一种基于沃希变换的测井自动分层方法

介绍了一种利用沃希（Ｗａｌｓｈ）变换实现测井曲线计算机自动分层方法。叙述了Ｗａｌｓｈ变换的基本理论和用于测井自动分层的实现过程。通过实际资料的处理证明,该技术是一种快速、准确的认识岩性界面的方法,具有很好的实用价值。     

河南老湾花岗岩的源区成分模拟

老湾花岗岩的岩石化学、稀土元素和同位素特征指示出老湾花岗岩源于下地壳经部分熔融作用形成。源岩中含有壳源和幔源物质,具类似于高钾钙碱性安山岩的岩石化学特点。详细的研究表明了早元古界桐柏山群不能成为老湾花岗岩的源岩。模拟的太古代岩系岩石化学成分经高程度的部分熔融作用可以形成老湾花岗岩。     

关于某些分块矩阵的逆矩阵的注记

针对次对角线方向,给出了某些分块矩阵的逆矩阵的存在条件及逆矩阵的表示形式.     

岩体动态响应分析程序的微机化及其应用

开发微机化的数值分析程序是推广数值方法在岩体工程中应用的一条有效途径。本文首先介绍一种微机数值分析程序的内存数据处理方法，然后介绍据此对岩体动态响应分析的二维非线性有限元程序ＤＹＮＰＡＫ的微机化改造和应用实例。     

Body Fuzzy Pattern Recognition in Woman Basic Block Design

Basic block is the foundation of clothing construction design because it is the media between body and clothes and the fitness of clothes should be based on the accuracy of basic block. That needs us to recognize body not to record it. This paper reports the Algorithm of woman body fuzzy pattern recognition. It is organized in three sections: (i) extracting woman body feature; (ii) establishing membership functions of feature indexes; (iii) presenting an Algorithm for woman body fuzzy pattern recognition by example.     

用地球化学特征判别川北含铀砂岩

文章阐述了川北砂岩型铀矿床的地球化学特征。根据能谱测量，用Ｕ，Ｔｈ，Ｋ元素的丰度和比值，获得铀富集的有利条件、不利条件。通过伽马能谱法（测Ｕ，Ｔｈ，Ｋ）和Ｘ射线荧光法（测Ａｓ，Ｂａ），区分含铀浅色砂岩和不含铀浅色砂岩，区分红色砂岩（红色泥岩）与浅色砂岩，缩小川北砂岩找铀矿的范围。     

用分段回归方法计算孔隙结构的分形维数

储层岩石的孔隙空间具有良好的分形特征,孔隙结构的分形维数可以用来定量描述孔隙结构的复杂程度。应用分形几何的原理,推导了储层岩石不同孔隙分布和毛细管压力曲线的分形几何模型。根据毛管压力曲线资料,用分段回归的方法计算了不同孔隙结构的分形维数。计算结果表明,用分段回归方法计算孔隙结构的分形维数能更好地反映孔隙结构的实际情况。若孔隙大小相差不大,孔隙结构的分形维数相等或比较接近;若孔隙大小相差较大、非均质性较强,得到的孔隙结构分形维数不同。     

IEEE 802.16a协议物理层ST-OFDM的研究

介绍了IEEE 802.16a协议,并以802.16a协议中的3种物理层实现方式之一--WirelessMAN-OFDM PHY为例,对STC(空时编码)和OFDM(正交频分复用)的结合应用(STC-OFDM)进行了阐述,同时对其BER(误比特率)性能进行了仿真,对仿真结果进行了分析.     

Characteristics of carbonate gas pool and multistage gas pool formation history of Hetianhe gas field, Tarim Basin, Northwest China

<正> Hetianhe is a big carbonate gas field which isfound and demonstrated in the period of "Chinese NationalNinth 5-Year Plan". The proved reserve of Hetianhe gas fieldis over 600 ×10⁸ m³. Its main producing layers are Carbon-iferous bioclastic limestone and Ordovician carbonate com-posed of buried hill. The former is stratified gas pool withwater around its side, and the latter is massive gas pool withwater in its bottom. The gases in the gas pools belong to drygases with normal temperature and pressure systems. Basedon the correlation of gas and source rock, the gases aremainly generated from Cambrian source rocks. According tothe researches on source rock and structure evolution, andthe observations on the thin section to reservoir bitumen andthe studies on homogenization temperature of fluid inclu-sions, the gas pool has been identified and divided into threeformation periods. The first is Late Caledonian when the oilgenerated from the Cambrian source rocks and migratedalong faults, as a form of liquid facies into Ordovician carbonate res-ervoir and accumulated there. After that, the crustuplifted, the oil reservoir had been destroyed. The second isLate Hercynian when condensate gases generated from theCambrian source rocks and migrated into Ordovician res-ervoir, as a form of liquid facies. Since the fractures hadreached P strata, so the trap might have a real poor preser-vation condition, and the large-scale gas pool formation hadnot happened. The third gas reservoir formation period oc-curred in Himalaya. The fractures on both sides of Hetianhegas field developed violently under the forces of compression,and thus the present fault horst formed. The dry gases gen-erated from Cambrian source rocks and migrated upwardsas the form of gas facies into Ordovician and Carboniferousreservoirs, and the large gas pool as discovered at presentwas formed finally.     

新疆若羌县赤石山变质核杂岩研究

新疆北山裂谷带西缘若羌县赤石山地区存在大型变质核杂岩构造。其下拆离盘为古元古界结晶基底杂岩 ,上拆离盘为中元古界白湖群变质岩系 ,滑脱拆离带为已变形的大型韧性正断层。核杂岩南、北侧发育上叠盆地 ,北侧形成“年轻”正断层及同构造期岩浆岩。变质核杂岩的形成与晚古生代北山陆内裂谷区域伸展有直接联系。该区变质核杂岩的首次厘定 ,对深化北山裂谷的研究具有重要意义