塔里木及邻区晚古生代早期古气候与构造

影响塔里木及邻区晚古生代早期气候的地球内部因素为古昆仑和南天山两个古洋盆封闭及有关的两条缝合构造带演化，从而形成上述时空段内热带海洋气候、热（亚热）带季风气候、热带沙漠气候以及热带滨岸干湿气候区域的更替，古气候特征的判断主要依据古地磁数据、古生态气候学、沉积环境诸方面。     

从层序地层学研究试论华北地区寒武系与奥陶系分界

华北地区寒武系－奥陶系过渡沉积可划分为三个层序：凤山层序、两河口－红花园层序和大湾层序，凤山层序与两河口－红花园层序之间的界面为Ⅱ型层序界面（ＳＢ２），而两河口－红花园层序与大湾层序之间的界面为Ｉ型层序界面（ＳＢ１）。华北地区寒武系－奥陶系界线应置于两河口－红花园层序的海侵体系域的下界面，在徐州地区为三山子组（狭义）与韩家组之间，在北京西山为韭园组微晶丘与冶里组之间。     

Parameters of Land-Surface Processes for Gobi in North-West China

Using data from the intensive observation period (May–June 2000) of the NWC-ALIEX (The Field Experiment on Interaction between Land and Atmosphere in Arid Region of North-west China), the characteristics and mechanisms of some key land-surface process over Gobi in a typical arid region of north-west China are analyzed and several parameters of land-surface processes are calculated. The weighted mean of the surface albedo over a typical arid region of the Dunhuang Gobi is calculated using the relative reflection as a weighting factor, and its value is 0.255 ± 0.021. After removing the influence of precipitation, the mean soil heat capacity over a typical arid region of the Dunhuang Gobi is 1.12 × 10⁶ J m^-3 K^-1,which is smaller than that observed in the Heihe (China) River basin Field Experiment (HEIFE). The mean soil heat diffusivity and conductivity are about half of those observed in HEIFE.     

中国兴凯湖北岸平原晚全新世花粉记录及泥炭沼泽形成

通过兴凯湖北岸平原泥炭剖面高分辩率花粉分析研究，对晚全新世花粉划分4个组合带。XKH-4组合时期(1857～1746aB．P．)为沼泽发育前期，这一时期花粉浓度小，陆生草本植物占优势，气候干冷。XKH-3组合时期(1746～1287aB．P．)为沼泽发育早期，这一时期花粉浓度较大，且水生植物花粉含量为剖面最高，喜温落叶阔叶植物大发展时期，气候温和湿润。XKH-2组合时期(1287～602aB．P．)为沼泽发育中期，这一时期花粉浓度最小，但以陆生草本植物为主，木本植物为辅，水生植物急剧减少，针叶植物出现两次高峰，气候向冷干方向发展。XKH-1组合时期(602aB．P．至今)为沼泽发育盛期，这一时期花粉浓度最大，陆生草本植物大发展时期，气候波动较大。     

Estimation of ocean primary productivity and its spatio-temporal variation mechanism for East China Sea based on VGPM model

According to calculation results of ocean chlorophyll concentration based on SeaWiFS data by SeaBAM model and synchronous ship-measured data, this research set up an improved model for CaseⅠand CaseⅡwater bodies respectively. The monthly chlorophyll distribution in the East China Sea in 1998 was obtained from this improved model on calculation results of SeaBAM. The euphotic depth distribution in 1998 in the East China Sea is calculated by using remote sensing data of K490 from SeaWiFS according to the relation between the euphotic depth and the oceanic diffuse attenuation coefficient. With data of ocean chlorophyll concentration, euphotic depth, ocean surface photosynthetic available radiation (PAR), daily photoperiod and optimal rate of daily carbon fixation within a water column, the monthly and annual primary productivity spatio-temporal distributions in the East China Sea in 1998 were obtained based on VGPM model. Based on analysis of those distributions, the conclusion can be drawn that there is a clear bimodality character of primary productivity in the monthly distribution in the East China Sea. In detail, the monthly distribution of primary productivity stays the lowest level in winter and rises rapidly to the peak in spring. It gets down a little in summer, and gets up a little in autumn. The daily average of primary productivity in the whole East China Sea is 560.03 mg/m2/d, which is far higher than the average of subtropical ocean areas. The annual average of primary productivity is 236.95 g/m2/a. The research on the seasonal variety mechanism of primary productivity shows that several factors that affect the spatio-temporal distribution may include the chlorophyll concentration distribution, temperature condition, the Yangtze River diluted water variety, the euphotic depth, ocean current variety, etc. But the main influencing factors may be different in each local sea area.     

宁夏气象影视数字化节目制作系统的建立

在信息传播媒体的竞争日益严酷的时代,面对天气预报节目只依靠简单的画面加解说,拉洋片式传统方法这样一种一成不变的局面,策划创意制作出《天气资讯》节目,打破天气预报节目以往的节目形式和播出形式,以极少的投入获得最大的社会效益和经济效益。     

泰安基准台洞体及环境改造

大部分形变仪器长年工作在山洞内,洞室的潮湿对仪器及房间内装修材料影响很大,“十五”期间中国地震局投资近十万元对泰安台形变仪器专用山洞进行了改造。本文从改造内容,改造方法及改造效果几方面进行了阐述,为同类山洞改造提供借鉴。     

历史探究：“侯家窑人”与“许家窑人” 名称之争——浅谈“许家窑人”名称的合法性问题

本文简要回顾了“许家窑-侯家窑遗址”和所谓“许家窑人”的研究历史及其名称的沿革过程,并对“许家窑人”名称的合法性提出质疑。从考古学角度来看,前人将考古遗址名称确定为“许家窑-侯家窑遗址”是可以理解的,因为山西省阳高县许家窑村与河北省阳原县侯家窑村相邻,相距不远;同时该名称是经国务院1976颁布确定的,是受国家法律法规保护的。但从古人类学角度来看,将侯家窑村（74093地点）发现的古人类命名为“许家窑人”是不合情理的,也是不合法的,因为传统上古人类的名称都是以化石发现地来命名的（俗名）,正确的做法应该将侯家窑村发现的人类化石冠以生物学名称（学名）,如直立人、智人、龙人等。实际上,山西许家窑村（73113地点）根本就没有发现过任何人类化石。根据一些学者在文中提供的化石描述、测量数据及化石图片,笔者等倾向于认为,河北侯家窑村发现的人类化石可能属于‘龙人’的一个亲缘种（Homo aff. longi）,在更新世古人类研究中具有十分重要的科学价值。     

石英脉型钨多金属矿床的扇状成矿实例及找矿模型

石英脉型钨矿床是中国数量最多的钨矿床类型,但保有储量消耗迅速,迫切需要创新找矿模型,指导找矿突破。文章结合二十余年的找矿实践,通过详细分析扇状成矿矿床实例,构建了石英脉型钨矿床新的找矿模型。该模型强调赋矿裂隙为岩浆动力成因,在花岗岩体顶部呈扇状分布型式,岩浆期后热液恰在裂隙张开时充填其中而形成扇状成矿系统;提出“就岩找矿”、“就矿找矿”、“就矿找岩”的地质、地球化学和地球物理标志,指导矿床尺度的勘查工程部署。截至目前,该模型已在广东禾尚田钨锡矿床、广西珊瑚钨锡矿床、广西社垌钨钼矿床、江西盘古山钨铋矿床等获得了验证,找矿成效显著。     

现代深部岩溶研究进展与展望

现代深部岩溶问题是随着工程建设向复杂场地延伸而逐渐显现,由它带来的一系列地质工程问题对越岭隧道工程具有极强的控制性和危害性,如渝怀线圆梁山深埋特长越岭隧道工程出现的高压突水、突泥问题,既控制了工程的施工难度,又是一个极具挑战性的理论难题。综述了现代深部岩溶相关概念、发育类型、发育特征、形成机制等方面国内外研究现状,勾画了现代深部岩溶研究今后的重点,主要包括现代深部岩溶概念的厘定、现代深部岩溶工程地质分类及特征、现代深部岩溶受控因素、现代深部岩溶发育机制及演化、现代深部岩溶对越岭隧道工程控制作用等几方面的研究。