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1.
《地下水》2021,(4)
以水城观音山铁矿区为例,在收集资料和调查的基础上,对矿区水文地质概况;开采前后的充水因素、补径排条件、各矿体静止水位标高;开采后的水文地质变化特征等进行了分析、总结;重新划定了水文地质勘查类型。其结果为:矿山经过多年的开采,水文地质条件发生了极大变化,表现为:地下水位、排水量大幅度下降;井、泉大量干涸;河流、沟谷流量明显减少;但采空区积水、入渗补给条件、充水因素等发生变化。对老矿山开采后的水文地质特征适时动态认识与评价,为正确指导矿山安全生产提供有价值的水文地质资料。  相似文献   

2.
通过对桦甸市腰(土仓)子690铁矿矿区水文地质特征的分析,阐明了矿区的水文地质条件,确定了未来矿床开采技术条件。  相似文献   

3.
以偃龙煤田西部岩溶水系统为实例,分析了单斜岩溶水系统特征及其对烟矿开采的影响,阐明了单斜岩溶水系统中,补级区的水文地质条件相对简单,岩溶水对煤矿开采的影响较小。而在系统的排泄区,岩溶较为发育,水文地质条件较为复杂,因此岩溶水对煤矿开采的威胁较大。  相似文献   

4.
李赛  刘宇成  吴万红 《云南地质》2011,30(4):490-493
对跑马坪矿段地质、水文地质条件的调查,划分水文地质单元,对比矿段开采前后水文地质条件的变化、矿段涌水量与大气降水的关系等,分析矿段地下水水文地质特征。  相似文献   

5.
本文通过对矿区资料综合研究,分析了矿床含隔水层水文地质特征、断裂构造特征水文地质、地下水补径排特征,分析了矿床充水水源、充水通道等充水因素,厘清了矿床水文地质边界,认为矿床水文地质条件中等;在此基础上,结合矿山开采设计方案,选择解析法—"大井法"和"狭长水平坑道法"建立计算模型,分别计算预测了地下水矿坑涌水量;经分析对...  相似文献   

6.
李良云 《云南地质》2002,21(3):316-321
个旧东区为锡矿生产的主要基地。随着矿床开采水平不断下降,开采技术条件变得十分复杂,本文根据大量的实际资料,对矿区、矿田的水文地质特征进行分析研究,揭示了矿区地下水的运动、迁移、富集规律,对进一步开展矿区地下水水文地质工作具有指导意义。  相似文献   

7.
根据姚楼井田地质勘探所取得的资料,分析了B煤开采上覆岩土层的水文地质结构及工程地质特征,对该井田厚松散层含水层下近露头带开采的防水煤岩柱尺寸作出了评价,为开采设计提供了初步依据。  相似文献   

8.
山东省地下水资源及其潜力评价   总被引:2,自引:0,他引:2  
通过对山东省水文地质条件、地下水赋存特征、地下水开采现状及其动态特征进行系统研究的基础上,计算评价了全省地下水天然补给资源量、可开采资源量、开采程度和剩余可开采资源量。论述了地下水开采资源潜力的计算评价原则和判别标志,确定了全省主要的地下水资源潜力分布区。  相似文献   

9.
太平煤矿深厚土层的水文地质工程地质性质   总被引:1,自引:0,他引:1  
依据对太平煤矿3号煤区深厚土层的水文地质与工程地质勘测及室内外实验结果,分析了主要的水文地质与工程地质特征及其对3号煤开采的影响,对矿区防水煤岩柱留设高度进行了合理确定。   相似文献   

10.
淮南煤田地下水类型及其特征   总被引:2,自引:0,他引:2  
周士荣 《安徽地质》2008,18(3):221-225
淮南煤田为全隐蔽煤田,松散层厚度大,主要含煤地层为二叠系。通过大量的勘探资料及生产矿井的开采成果,对影响煤层开采的地下水进行了分类,并对其水文地质特征进行了阐述,为新区的建井与开采提供了参考资料和决策依据。  相似文献   

11.
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.  相似文献   

12.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

13.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.  相似文献   

14.
Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions. To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.  相似文献   

15.
PALEONTOLOGY     
正20141596 Liu Yunhuan(School of Earth Sciences and Resources,Chang’an University,Xi’an 710054,China);Shao Tiequan Early Cambrian Quadrapyrgites Fossils of Xixiang Boita in Southern Shaanxi Province(Journal of Earth Sciences and Environment,ISSN1672-6561,CN61-1423/P,35(3),2013,p.39-43,3 illus.,20 refs.)  相似文献   

16.
正20141719 Chen Zhijun(State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China);Chen Jianguo Automated Batch Mapping Solution for Serial Maps:A Case Study of Exploration Geochemistry Maps(Journal of Geology,ISSN1674-3636,CN32-1796/P,37(3),2013,p.456-464,2 illus.,2 tables,10 refs.)  相似文献   

17.
正20140962 Chen Fenning(Xi’an Institute of Geology and Mineral Resources,Xi’an710054,China);Chen Ruiming Late Miocene-Early Pleistocene Ostracoda Fauna of Gyirong Basin,Southern Tibet(Acta Geologica Sinica,ISSN0001-5717,CN11-1951/P,87(6),2013,p.872-886,6illus.,56refs.)  相似文献   

18.
PETROLOGY     
正1.IGNEOUS PETROLOGY20142008Cai Jinhui(Wuhan Center,China Geological Survey,Wuhan 430205,China);Liu Wei Zircon U-Pb Geochronology and Mineralization Significance of Granodiorites from Fuzichong Pb-Zn Deposit,Guangxi,South China(Geology and Mineral Resources of South China,ISSN1007-3701,CN42-1417/P,29(4),2013,p.271-281,7illus.,  相似文献   

19.
正20141205Cheng Weiming(State Key Laboratory of Resources and Environmental Information System,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China);Xia Yao Regional Hazard Assessment of Disaster Environment for Debris Flows:Taking Jundu Mountain,Beijing as an  相似文献   

20.
正20141266Fan Chaoyan(Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes,Guangzhou 510275,China);Wang Zhenghai On Error Analysis and Correction Method of Measured Strata Section with Wire Projection Method(Journal of  相似文献   

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