GPS在计算导弹脱靶量中的应用研究

将GPS技术应用于导弹靶试脱靶量测量,并对计算过程作了较为详细的分析和探讨。试验证明：利用GPS测定脱靶量,测量精度高,简单易行,可以在靶场逐步试验推广。     

南黄海北部盆地东北凹陷烃源岩的早期预测

烃源岩评价是沉积盆地油气地质研究的重要组成部分,尤其对油气勘探初期的战略选区与决策至关重要.南黄海北部盆地东北凹陷的油气勘探程度极低,至今尚无探井揭示烃源岩的发育特征,因此制约了凹陷的油气勘探进程.基于地质类比原理,采用与其相邻类似凹陷--北部凹陷综合对比的方法,应用层序地层、沉积相、地震相分析及含油气盆地动态数值模拟等技术,分析了东北凹陷主要烃源岩层的空间展布和生烃演化特征,并初步形成了一套适用于勘探程度低的地区烃源岩早期预测的方法技术流程.研究表明,南黄海北部盆地东北凹陷发育上白垩统泰州组主力烃源岩系,具有广阔的油气勘探前景.     

吐哈盆地丘东凝析气藏中侏罗统储层流动单元划分

对吐哈盆地丘东凝析气藏中侏罗统储层的流动单元的划分方法和参数选取进行探讨。针对丘东凝析低渗透气藏的储层和流体特点,纵向上对研究区中侏罗统地层进行小层精细划分,平面上应用SPSS统计分析软件对厚度、孔隙度、泥质含量、流动带指数等4个参数进行聚类分析和判别分析,将研究区中侏罗统储层砂体划分为4类流动单元。结果表明各流动单元的类型与储层物性、沉积微相具有很好的对应关系,能够客观地反映气藏储层的地质特征。虽然丘东凝析低渗透气藏中流动单元的划分和油藏中流动单元的划分没有太大差别,但是参数的选取却与油藏中的存在着明显的不同。     

甘肃两河口地区水系沉积物异常评价

对两河口地区1:5万水系沉积物资料处理,圈定了大量元素异常。应用R型因子分析结果,划分元素组合。从元素组合特征方面分析,评价异常找矿意义,确定了7个找矿远景区,其中1号异常为最佳找矿靶区。     

新疆与哈萨克斯坦寒武纪磷块岩资源

新疆和哈萨克斯坦寒武纪均为主要的磷矿成矿时代之一,但所形成的磷块岩资源量差别巨大．新疆寒武纪磷块岩矿层薄、矿石质量差、储量很少,哈萨克斯坦小卡拉套山寒武纪磷块岩矿层厚度大、矿石质量好、储量巨大．从实施“走出去”战略出发,邻国小卡拉套地区丰富的磷矿资源对于弥补新疆磷矿资源的严重不足具有重要意义．     

南京市大比例尺地形图的动态更新和维护研究

城市规划需要现势性强的全覆盖的城市大比例尺地形图,城市规划、建设导致地形图的快速变化。如何处理这一对矛盾,最大程度地实现测绘对城市规划、建设和管理的保障,是一个难题。将测绘与规划管理的日常业务进行结合,提出一整套城市大比例尺地形图的动态更新和维护的方法,制定相应的数据标准和规范,研制了支撑平台,并在浦口区进行实践,具有较强的可操作性。     

Geochemical Mapping: With Special Emphasis on Analytical Requirements

More than 40 national and regional geochemical mapping projects in the world carried out from 1973 to 1988 do not conform to common standards. In particular they have many analytical deficiencies. In the period 1988 to 1992, the International Geochemical Mapping project （Project 259 of UNESCO＇s IGCP Program） prepared recommendations designed to standardize geochemical mapping methods. The analytical requirements are an essential component of the overall recommendations. They included the following： 71 elements should be analyzed in future mapping projects; the detection limits of trace and ultratrace elements must be lower than the corresponding crustal abundances; and the Chinese GSD and Canadian STSD standard sample series should be used for the correlation of global data. A proposal was also made to collect 5000 composite samples, at very low sampling densities to cover the whole Earth＇s land surface. In 1997 an IUGS Working Group on Global Geochemical Baselines was formed to continue the work which began with IGCP 259. From 1997 up to now, new progress has been made especially in China and FOREGS countries under the aegis of this working group, including the study of suitable sampling media, development of a multi-element analytical system, new proficiency test for selection of competent laboratories and role of wide-spaced mapping in mineral exploration. One of the major problems awaiting solution has been the inability of many laboratories to meet the IGCP recommendations to generate high quality geochemical maps. Fortunately several laboratories in China and Europe have demonstrated an ability to meet the requirements and they will be well placed to render technical assistance to other countries.     

Oviraptorosaurian Eggs (Dinosauria) with Embryonic Skeletons Discovered for the First Time in China

Two elongatoolithid dinosaur eggs from the Upper Cretaceous of Ganzhou, Jiangxi Province and the embryonic skeletons they bear are described. They represent the first oviraptorosaurian eggs with embryonic skeletons in China and provide the first example that an oospecies can be correlated to certain dinosaur taxon/taxa. The two eggs are the same as the pair of the eggs inside a female oviraptorosaurian pelvis from the same horizon of the same area in both macro- and micro-structures of the egg shells, and can he referred to the oospecies, Macroolithus yaotunensis Zhao, 1975. The morphology of the preserved part of the embryonic skeletons indicates that they may have been laid by an oviraptorid, Heyuannia huangi from Guangdong Province or a closely related oviraptorosaurian, which may have been lived in the Ganzhou area too in the Late Cretaceous. The embryonic skeletons of the two eggs are not in the same developing stage. In one of the eggs, the postzygapophysis of the preserved vertebrae are well ossified, indicating that it was just hatched.     

Distribution of Palygorskite in the Lingtai Profile of Chinese Loess Plateau: Its Paleoclimatic Implications

Palygorskite is a typical indicator mineral of the arid and strong evaporation environment. Distribution of palygorskite in loess-red clay sequences may act as an important indicator for reconstruction of the paleoenvironment and paleoclimate. In this paper, field emission scanning electron microscope and high-resolution transmission electron microscope observations on the red clay-loess-paleosol of the Renjiapo profile at Lingtai, Gansu Province indicate that palygorskite occurs widely in red clay sequences formed before 3.6 Ma, but no occurrence has been found in eolian sediments since 3.2 Ma. Micromorphological features and microstructure of palygorskite show that it is an autogenic mineral formed during pedogenesis, and transformed from iilite-montmorilionite under the pore water action. In the Lingtai profile, the disappearance horizon of palygorskite is consistent with those of increasing magnetic susceptibility, dust flux and depositional rate. The distribution of palygorskite in the profile indicates that the interval of around 3.6 Ma was an important transformation period of the East Asian paleomonsoon, when changes took place in the East Asia paleoclimate pattern, i.e. a high-frequency strong fluctuation alternative evolution of the environment. Therefore, palygorskite is a key indicator mineral of the East Asian paleomonsoon evolution of that time.     

建立影像地图集生产系统,提高实践性教学质量

结合《苏州市影像地图集》的设计和研制,着重讨论基于新技术进行影像地图集生产的软硬件环境,以及通过对新技术的生产流程、过程控制方法等关键环节的技术研究和实践,建立了影像地图集生产实践教学系统。该系统为教师提供了先进的科学研究、技术开发和技术应用环境和条件,为开展实践性教学和进行地图集设计、生产提供理论和技术指导。