汾河下游三万年来沉积环境演化

根据汾河下游岩性特征、沉积物粒度、粘土矿物和孢粉分析，探讨了汾河下游3万年来环境演化规律。30－11Ka.B.P为晚更新世末次冰期盛冰期，气修干寒；11Ka以来，经历了3个气候旋回，变化周期为3.5Ka左右，黄河中游早期文明起源及人类生产活动，与本区气候关系有很好的耦合性。     

低维空间中带调和势的非线性Schrdinger方程

研究一维和二维空间中带调和势的非线性Schr dinger方程iφt +12 Δφ - 12 ｜x｜2 φ +a｜ φ｜2 φ +b｜φ｜4φ =0 ,φ(0 ,x) =φ0 ,t≥ 0 ,x∈Rn,a、b为常数 ,针对非线性项互为排斥的情况 ,应用Tsutsumi和Zhang(Adv .Math .Sci.Appl.,1998,8(2 ) :6 91～ 713.)的有关方法 ,讨论了上述Cauchy问题在一定条件下解的不稳定性质     

Ramsey数R(k,l;r)的构造性下界

确定Ramsey数的构造性下界是组合数学中很有意义而又非常困难的课题,迄今仅有个别结果。本文将研究一类组合竞赛,给出任意Ramsey数R(k,l;r)的构造性(算法性)下界。     

安徽下扬子区北缘薄皮构造研究

安徽下扬子区北缘薄皮构造之表层构造丰富、典型;受基底与盖层间的切性滑脱面及下志留统高家边页岩韧——脆性滑脱面的联合控制,薄皮构造呈往南东变浅的楔形。薄皮构造以单剪方式往南东运动,缩短量达94km,缩短率约63.4％;起因于印支运动晚期至燕山运动早期扬子板块对华北板块的左行客斗向陆——陆碰撞所产生的拆离,先存生长正断层及板块边界的陆缘性质决定了其内部层块格局。薄皮构造的突发隆起带及韧性滑脱面分别是寻找油气和金的有利地带。     

两个度量空间中集值映象的不动点定理

本文证明了两个度量空间集值映象的一个不动点定理,另一个关于紧度量空间的类似结果也被证明。     

H－空间上N－人非协作对策的Nash平衡点的存在性定理

本文给出Ｈ－空间上几种对策模型的Ｎａｓｈ平衡点的存在性定理，这些结论不仅是Ｈａｕｓｄｏｒｆｆ拓扑线性空间中相应结论的推广，而且为进一步研究Ｈ－空间上对策的解及稳定性打下一定基础。     

鄂尔多斯盆地下古生界成岩后生作用及储集性

以最新资料研究表明，鄂尔多斯盆地下古生界存在４种主要的成岩后生作用，５个储集空间形成阶段和４个天然气储集层。     

米仓山南缘奥陶纪地层新见

详细描述了米仓山南缘奥陶系剖面。将该区奥陶系划分为湄潭组、宝塔组和龙马溪组三个岩石地层单位,并探讨了其空间变化规律,同时根据生物组合特征建立了四个生物带,发现了Ｈｉｒｎａｎｔｉａ－Ｋｉｎｎｅｌａ组合带的存在。拟定后的龙马溪组为一跨晚奥陶世－早志留世的岩石地层单位。     

Lower Cambrian small shelly faunas from Zhejiang (China)and their biostratigraphical implications

Despite a long history of research on the Early Cambrian in China most available data on small skeletal fossils concern fossil associations of the shallow carbonate platform. Information on skeletal fossils from marginal shelf environments of the Yangtze Platform is scanty, which may reflect the rarity of fossils in deeper sedimentary environments but is also due to limitation of carbonate distribution and outcrops, difficulties in fossil extraction, and a general research focus on the Precambrian-Cambrian boundary beds on the carbonate platform. Here we present a documentation of Meishucunian to Qiongzhusian small skeletal fossils from the lower Hetang Formation and the chert unit at its base from the Jiangshan region, Zhejiang Province, representing a relatively deep shelf environment compared to the inner shelf region. The earliest association (Meishucunian) from the chert unit underlying the Hetang Formation is mainly characterized by the occurrence of Protohertzina anabarica, P. unguliformis, Fengzuella zhejiangensis, and Kaiyangites novilis, which differs somewhat in composition from SSF-associations of typical inner shelf deposits. The enigmatic skeletal fossil Fengzuella zhejiangensis, which exhibits an unusual secretional growth mode previously unrecognized from the Early Cambrian, is described in detail. A younger (Qiongzhusian) fossil association contains numerous arthropod remains, such as disarticulated spines of arthropods (Jiangshanodus- and Kijacus-type), which have previously been considered as conodont-like fossils, and bradoriid valves.     

森的第k个特征根的Sharp下界

设λ_k是n个顶点森的第k个特征根,q是边独立数。本文证明了关于λ_k（2≤k≤q-1）的一个猜想,同时给出了λ_k的下界;并且关于森获得了λ_k的Sharp下界,关于树在k较小时获得了λ_k的Sharp下界。