四川兴文5.7级地震烈度评定及结构震害简析

四川兴文5.7级地震共致宜宾市兴文县、珙县和长宁县3个县22个乡镇受灾,震区抗震设防烈度为Ⅵ度。震区主要建筑物结构类型为框架结构、砖混结构、砖木结构和土木结构,大多数房屋没有经过抗震设防加固,抗震性能一般。通过对震区3个县68个抽样点的调查,发现框架结构和设防砖混结构在此次地震中表现出了良好的抗震性能。同时对不同结构类型房屋的构造方式、分布情况和震害特点进行了分析,并针对不同的震害特征,为今后该地区的灾后恢复重建和防震减灾工作提出了对策建议。     

柴达木盆地西部地区渐新世下干柴沟组上段盐湖沉积特征

利用大量地质及地球化学资料,开展了柴达木盆地西部地区渐新世下干柴沟组上段盐湖沉积特征研究,重点识别岩石类型,恢复古沉积环境,建立沉积模式,探讨控制因素。研究认为：盐湖环境主要发育两大类、五小类沉积相组合,盐湖边缘沉积相包括滨岸斜坡带相组合、缓坡带相组合、陡坡带相组合,盆内沉积相包括水下隆起带相组合和盐湖深水区相组合;盐湖可划分早、中、晚3个沉积演化阶段,分别对应半咸水湖泊、咸水湖泊和盐湖;形成碳酸盐岩与钙质砂岩、富含石膏的碳酸盐岩与泥岩、厚层石盐与薄层碳酸盐岩等主要岩石组合;盐湖沉积主控因素为气候、古地貌与构造运动。     

局部表面参数化的实景三角网模型语义增强方法

倾斜摄影测量方法已可自动获取城市规模的实景三角网模型,然而散乱的三角网缺乏精细的几何结构和功能语义信息。为克服上述问题,提出一种局部表面参数化的实景三角网模型语义增强方法:将具有语义信息的独立三维部件与实景三角网模型的无缝融合问题,通过定义三维表面结构树,转换为局部区域的三角网替换操作;在待融合区域附近,将原实景三角网模型和替换的三维语义部件,通过局部参数化表达,UV展开为二维平面三角网;在二维平面上构建约束Delaunay三角网(CDT),实现两模型的无缝拼接,逆映射至三维空间并自动重建语义部件。通过深圳某区域的倾斜影像进行的试验证明,本文方法能有效实现具有开放边界和语义信息的部件模型与表面模型的无缝融合。与商业软件Maya对比,这种基于插入、融合的手段对提高建模效率具有实用价值。     

多波束测深系统海底目标探测能力评估方法

为了有效衡量多波束测深系统的目标探测性能,提高舰船水下目标搜寻、援潜救生和打捞能力等,对当前多波束测深系统目标探测问题进行分析,推导了多波束测深系统目标探测分辨率估计模型。以SONIC 2024型多波束测深系统为例,分析了不同水深下在多波束测深系统垂直航迹方向、沿航迹方向分辨率的变化规律及量级大小,对覆盖宽带和航速等参数指标设置提出了合理建议,为多波束测深系统目标探测能力的准确评估提供依据,具有一定参考价值。     

Nutrient compositions of cultured Thalassiosira rotula and Skeletonema costatum from the Jiaozhou Bay in China

Carbon, nitrogen, phosphorus, silicon composition of cultured two different sized phytoplankton common species of Thalazsiosira rotula and Skeletonema costatum from the Jiaozhou Bay were measured. Carbon, nitrogen, phosphorus, silicon contents in cell were obvious higher in T. rotula than in S. costatum, but the percents of nitrogen, phosphorus, sihcon contents in cell dry mass in T. rotula were lower than those in S. costatum. The dry mass concentrations of nitrogen,phosphorus, silicon in S. costatum were much higher than those in T. rotula, particularly silicon, the former was 6. 4 times of the latter, showing that S. costatum could more assimilate these elements. Especially, S. costatum had competitive dominance for assimilating silicon, which is beneficial to its becoming a major dominant species in relative short silicon of the Jiaozhou Bay. There were some differences in numerical value of nutrient ratios both laboratory-cultured phytoplankton and different sized suspended particulates （ mainly phytoplankton） in the Jiaozhou Bay, which was caused by the changes of environment. High contents of carbon, nitrogon and relative low phosporus, sil- icon, high molar ratio of nitrogen to phosphorus （far higher than Redfield value） and low ratio of silicon to phosphorus and silicon to nitrogen （far lower than Redfield values） in the two diatoms and different sized suspended particulates were consistent with those in the seawater. Relative short silicon in the seawater and phytoplankton showed that silicon was possibly affectting phytoplankton growth in the Jiaozhou Bay.     

Two new species of the genus anthenoides (Echinodermata: Asteroidea) from southern China

Two new species of the genusAnthenoides from the southern China are described.A. laevigatus sp. nov. shows affinities withA. epixanthus. A. tenuis sp. nov. is related toA. cristatus (Sladen). Contribution No. 1472 from the Institute of Oceanology, Academia Sinica     

理塘断裂带沙湾段的晚第四纪活动性*

理塘断裂带沙湾段展布于四川西南部的木里河流域,处于理塘断裂带的南东尾端,为左旋走滑运动性质。文章在航空照片判译的基础上,通过野外研究发现,该断裂段的断错地貌现象主要集中分布在绒龙沟-沙湾的木里河东岸坡麓地带,表现为断层陡坎、断塞塘、断错冲沟、河流阶地及洪积扇等。由5个地点的断裂位错值和位错开始的年代学(TL和¹⁴ C)测试结果,估计的该断裂段晚更新世以来的平均水平滑动速率为2.1±0.3mm/a。在该断裂上开挖的3个探槽资料表明,该断裂段存在史前强震的地质记录,最晚一次强震的发生时间介于1310±90~950±30aB.P.之间,强震所导致的垂直位错量约0.5m, 同震水平位错1.30~1.45m左右。根据同震位错量及断裂长度估计的地震震级为7.0级左右。     

四川玉农希断裂的全新世活动与1975年康定六巴6.2级地震

玉农希断裂呈N20°～30°E方向展布于四川省西部高原,构成贡嘎山第四纪强烈隆起断块的西边界.在北西西-近东西向的区域主压应力作用下,玉农希断裂第四纪以来主要表现为挤压逆冲性质.断错地貌研究结果表明,该断裂为一条全新世弱活动断裂,平均垂直滑动速率为0.5～0.6 mm/a左右.1975年1月15日康定六巴6.2级地震发生于该断裂上,宏观震中位置位于六巴乡溯布-莫达村附近,极震区长轴方向与玉农希断裂走向一致,是该断裂最新活动的表现.     

Features of Minerogenic Series Related to Continental VolcanicRocks in the Southeastern Coastal Area of China-A Case Study of the Daiyunshan-ShiniushanVolcanic Depression in Fujian

The Daiyunshan-Shiniushan volcanic depression in Fujian Province is situated in a volcanic belt of the southeast coastal area in China along the west Pacific Ocean. A new breakthrough has been made in the exploration of gold and silver ore deposits in recent years. The minerogenic series of the Daiyunshan-Shiniushan volcanic depression is discussed in this paper based on the analysis of major metallogenic types and factors. According to the study of enormous ore deposits and occurrences in the study area, two minerogenic series have been recognized: 1. Late Jurassic Au-Ag-Pb-Zn minerogenic series related to intermediate-acid, acid volcanic formations; 2. nonmetallic minerogenic series (pyrophyllite, alunite pearlite, andalusite, zeolite, corundum and so on) related to intermediate and acid volcanic formations. The division and study of the minerogenic series have revealed metallogenic and time-space distribution characteristics of the ore deposits in the volcanic belt of the southeast coastal area in Ch     

边坡测点平面位移图及其应用

针对目前边坡变形监测数据事理方法的不足,设计了一种简洁、直观、信息量大的变形位移轨迹图,较好地将变形时段、变形量、变形方向有机地结合在一起。