST)的CT表现,以提高对GIST的诊断水平.方法:搜集经手术和病理证实的胃肠道间质瘤32例,回顾性分析其CT和病理表现.所有病例均行CT平扫及增强扫描.结果:32例肿瘤均为单发,位于胃部17例,空肠和回肠7例,结肠及直肠3例,食管1例,十二指肠和肠系膜各2例.良性9例,恶性23例.CT表现为粘膜下富血供性肿块,肿瘤倾向于腔外生长,可有囊变、坏死及钙化.双期增强扫描见静脉期较动脉期强化显著.结论:CT是GIST的主要影像学检查方法,CT表现有一定的特征性,对胃肠道间质瘤的定位和定性判断,以及鉴别诊断有重要价值,但定性诊断需依赖免疫组化和电镜检查.     

Application of remote sensing technique to mapping of the map series of karst geology in China and Southeast Asia

Based on the mapping program of the map series of karst geology in China and Southeast Asia, the paper summarizes the application of remote sensing technique and the process of acquiring information from remote sensing images. Generally, remote sensing technique serves as an effective method to recognize information about karst topography, rocky desertification and karst collapse. Interpretation of remote sensing images, in combination with field verification and cartographic generalization, provides basic data for updating the program database and compiling synthetic maps. In interpreting remote sensing images, automatic extraction can make it more efficient and visual interpretation can improve its accuracy.     

Distribution and evolution features of salinized soil in Hebei Plain

In order to study the distribution and evolution features of saline soil, the correlations between the groundwater depth, salinity and salinization of soil are examined through analyzing the hydrometeorological data and distribution maps of saline soil, groundwater depth and salinity in 1957 and 2005. The results show that the area of salinization has generally decreased. The area of salinization decreases with the increasing groundwater depth, and the dynamic evolution characteristics appeared between the groundwater depth and area of salinization. The area of heavy salinization is greatest when the groundwater salinity is > 5 g/L, the area of moderate salinization is greatest when the groundwater salinity is between 2-5 g/L, the area of light salinization is greatest when the groundwater salinity is 1-2 g/L and the area of non-salinization is greatest when the groundwater salinity is <1 g/L. The area of heavy salinization was characterized with groundwater depth <2.5 m and salinity >1.8 g/L. The area of non-salinization was characterized with groundwater depth >4.0 m and salinity 0.2-1.5 g/L.