滇东地区早寒武世磷块岩的藻类化石

滇东早寒武世磷块岩薄片中发现大量藻类化石。本文所讨论的磷质藻类化石主要有:球状藻类、丝状藻类、疑源类、叠层石类、核形石类和花纹石类(凝块石类)等27个属种(或型),它们构成各种颗粒磷块岩、叠层石磷块岩、藻丘磷块岩,是磷块岩富矿的主要组分,P_2O_5可达30—37％。这些多门类的藻类化石,为生物成磷作用和成矿环境提供了主要依据,也为震旦—寒武系界线划分提供了新的资料。     

沙质海岸防波堤附近岸线变形预测

本文提出一种适用于沙质海岸线变形计算的数值模型.由于本模型采用了隐格式,与过去提出的模型相比,具有计算稳定性好、时间步长可取得较大、上机运行时间大大缩短等优点同时,考虑了岸线随时间变化而引起的对波浪折射的影响;在防波堤下游一侧考虑了波浪绕射和折射对岸滩冲刷的综合作用.作为算例,对某一港口防波堤附近的岸线变形进行了计算,表明用隐格式和显格式模型得到的结果颇为接近,与物理模型试验得到的结果相比较也很一致.因此,本文提出的这一隐格式模型可用于海岸工程的规划和设计中.     

用隐函数定理解一类带位移的非线性奇异积分方程

本文在空间H_δ~o上讨论一类带位移的非线性奇异积分方程的可解性,指出了当参数λ绝对值充分小时该方程存在唯一解,然后应用隐函数定理得出该方程对任意固定的参数λ解的存在性定理。     

植保机械预压空气室的研究

预压空气室虽在国内外生产的植保机械用隔膜泵上已普遍应用,但对该类空气室的性能研究未引起重视。本研究表明,空气室的充气压力、气室隔膜的材质和结构尺寸对气室的稳压效果很有影响,如设计和使用不当,不但达不到预期的稳压效果,还可能加大压力波动。本文通过理论和试验数据的频谱分析指出,预压空气室的充气压力应与工作压力很好匹配,压力脉动最小的最佳充气压力与工作压力之间成线性关系,并建议隔膜泵预压空气室应装有充气压力指示装置。     

Fuzzy综合评判 在毕业生质量跟踪调查研究中的应用

本文根据对毕业生跟踪调查所获得的信息,运用Fuzzy数学综合评判的方法,进行定量分析,从而得出综合评价结论.     

Interaction of fluid dynamic factors in the migration and accumulation of natural gas

The migration of fluid petroleum gas, described as fluid potential, depends only on gravity, fluid pressure controlled by depression and capillary force during tectonically stable period; but on tectonic stress during the tectonically active period with severe compression. This method is applied in the Junggar Basin, showing that the migration of Jurassic gas during Cretaceous and Eocene and the migration of Permian gas from Jurassic till the present are determined by capillary force and fluid pressure (including overpressure) which is controlled by depression; the migration of Jurassic gas from Eocene till the present and the migration of Permian gas during Triassic are controlled by tectonic stress.     

虚拟内窥镜中心路径抽取技术

目的在空腔器官中提取一条最佳的用于虚拟内窥镜漫游的中心路径。方法采用基于距离变换的方法进行路径抽取。结果给出了虚拟内窥镜中心路径的定义，总结了中心路径的基本特性。结论在虚拟人脑内窥镜系统中实现了中心路径的提取，用于器官内窥检查，效果良好。     

基于三维人体测量的参数化人台的研究

为了提高服装的合体性，在对三维人体测量结果统计分析的基础上，提出了参数化人台设计技术路线．在VC＋＋．net单文档视图模式下调用OpenGL，通过多边形曲面造型方法实现了可用按钮和键盘来控制的参数化人台设计．结果生成了反映人体特征的标准系列人台和个性化人台，用于三维服装CAD和服装人台的制作。     

Composition of sandstone and heavy minerals implies the provenance of Kuqa Depression in Jurassic, Tarim basin, China

The petrological characteristics and heavy mineral assembly of the Jurassic System in Kuqa Basin are consistent with the tectonic evolution, which is the major factor controlling the filling process of Kuqa Basin. Controlled by the source areas at the both sides of the Basin, the matrixes are dominated by sedimentary rock, high-grade metamorphic rock, acid magmatic rock, and the highest heavy mineral assemblage of zircon-garnet-magnetite in the content. According to heavy mineral indexes, the Jurassic strata can be classified into three rhythmic units of heavy mineral. The lower sequence contains abundant heavy minerals and relatively high content of detritus and its matrixes primarily came form the recycling orogen. The assemblage of “zircon-garnet-magnetite” indicates that the sedimentary area in the early evolution period of the basin is relatively near the provenance. The middle sequence is different from the lower sequence in the heavy mineral assemblage and has the different characteristics from that of source rock. The heavy mineral assemblage is “garnet-zircon” with the highest content of garnet and its main matrices are the high-grade metamorphic rock, acid magmatic rock and hydrothermal vein at the northeastern edge of the basin. The middle and upper sequences are characterized by the clast provenance, which is primarily from the recycling orogen at the northern edge of the basin and secondarily from the southern uplift. As a result of the two provenances, the strata with apparent changes of heavy mineral assemblage and index better coincides with the interfaces of the secondary strata sequences, which reflects the denudation history and the filling process of the orogen at the northern edge of the basin.