鄂尔多斯地区晚古生代陆相沉积层序地层学研究

鄂尔多斯地区晚古生代陆相沉积占据了较长的时期，基于现代沉积学理论和层序地层学思想，本文从鄂尔多斯地区晚古生代沉积盆地的沉积特点出发，建立一套比较切合实际的层序地层划分方案，研究了该区晚古生代陆相沉积层序地层学，比较客观地反映了盆地沉积作用和构造演化历史。     

塔里木盆地草湖凹陷油气勘探的基本条件及前景分析

“九·五”期间 ,我们对塔里木盆地库尔勒鼻凸—草湖凹陷油气勘探靶区进行了详细的研究。这个地区 ,经过十余年勘探 ,成果不理想。因此 ,有的研究者认为无进一步勘探的价值 ,有的专家则认为是有利的后备区。通过研究 ,我们认为 ,库尔勒鼻凸由于长期暴露 ,无进一步勘探价值 ;而草湖凹陷虽不是象阿克库勒凸起那样的优越的勘探区 ,但仍具备一定勘探前景 ,可以作为较为有利的后备接替勘探区。有利区块为小干湖区块和草 1井区块 ,其次是草湖凹陷西斜坡。     

Expert System for Statistical Prediction of Mineral Deposits on Middle and Large Scales

The expert system for statistical prediction of mineral deposits on middle and large scales takes the system of scientific exploration theories, criteria and methods proposed by Professor Zhao Pengda as the field expert knowledge. At present the developed system focuses on two aspects: synthetic exploration and quantitative exploration. Among the three basic theories for the prediction of deposits, it highlights the applications of seeking anomaly theory. This system is characteristic in the determination of geological background, the study of geological anomalies and the delineation of geological background, the study of geological anomalies and the delineation of mineralization anomalies. The system combines closely the knowledge base, method base and database ,integrates the input and output information of multi-sources and multi-variables, data , graphs and imagine processing system and inquiring system as a whole . So the system can meet in general all kinds of demands in statistical prediction of m     

降低金刚石钻头烧结温度的方法

人相图上分析了制取预合金胎体粉末以降低钻头烧结温度的可行性，并结合生产实践介绍了２种预合金粉末的制备方法，从而把制造金刚石钻头的烧结温度降低到９００℃。     

A QUASI-TWO-DIMENSIONAL STREAM TUBE MODEL FOR SIMULATING FLOW IN ALLUVIAL RIVERS

I. INTRODUCTIONIt is necessary, sometimes, to predict river bed deformahon during the alanning and design stages of a hydraulic project. As the nuvial process is quite complicated, the I --Dmathematical models currently in use can not satisfy the various needs in hydraulic engineering. Particularly in engineering practice, there is a strong desire of knowing the hydraulicconditions and river bed deformation in details. Some two dimensional models as well asqusi--two--dissensional models …     

ASSESSMENT OF THE EFFECTIVE RANK OF A (CO)VARIANCE MATRIX: A NON-PARAMETRIC GOODNESS-OF-FIT TEST

Each eigenvector of the dispersion matrix[X]~T[X]was shown to be a partial predictor of the originaldata matrix [X],the sum of the predictions from the individual principal components being equal to theexpectance of [X].By comparing the distributions of the members of two neighbouring predictedmatrices,[X]_(1...i)and [X](1...i+1)(i.e.the sums of the first i and i+1 individual predictions respectively),it was shown that they should be indistinguishable provided that i is equal to or greater than the effectiverank of [X],and significantly different otherwise.This was confirmed by analysing the visible absorptionspectra of methyl orange and methyl red solutions as well as the Raman spectra of Na_2SO_4 and MgSO_4solutions.On the grounds of these findings,a non-parametric goodness-of-fit test for assessing theeffective rank of[X]was proposed which proved to be comparatively conservative and more robust thanmost currently used tests.