COM技术在地球化学数据处理系统中的应用   总被引：1，自引：1，他引：0  

邱玉宝  胡光道  F.Al Bassam 《物探化探计算技术》2002,24(4):352-358

区域地球化学信息作为反映矿产资源区域特性的重要指标,在区域矿产资源评价中占有重要的地位,为了有效利用该指标,这就要求研究实用可行的数据处理系统来更好地对地球化学数据进行处理,随着数据处理方法的不断完善和地矿信息化工作的不断提高,要求处理系统本身具有可重用性,可扩展性,高效性等特点,而组件对象模型（COM）技术提供了一种如何建立可重用、可扩展组件,以及如何通过组件高效率地构筑应用程序的一个规范,使得软件系统以组件方式集成成为可能,作者在COM技术内涵基础上,结合地球化学数据处理系统目前存在的若干问题,探讨了COM组件技术在地球化学数据处理系统中的应用,并对数据处理组件进行了分析设计。  相似文献   

Use of Solute and Isotopic Composition of Ground Water to Constrain the Ground Water Flow System of the Azraq Area, Jordan   总被引：1，自引：0，他引：1  

Nizar S. Abu-Jaber  Ali Jawad Ali  Khaldoon Al  Qudah 《Ground water》1998,36(2):361-365

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Storm-water hydrograph separation of run off from a mine-tailings impoundment formed by thickened tailings discharge at Kidd Creek, Timmins, Ontario   总被引：1，自引：0，他引：1  

Tom A. Al  David W. Blowes 《Journal of Hydrology》1996,180(1-4):55-78

The Kidd Creek Cu---Zn sulphide mine is located near Timmins, Ontario. Mill tailings are thickened and deposited as a thickened slurry in a circular, conical-shaped pile with an area of approximately 1200 ha. Deposition of tailings as a thickened slurry results in a relatively uniform grain-size distribution and hydraulic conductivity, and a thick tension-saturated zone above the water table. The tailings are drained by numerous small, ephemeral stream channels, which have developed in a radial pattern. During storms, water from these streams collects in catchment ponds where it is held before treatment. The contribution of tailings pore water to the run off is of interest because of the potential for discharge of pore water containing high concentrations of Fe(II)-acidity, metals and SO₄ to the stream. Hydraulic head measurements, measurements of water-table elevation and groundwater flow modelling were conducted to determine the mechanisms responsible for tailings pore water entering the surface streams. Chemical hydrograph separation of storm run off in one of these streams, during three rainfall events, using Na and Cl as conservative tracers, indicates that the integrated tailings pore water fraction makes up between less than 1 % and 20% of the total hydrograph. This range is less than the maximum fraction of tailings pore water of 22–65% reported for run off from a conventional tailings deposit. At this site, preferential flow through permeable fractures may be the dominant mechanism causing discharge of tailings pore water to storm run off. Estimates of the mass of Fe(II) that discharges to the surface run off from the pore water range up to 2800 mg s⁻¹ during a moderate intensity, long duration rainfall event. The greatest potential for discharge of significant masses of solutes derived from the pore water exists during long duration rainfall events, when the water table rises to the surface over large areas of the tailings impoundment.  相似文献   

Improved Geological Interpretation Using Landsat TM Data in Lancang-Jinghong Area, Yunnan Province, China     

BassamFAIBassam 《中国地质大学学报(英文版)》2003,14(1):52-58

Landsat TM digital spectral data of Lancang-Jinghong area (Yunnan Province) has been used for the purpose of geological interpretation. To meet this object, different image processing tech-niques including selected band color composites, principal component analysis and IHS decorrelation stretching are used to improve the discrimination of different lithologicai and structural features in the area. It was found that IHS decorrelation stretching images obtained from the transformation of false color composite 741 (in red, green and blue) provided the best results based on the original data. By combining the characteristics of images produced by different approaches and other canonically trans-formed images with available geological data and surface observations, the geological interpretation could be done with satisfactory degree of accuracy.  相似文献   

GIS Predictive Model for Producing Hydrothermal Gold Potential Map Using Weights of Evidence Approach in Gengma Region, Sanjiang District, China     

BassamFAIBassam 《中国地质大学学报(英文版)》2003,14(3):283-292

Gengma region, Sanjiang district is known to have some large-scale gold deposits. GIS predictive model for hydroghermal gold potential was carried out in this region using weights of evidence modeling technique. Datasets used include large-scale hydroghermal gold deposit records, geological, geophysical and remote sensing imagery. Based on the geological and mineral characteristics of areas with known gold occurrences in Sanjiang, several geological features were thought to be indicative of areas with potential for the occurrence of hydroghtermal gold deposits. Indicative features were extracted from geoexploration datasets for use as input in the predictive model. The features include host rock lithology, geologic structures, wallrock alteration and associated (volcanic-plutonic) igneous rocks. To determine which of the indicative geological features are important spatial predictors of area with potential for gold deposits, spatial analysis was done through the modeling method. The input maps were buffered and the optimum distance of spatial association for each geological feature was determined by calculating the contrast and studentized contrast. Five feature maps were converted to binary predictor patterns and used as evidential layers for predictive modeling. The binary patterns were integrated in two combinations, each of which consists of four patterns in order to avoid over prediction due to the effect of duplicate features in the two structural evidences. The two produced potential maps define almost similar favorable zones. Areas of intersections between these zones in the two potential maps placed the highest predictive favorable zones in the region.  相似文献   

Adsorption of dimethoate and 2,4-D on Jordan Valley soils and their environmental impacts   总被引：1，自引：0，他引：1  

M. Al Kuisi 《Environmental Geology》2002,42(6):666-671

The adsorption process of dimethoate and 2,4-dichloro-phenoxy acetic acid (2,4-D) on Jordan Valley soils from aqueous solution at 25 °C has been studied. The adsorption isotherms may be classified as L-type of the Giles classification. The K_ads values (Freundlich equation) vary between 1.01 (JV5) and 10.36 (JV7) for dimethoate insecticide and between 4.41 (JV5) and 14.87 (JV7) for 2,4-D herbicide, depending on the soil type. The adsorption of 2,4-D herbicide on soils in the study area is about threefold higher than that of dimethoate insecticide. The adsorption process of dimethoate and 2,4-D pesticides seem to be primarily controlled by the organic matter content of the soils and the clay content (most especially montmorillonite).  相似文献   

Découverte de niveaux phosphatés associés à des restes de vertébrés dans les dépôts carbonatés du Coniacien–Santonien du Jabal Abtar : épisode précoce de la phosphatogenèse sénonienne des Palmyrides (Syrie centrale)     

A Khaled Al Maleh  Nathalie Bardet 《Comptes Rendus Geoscience》2003,335(4):391-400

Sedimentologic study of carbonated sediments of the Rmah-I member (Coniacian–Santonian) of Jabal Abtar, central southern Palmyrides (Central Syria), uncovers phosphatic levels, associated with marine vertebrate remains, that give evidence of an early episode of the Senonian phosphatogenesis in the Palmyrides. Sedimentary sequence analysis reveals a gradual marine transgression during the Senonian. Phosphatic sedimentation occurred in a shallow neritic marine environment almost connected with the open sea. Condensed sedimentation could have contributed to the phosphatogenesis. To cite this article: A.K. Al Maleh, N. Bardet, C. R. Geoscience 335 (2003).  相似文献   

Fault-related folds and along-dip segmentation of breaching faults: syn-diagenetic deformation in the south-western Sirt basin, Libya     

L. Fodor  S. M. Turki  H. Dalub  A. Al Gerbi 《地学学报》2005,17(2):121-128

Field examples of fault-related folds were observed in the south-western margin of the Sirt basin, south-central Libya. Single or paired (conjugate) monoclines, drape synclines, special drag faults can be put in a geometric and evolutionary model, which describes the propagation of basement faults to overlying sediments. At the first stage of evolution the propagating normal or oblique-slip faults show segmentation along-dip direction. Fault segments are separated by continuous, moderately to strongly bended horizons, which show different degrees of diagenesis than surrounding intervals. Fault-related folding and faulting was coeval with lithification of certain carbonate levels. Their gradual cementation increased the rigidity of layers promoting discrete faulting and breaching of fault-related folds. However, folding can be maintained up to the extent when layer dip approaches the dip of the propagating fault zone. This type of deformation can be characteristic for sequences consisted of lithified carbonates sandwiched between thicker marl/shale intervals.  相似文献   

Role of fluvial and structural processes in the formation of the Wahiba Sands, Oman: A remote sensing perspective   总被引：1，自引：0，他引：1  

C.A. Robinson  F. El-Baz  T.M. Kusky  M. Mainguet  F. Dumay  Z. Al Suleimani  A. Al Marjeby 《Journal of Arid Environments》2007,69(4):676-694

The Wahiba Sands in northeastern Oman are bordered on the north, south and west by highlands. Remote sensing data are used to characterize the region between 19–23.5°N and 56.5–60°E by mapping surface and near-surface drainage, faults and fractures and aeolian features. It is suggested that the sands were originally deposited with surface runoff from the principal wadis and fluvially reworked fault zones, which define the northeastern and southwestern margins. These fluvial processes resulted in the accumulation of the vast groundwater resources now stored there. During dry climates, wind became the principal modification regime and it began to sort and shape the sediments into the dune forms that characterize today's Wahiba region. The thickness of the sands reflects the depth of the basin in which they lie. The center of the basin is filled with the thickest sand (the High Sands) and contains the highest groundwater concentrations. Presently, aeolian reworking dominates in the Wahiba region, although the Low and the Peripheral Sands continue to experience some fluvial action from occasional, seasonal rainfall. Even though dry conditions dominate today, it is clear that similar to the Sahara of North Africa, the surface sands of the Wahiba basin are indicators of groundwater occurrence.  相似文献   

Structure,chemical composition,and formation conditions of the Berezovskii volcanic complex in the southern Magnitogorsk megazone (Southern Urals)     

A. V. Rudakova  N. V. Pravikova  Al. V. Tevelev 《Moscow University Geology Bulletin》2007,62(1):40-45

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