高炉渣合成Ca-α-Sialon-SiC粉的热力学分析及工艺优化

在热力学分析的基础上，以高炉渣为原料，引入适当的添加剂，利用碳热还原－氮化的方法制备了Ｃａ－α－Ｓｉａｌｏｎ－ＳｉＣ粉，得到的Ｃａ－α－Ｓｉａｌｏｎ含量最高可以达到８１％；利用统计模式识别结合人工神经元网络优化了工艺．     

机械活化粉末制备W-Cu合金的微观组织

为了改善制备工艺和提高W-Cu合金的密度与性能,对原料粉末进行了机械活化处理,通过成形和烧结制备了W-Cu合金,考察了活化后粉末的变化,观察了合金的烧结组织并测量了密度.结果表明,机械活化能增大钨铜粉末的表面能和晶格畸变能,有效地促进烧结,改善烧结组织;烧结体中存在大量团絮状组织,团粒内部钨颗粒主要以固相方式烧结在一起,而团粒之间则以液相烧结为主.烧结组织细密、均匀,相对密度达98%以上;烧结组织中钨铜两相在微米尺度下仍然结合良好,部分界面出现了互溶.     

Chronostratigraphic units in the Jurassic and their boundaries: Definition, recognition and correlation, causal mechanisms

The historical development of the chronostratigraphic classification of the Jurassic into series, stages and zones is summarised. Traditionally, the series and stages are defined hierarchically in terms of the standard (ammonite) zones they contained but since Hedberg (1976)［1］ they have been defined by a basal boundary stratotype (GSSP). To date four Jurassic Stages have ratified GSSPs; progress with the others is outlined. The primary marker for the definition of the Stage boundaries is biochronology based on evolution of ammonites, with secondary markers based on biostratigraphy of other fossil groups, chemostratigraphy and magnetostratigraphy. Causal mechanisms for the environmental changes that caused ammonite evolution are reviewed and possible methods of correlation with nonmarine successions are briefly discussed.     

断陷盆地构造枢纽部位油气富集规律

以十屋断陷为例,根据其构造演化、主要断层特征及油气成藏条件分析,揭示多旋回断陷盆地构造枢纽带与油气富集关系.结果表明:十屋断陷枢纽部位经历了断陷期、断拗过渡期、拗陷期、萎缩隆升期等复杂的构造演化,多期差异构造变形及断裂活动导致了小宽枢纽带南段和北段具有相似性及差异性,后期构造反转发育部位多为早期断层发育部位,且主要集中在主干断层上,构造运动产生位移被断裂和褶皱吸收;不同阶段的隆起部位相叠加,使枢纽部位与构造高点相对位置发生变化,枢纽部位相对位置由原来的古隆起演变为斜坡部位;枢纽部位早期为油气的有利指向区,晚期具有良好的保存条件,同时发育多类型圈闭、有利沉积相组合及生储盖组合,围绕枢纽带可形成复式油气聚集带.     

Chronostratigraphic units in the Jurassic and their boundaries: Definition, recognition and correlation, causal mechanisms

The historical development of the chronostratigraphic classification of the Jurassic into series, stages and zones is summarised. Traditionally, the series and stages are defined hierarchically in terms of the standard (ammonite) zones they contained but since Hedberg (1976)［1］ they have been defined by a basal boundary stratotype (GSSP). To date four Jurassic Stages have ratified GSSPs; progress with the others is outlined. The primary marker for the definition of the Stage boundaries is biochronology based on evolution of ammonites, with secondary markers based on biostratigraphy of other fossil groups, chemostratigraphy and magnetostratigraphy. Causal mechanisms for the environmental changes that caused ammonite evolution are reviewed and possible methods of correlation with nonmarine successions are briefly discussed.     

浅谈高校图书馆服务模式创新和形象塑造

网络化、信息化、数字化时代的到来改变了图书馆的运行环境,使高校图书馆的信息服务出现了危机,因此需要创新服务模式,优化服务流程,即开展个性化服务,设立学科信息服务中心,开展层次化信息服务。