首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献,搜索用时 78 毫秒
1.
这次小口径钻探工作座谈会,从五月九日开始,到今天结束了。会议开始时钮形平同志讲了话,他回顾了以往小口径钻探所取得的成绩和经验,指出了当前存在的问题。到会同志一致同意这个讲话。会议期间,有十多位同志在大会上介绍了经验,大家还参观了湖南局四○五队茶田矿区的施工现场,此后又分组进行了专题座谈讨论。通过会议,沟通了情况,交流了经验,商订了今后发展小口径钻探的初步规划,明确了有关技术政策,从而统一了思想,坚定了信心,对这项新技术的推广必将产生很大的推动作用。这里,我根据会议讨论的情况,谈几个问题。  相似文献   

2.
山东省第二轮区域地质调查主要进展   总被引:5,自引:0,他引:5  
山东省第二轮区调工作始于70年代末,完成了1:20万填图面积112326km^2和1:5万填图面积63137km^2,基础地质研究取得巨大进展:地层方面,建立了一些新的岩石地层单位,重新厚定了地层层序,进行了以岩石地层为主的地层多重划分对比,对各时代地层的沉积作用进行了探讨;侵入岩方面,初步完成了我省侵入岩岩石谱系单位的统一划分工作,研究了侵入岩的演化,成因、侵位机制和形成时代,尤其是从前寒武纪基底中识别出大量变形变质或未变形变质侵入岩,并对其进行了岩石谱系单位划分;变质岩方面,分析了原岩建造及形成环境,划分了变质岩系的变质相,变质相系和叠加变质作用,测定了大量pT数据,确定了一些变质岩的PTt轨迹,对变质作用类型进行了研究,发现了高压,超高压变质带并对其进行了探讨;构造方面,发现了研究了大量韧性变形带,对胶南-威海造山带7和郯庐断裂带进行了深入研究,矿产方面,主要是对各种矿产的成因和形成规律进行了探讨。  相似文献   

3.
陈清涛  黄启海 《地下水》2009,31(6):117-118
冠县是一老井灌区农业县,水资源严重匮乏,属水危机区,近几年来,结合区内缺水现状和农作物种植情况,因地制宜,坚持“以人为本,创建和谐水利”的原则,大力推广发展了管灌、地膜灌、喷灌、滴灌、微喷灌等节水工程,推广应用了农艺节水技术,实行科学用水、计划用水,优化节水灌溉制度,缓解了区内水资源的供需矛盾,实现了水资源优化配置,达到了农业增效、农民增收的目的,取得了明显的效果,有利地促进了全县经济社会的可持续发展。  相似文献   

4.
自备水源缺乏统一管理,缺少监督,效率低下,地下水超采严重,形成地下漏斗区,严重影响了城市安全;地下水质较差,威胁城区居民身体健康,关闭自备水源,统一供应优质水源,既节约了水资源,又保障了居民健康,给供水系统也带来了利益。  相似文献   

5.
许静  黄启海  宫延之  许刚 《地下水》2003,25(3):155-155,162
冠县水资源严重匮乏,属水危机区。近十几年来,结合区内缺水现状和农作物种植情况,因地制宜,推广发展了管灌、地膜灌、喷灌、滴灌、微喷灌等节水工程。推广应用了农艺节水技术,实行科学用水,计划用水,优化节水灌溉制度,取得了明显的效果,缓解了区内水资源的供需矛盾,实现了水资源优化配置,促进了经济社会的可持续发展。  相似文献   

6.
应用充气泡沫泥浆效益显著   总被引:1,自引:0,他引:1       下载免费PDF全文
王秉晋 《探矿工程》1993,(2):9-11,14
研究并分析了充气泡沫泥浆,介绍了配制方法和泥浆性能,在完整地层使用该泥浆钻进提高了效率,在漏失地层使用,可防漏治漏,提高了工程质量,降低了成本。  相似文献   

7.
凌泽民 《中国岩溶》1996,15(1):124-131
论文讨论了宁波市的主要环境地质问题并提出了相应的防治对策,作者对由于长期开采承压含水层中的地下水导致的地面沉降及海水入侵问题进行了探讨了,研究评价了软土地基的稳定性,在通过资料收集,分析,对软土的变形及强度特性的基础上进行研究,建立了岩土数据库,并对软土的微结构及演化历史作了定量研究,还综合分析了影响地基稳定的各种因素,利用模糊数学对地基稳定性进行了评价,在考虑地面沉降的现状及其影响因素的情况下,  相似文献   

8.
王汪凯 《江苏地质》1997,21(4):248-252
在分析了温度,压力诸因素与金刚石产,质量之间关系的基础上,提出了合理,高效的合成工艺方案,特别是在实施合成工艺方面,提出了见解和措施,并且收到了较好的实际效果。  相似文献   

9.
江川 《核地知与行》2010,(1):F0004-F0004
2月2日,局在南昌召开了2010工作会议,会议认真总结了2009年度的工作,表彰了先进,研究部署了今年的任务。副省长洪礼和给大会发来贺信,对我局工作给予了充分肯定,对今后的发展提出了殷切希望和要求。  相似文献   

10.
彭放  徐中祥 《地球科学》1995,20(1):63-67
首先提出了灰色系统关联度的一个新模型,分析了该模型的性质,其次讨论了应用该模型和关联滤波法预测矿体埋深的问题,然后进行了理论模型试算,证实了本方法的理论效果,最后,指出了新模型的主要优点。  相似文献   

11.
Komatiites are mantle-derived ultramafic volcanic rocks. Komatiites have been discovered in several States of India, notably in Karnataka. Studies on the distribution of trace-elements in the komatiites of India are very few. This paper proposes a simple, accurate, precise, rapid, and non-destructive wavelength-dispersive x-ray fluorescence (WDXRF) spectrometric technique for determining Sc, V, Cr, Co, Ni, Cu, Zn, Rb, Sr, Y, Zr, Nb, Ba, Pb, and Th in komatiites, and discusses the accuracy, precision, limits of detection, x-ray spectral-line interferences, inter-element effects, speed, advantages, and limitations of the technique. The accuracy of the technique is excellent (within 3%) for Sc, V, Cr, Co, Ni, Cu, Zn, Rb, Sr, Zr, Nb, Ba, Pb, and Th and very good (within 4%) for Y. The precision is also excellent (within 3%) for Sc, V, Cr, Co, Ni, Cu, Zn, Rb, Sr, Y, Zr, Nb, Ba, Pb, and Th. The limits of detection are: 1 ppm for Sc and V; 2 ppm for Cr, Co, and Ni; 3 ppm for Cu, Zn, Rb, and Sr; 4 ppm for Y and Zr; 6 ppm for Nb; 10 ppm for Ba; 13 ppm for Pb; and 14 ppm for Th. The time taken for determining Sc, V, Cr, Co, Ni, Cu, Zn, Rb, Sr, Y, Zr, Nb, Ba, Pb, and Th in a batch of 24 samples of komatiites, for a replication of four analyses per sample, by one operator, using a manual WDXRF spectrometer, is only 60 hours.  相似文献   

12.
Susan E. Hogg 《Earth》1982,18(1):59-76
Following McGee's (1897) use of the term sheetflood, there developed a variety of conflicting opinions and numerous terminologies relating to this process, many of which are ill-considered and poorly defined. A classification system is devised on both a hydrologic and geomorphic basis which dispenses with many superfluous terms that have been used with respect to sheetfloods. Magnitude of a storm is expressed in terms of the amount of surface runoff generated from a given storm due to the surface conditions.A sheetflood is defined as a sheet of unconfined flood water moving down a slope. The frequency of a sheetflood is relatively low while its magnitude is relatively great. Sheetflow is defined as relatively high-frequency, low-magnitude overland flow occurring in a continuous sheet and is restricted to laminar flow conditions. Sheetwash, a term of geomorphic origin, is considered to be redundant and is superseded by the more meaningful term rainwash defined as the washing action of rain on slopes.  相似文献   

13.
This paper reports the first results of a study of 11 isotope systems (3He/4He, 40Ar/36Ar, 34S/32S, 65Cu/63Cu, 62Ni/60Ni, 87Sr/86Sr, 143Nd/144Nd, 206–208Pb/204Pb, Hf–Nd, U–Pb, and Re–Os) in the rocks and ores of the Cu–Ni–PGE deposits of the Norilsk ore district. Almost all the results were obtained at the Center of Isotopic Research of the Karpinskii All-Russia Research Institute of Geology. The use of a number of independent genetic isotopic signatures and comprehensive isotopic knowledge provided a methodic basis for the interpretation of approximately 5000 isotopic analyses of various elements. The presence of materials from two sources, crust and mantle, was detected in the composition of the rocks and ores. The contribution of the crustal source is especially significant in the paleofluids (gas–liquid microinclusions) of the ore-forming medium. Crustal solutions were probably a transport medium during ore formation. Air argon is dominant in the ores, which indicates a connection between the paleofluids and the atmosphere. This suggests intense groundwater circulation during the crystallization of ore minerals. The age of the rocks and ores of the Norilsk deposits was determined. The stage of orebody formation is restricted to a narrow age interval of 250 ± 10 Ma. An isotopic criterion was proposed for the ore-bearing potential of mafic intrusions in the Norilsk–Taimyr region. It includes several interrelated isotopic ratios of various elements: He, Ar, S, and others.  相似文献   

14.
We describe the new mineral species titanium,ideally Ti,found in the podiform chromitites of the Luobusha ophiolite in Tibet,People’s Republic of China.The irregular crystals range from 0.1 to 0.6 mm in diameter and form an intergrowth with coesite and kyanite.Titanium is silver grey in colour,the luster is metallic,it is opaque,the streak is grayish black,and it is non-fluorescent.The mineral is malleable,has a rough to hackly fracture and has no apparent cleavage.The estimated Mohs hardness is 4,and the calculated density is 4.503 g/cm3.The composition is Ti 99.23-100.00 wt%.The mineral is hexagonal,space group P63 /mmc.Unit-cell parameters are a 2.950(2),c 4.686(1),V 35.32(5) 3,Z = 2.The five strongest powder diffraction lines [d in(hkl)(I/I0)] are: 2.569(010)(32),2.254(011)(100),1.730(012)(16),1.478(110)(21),and 0.9464(121)(8).The species and name were approved by the CNMNC(IMA 2010–044).  相似文献   

15.
Mining induced subsidence can significantly affect mining costs where major surface facilities and natural environment need to be protected. Overburden grout injection is a technology used to control coal mine subsidence by injecting the mine waste material extracted from the coal back into the inter-burden rock during longwall mining. The flowing slurry is here categorised as a nonlinear viscous cohesive (Bingham plastic) fluid. During longwall mining the grout slurry is pumped into the separated beds of the rock mass through a central vertical borehole, which is drilled deep into the inter-burden rock strata above the coal seam. However, a blockage can occur in the injection system when the slurry velocity falls below a certain critical threshold velocity, indicating a material phase change from cohesive-viscous to cohesive-frictional. In situ field injection tests through boreholes have been simulated at a smaller scale at the CSIRO laboratory in Brisbane by pumping the slurry through a radial disk (gap = 4 mm) from its centre. Laboratory experiments indicate a general, nonlinear, cohesive, viscous, frictional model for shear behaviour of the slurry, in which the material shear parameters are functions of the disk radial distance. Complete dimensional and dimensionless analytical solutions have been developed based on an approach related to Bingham–Herschel–Bulkley fluid mechanics. The derived formulae include relations for minimum pump pressure, local pressure and pressure gradient, wall shear stress, volume rate, velocity and velocity gradient. The theoretical results match the experimental measurements. The experiments covered slurries with maximum particle sizes of 0.5 to 2 mm with about 50% being larger than 100 µm. The viscosities at the various solids concentrations were measured with a standard torsion viscometer. This study differs from the previous research in several distinct aspects, namely, consideration of the variable shear parameters rather than fixed values, inclusion of total nonlinear behaviour, and implementation of a friction function to mimic behaviour of the deposited and consolidating stiff slurry, which can cause a significant pressure rise as a result of the increased shear resistance.  相似文献   

16.
The Kay Tanda epithermal Au deposit in Lobo, Batangas is one of the Au deposits situated in the Batangas Mineral District in southern Luzon, Philippines. This study aims to document the geological, alteration, and mineralization characteristics and to determine the age of the mineralization, the mechanism of ore deposition, and the hydrothermal fluid characteristics of the Kay Tanda deposit. The geology of Kay Tanda consists of (i) the Talahib Volcanic Sequence, a Middle Miocene dacitic to andesitic volcaniclastic sequence that served as the host rock of the mineralization; (ii) the Balibago Diorite Complex, a cogenetic intrusive complex intruding the Talahib Volcanic Sequence; (iii) the Calatagan Formation, a Late Miocene to Early Pliocene volcanosedimentary formation unconformably overlying the Talahib Volcanic Sequence; (iv) the Dacite Porphyry Intrusives, which intruded the older lithological units; and (v) the Balibago Andesite, a Pliocene postmineralization volcaniclastic unit. K‐Ar dating on illite collected from the alteration haloes around quartz veins demonstrated that the age of mineralization is around 5.9 ± 0.2 to 5.5 ± 0.2 Ma (Late Miocene). Two main styles of mineralization are identified in Kay Tanda. The first style is an early‐stage extensive epithermal mineralization characterized by stratabound Au‐Ag‐bearing quartz stockworks hosted at the shallower levels of the Talahib Volcanic Sequence. The second style is a late‐stage base metal (Zn, Pb, and Cu) epithermal mineralization with local bonanza‐grade Au mineralization hosted in veins and hydrothermal breccias that are intersected at deeper levels of the Talahib Volcanic Sequence and at the shallower levels of the Balibago Intrusive Complex. Paragenetic studies on the mineralization in Kay Tanda defined six stages of mineralization; the first two belong to the first mineralization style, while the last four belong to the second mineralization style. Stage 1 is composed of quartz ± pyrophyllite ± dickite/kaolinite ± diaspore alteration, which is cut by quartz veins. Stage 2 is composed of Au‐Ag‐bearing quartz stockworks associated with pervasive illite ± quartz ± smectite ± kaolinite alteration. Stage 3 is composed of carbonate veins with minor base metal sulfides. Stage 4 is composed of quartz ± adularia ± calcite veins and hydrothermal breccias, hosting the main base metal and bonanza‐grade Au mineralization, and is associated with chlorite‐illite‐quartz alteration. Stage 5 is composed of epidote‐carbonate veins associated with epidote‐calcite‐chlorite alteration. Stage 6 is composed of anhydrite‐gypsum veins with minor base metal mineralization. The alteration assemblage of the deposit evolved from an acidic mineral assemblage caused by the condensation of magmatic volatiles from the Balibago Intrusive Complex into the groundwater to a slightly acidic mineral assemblage caused by the interaction of the host rocks and the circulating hydrothermal waters being heated up by the Dacite Porphyry Intrusives to a near‐neutral pH toward the later parts of the mineralization. Fluid inclusion microthermometry indicates that the temperature of the system started to increase during Stage 1 (T = 220–250°C) and remained at high temperatures (T = 250–290°C) toward Stage 6 due to the continuous intrusion of Dacite Porphyry Intrusives at depth. Salinity slightly decreased toward the later stages due to the contribution of more meteoric waters into the hydrothermal system. Boiling is considered the main mechanism of ore deposition based on the occurrence of rhombic adularia, the heterogeneous trapping of fluid inclusions of variable liquid–vapor ratios, the distribution of homogenization temperatures, and the gas ratios obtained from the quantitative fluid inclusion gas analysis of quartz. Ore mineral assemblage and sulfur fugacity determined from the FeS content of sphalerite at temperatures estimated by fluid inclusion microthermometry indicate that the base metal mineralization at Kay Tanda evolved from a high sulfidation to an intermediate sulfidation condition.  相似文献   

17.
Slope hummocks, a type of nonsorted patterned ground, are composed of stratified, organic, silty sand, and develop through the interaction of niveo-eolian deposition, solifluction, slopewash, and vegetation growth. Fields of hummocks show consistent patterns: forms on convex slopes increase in height downslope until the channel is reached, whereas those on convexo-concave slopes increase on the upper convexity but are buried by niveo-eolian deposition downslope of the snowbank remnant. These trends can be reproduced using a simple numerical model based on measured slope and snow depth profiles, sediment concentrations in the snow and solifluction rates. The model indicates that hummocks transit slopes of 20-40 m in about 2-4 ka, a time-frame that is plausible given site emergence, measured rates of solifluction, and published dates for organic horizons within hummocks on northern Ellesmere Island. Sensitivity analyses show that long-term effect of climate warming on hummock heights may differ depending on whether it is accompanied by precipitation increase or decrease. The required combination of two-sided freezing to promote plug-like movement, incomplete vegetation cover and thin snow that enable eolian erosion during winter and spring, and vegetation growth in snow-bed sites to stabilize niveo-eolian deposits may explain why these forms are important regionally but apparently are not present throughout the Arctic.  相似文献   

18.
This paper investigates sweat to deepen theoretical understandings of how gender is lived. To do so we adopt a visceral approach that opens possibilities of thinking geographically about the affective ties and emotional bonds of sweat to engage with feminist logics of embodiment. Our interest is in what sweaty bodies can ‘do’. Attention is given to the way that affects, emotions and sensations associated with being sweaty, smelling sweat, as well as touching one’s own sweat, and that of others, provides insights into the gendered lives of people as they move through different context. Our analysis of how gendered is lived through sweaty bodies draws on ‘Summer Living’ narratives of 17 participants who understand themselves as men and live in Wollongong, a city of around 280,000 people on the east coast of New South Wales, Australia. We illustrate the theoretical significance of thinking about sweat for gender and geography by discussing the ambiguity, proximity and collectivity of sweaty bodies; and, the fragility, multiplicity and vitality of sweaty bodies. To conclude we outline how a visceral approach provides possibilities to improve household sustainability policies.  相似文献   

19.
A new mineral species, named naquite(FeSi), is found in the podiform chromitites of the Luobusha ophiolite in Qusong County, Tibet, China. The detailed composition is Fe 65.65, Si 32.57 and Al 1.78 wt%. The mineral is cubic, space group P213. The irregular crystals range from 15 to 50 μm in diameter and form an intergrowth with luobusaite. Naquite is steel grey in color, opaque, with a metallic lustre and gives a grayish-black streak. The mineral is brittle, has a conchoidal fracture and no apparent cleavage. The estimated Mohs hardness is 6.5, and the calculated density is 6.128 g/cm3. Unit-cell parameters are a 4.486 (4) ?, V 90.28 (6) ?3, Z=4. The five strongest powder diffraction lines [d in ? (hkl) (I/I0)] are: 3.1742 (110) (40), 2.5917(111) (43), 2.0076 (210) (100), 1.8307 (211) (65), and 1.1990 (321) (36). Originally called ‘fersilicite’, the species and new name have now been approved by the CNMNC (IMA 2010–010).  相似文献   

20.
We collected groundwaters in and around a large (313 Mt at 1.08% Cu and 0.3% cutoff) undisturbed porphyry copper deposit (Spence) in the hyperarid Atacama Desert of northern Chile, which is buried beneath 30–180 m of Miocene piedmont gravels. Groundwaters within and down-flow of the Spence deposit have elevated Se (up to 800 μg/l), Re (up to 31 μg/l), Mo (up to 475 μg/l) and As (up to 278 μg/l) concentrations compared to up-flow waters (interpreted to represent regional groundwater flow). In contrast, Cu is only elevated (up to 2036 μg/l) in groundwaters recovered from within the deposit; Cu concentrations are low down gradient of the deposit. The differential behavior of the metals/metalloids occurs because the former group dissolves as anions, enhancing their mobility, whereas the base metals dissolve as cations and are lost from solution most likely through adsorption to clay surface exchange sites and through formation of secondary copper chlorides, carbonates, and oxides. Most groundwaters within and down-flow of the deposit have Eh–pH values around the FeII/FeIII phase boundary, limiting the impact of Fe-oxyhydroxides on oxyanions mobility. Se, Re, Mo, and As are all mobile (with filtered/unfiltered samples ~ 1) to the limit of sampling 2 km down gradient from the deposit. The increase in ore-related metals, metalloids, and sulfate and decrease in sulfate–S isotope ratios (from values similar to regional salars, + 4 to + 8‰ δ34SCDT to lower values closer to hypogene sulfides, + 1 to + 4‰ δ34SCDT) is consistent with active water–rock reactions between saline groundwaters and the Spence deposit. It is likely that hypogene and/or supergene sulfides are being oxidized under the present groundwater conditions and mineral saturation calculations suggest that secondary copper minerals (antlerite, atacamite, malachite) may also be actively forming, suggesting that supergene and exotic copper mineralization is possible even under the present hyperarid climate of the Atacama Desert.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号