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本文从火山机构的组成地层,空间形态,岩相特征和岩石特征,论述了满杖子破火山地质特征,分析了火山岩岩石化学,微量元素和稀土 球化学特征。 相似文献
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本文对右玉县小南山汉诺坝组玄武岩进行了地层、岩石学、岩浆喷发及岩石化学、岩石地球化学方面的研究和总结,采用了目前较为前缘的地学理论,从岩石地球化学特征方面入手,结合区域地质特征,探讨了研究区玄武岩成因及构造背景。 相似文献
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本文通过大量实际资料,对兴隆平泉地区花岗岩类岩石化学、部分金属元素、微量元素及稀土元素分布等进行分析,主要论述了该区与成矿有关的两类岩石即花岗岩-花岗斑岩类及花岗闪长岩类岩石的地球化学特征,指出两类岩石在地球化学特征上的差异不仅与岩性有关,而且主要与成矿物质来源有关。 相似文献
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本文详细论述了东乡－余江斜长角闪岩的地持同特征，岩石特征，岩石化学地球化学特征及同位素年代学研究，并就其形成构造环境作了初步探讨。 相似文献
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本文对中华麦饭石的岩石学、岩石化学、微量元素地球化学、REE地球化学、岩石物理化学特征以及形成条件和成因机制等进行了较全面的地学研究,为今后麦饭石的开发、应用提供了重要的信息资料。 相似文献
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《Geoforum》2015
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
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Sulfide minerals in the Boulder batholith occur 1. as disseminated grains, visible in hand specimens; 2. in aplitic-pegmatitic pods and masses; 3. along joint and shear surfaces; 4. in hydrothermal veins; and 5. as minute masses within pyrite and silicate minerals and along intergranular sites. Hydrothermally altered rocks have an average sulfide content of 0.8 weight per cent, compared to an average of 0.01 per cent for unaltered rocks. Unaltered rock of the batholith may contain as much as 0.7 weight per cent sulfide. Sulfide inclusions in pyrite, the most abundant sulfide of the batholith, are common and represent a captured iss-phase which later changed to chalcopyrite plus pyrrhotite or mackinawite. Inclusions are most abundant, and more complex, in pyrites of hydrothermally altered and ore rocks. Electron-probe analyses show that pyrites of the Boulder batholith have very similar compositions to those found for pyrites from other ore deposits around the world. 相似文献
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Arsenic concentrations of less than 5 ppb to as large as 1,260 ppb in stream waters and from 5 ppm to 4,000 ppm in stream
sediments were found in the Pedro Dome-Cleary Summit area, Alaska. Waters from three of 20 wells sampled had arsenic concentrations
exceeding the U.S. Public Health Service recommended limit of 50 ppb. The high arsenic levels are a consequence of arsenic
enrichment in the rocks of the area. Placer and lode-gold mining may increase the arsenic content of the waters by exposing
arsenic-containing rocks to surface waters and by increasing the load of arsenic-rich sediments in the streams. Finding these
disturbingly large concentrations of arsenic in the waters of the Fairbanks area was the major result of this work, inasmuch
as a subsequent study (to be published) revealed arsenic concentrations as large as 10 ppm in domestic wells and prompted
an extensive study by Federal and State agencies of the health hazard posed by these arsenic-rich waters. 相似文献
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Polished and thin section examinations of samples from Indiana Coal Bed V (Springfield) have shown three sulfides to be present; namely pyrite, marcasite and sphalerite. Pyrite and marcasite are dominant forms whereas sphalerite is very minor. These sulfides appear to have formed in four distinct stages as judged on the basis of mineralogy and mineral texture. Pyrite occurs as framboids throughout the coal seam, as fibrous crystals in two horizons of the coal and in massive form as cleat fillings and cell fillings in fusinite and semi-fusinite. Marcasite occurs in spherical polycrystalline and twinned grains, as polycrystalline overgrowths on framboids, as cementing material for clusters of framboids, as blocky polycrystalline grains and with pyrite as cell fillings in fusinite and semi-fusinite. Sphalerite occurs exclusively as cell fillings in semi-fusinite. The paragenetic sequence indicates fluctuations in the overall coal bed chemistry. Individual sections display evidence of chemical variation on the micro scale. 相似文献
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M. Ahmed 《International Journal of Coal Geology》1996,30(4):319-325
There are five workable coal beds in the Tikak Parbat Formation of the Barail Group in the Makum coalfield, Tinsukia District, Assam. Two of these beds, 18 and 6 m thick, are persistent across the field. The coal is high volatile bituminous B/C, has excellent coking properties, and is of great importance as a blending coal to improve the coking properties of the lower-quality Gondwanan coals.These coals are bimacerites as vitrinertite or trimacerites as duroclarite. Virtrinite predominates with minor amounts of other macerals and minerals. The high percentage of vitrinite indicates that the bark and woody tissues were the dominant contributors to the precursor peat. These peats were strongly decomposed under anaerobic conditions as indicated by the abundance of the collinite type of vitrinite. 相似文献
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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
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A solution of dilute hydrochloric acid, ascorbic acid, and potassium iodide has been found to dissolve weakly bound metals in soils, stream sediments, and oxidized rocks. Silver, Bi, Cd, Cu, Mo, Pb, Sb, and Zn are selectively extracted from this solution by a mixture of Aliquat 336 (tricaprylyl methyl ammonium chloride) and MIBK (methyl isobutyl ketone). Because potentially interfering major and minor elements do not extract, the organic separation allows interference-free determinations of Ag and Cd to the 0.05 ppm level, Mo, Cu, and Zn to 0.5 ppm, and Bi, Pb, and Sb to 1 ppm in the sample using flame atomic absorption spectroscopy. The analytical absorbance values of the organic solution used in the proposed method are generally enhanced more than threefold as compared to aqueous solutions, due to more efficient atomization and burning characteristics. The leaching and extraction procedures are extremely rapid; as many as 100 samples may be analyzed per day, yielding 800 determinations, and the technique is adaptable to field use.The proposed method was compared to total digestion methods for geochemical reference samples as well as soils and stream sediments from mineralized and unmineralized areas. The partial leach showed better anomaly contrasts than did total digestions. Because the proposed method is very rapid and is sensitive to pathfinder elements for several types of ore deposits, it should be useful for reconnaissance surveys for concealed deposits. 相似文献
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Trevor D. Ford 《Geology Today》2013,29(6):229-237
The area around Castleton in the English county of Derbyshire has extensive outcrops of Carboniferous Limestone, showing complex sedimentary facies changes as well as interleaved extrusive basaltic volcanic rocks. Overlying these are the lower parts of the Millstone Grit, ranging from marine shales through a variety of deltaic sandstones. The limestones are hosts to hydrothermal mineral deposits, with veins containing galena, fluorspar, baryte and calcite. A unique variety of fluorspar is Blue John, mined for ornamental purposes since the mid‐eighteenth century. Landscape features include a massive landslip, dry valleys, loess, dolines, scree slopes and various karstic landforms. A complex hydrological system encompasses numerous caves, of which four are open to visitors. 相似文献
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生物礁的研究现状与发展趋势 总被引：27，自引：2，他引：25
生物礁是由固着生物所建造的本质上是原地沉积的碳酸盐建造。生物礁内部孔隙和空洞非常发育,从而成为油气和多种矿藏资源的有利富集场所,所以生物礁的研究具有重要的实际意义,而且越来越受到人们的关注。生物礁成分、构造以及形态复杂多样,研究历史非常久远并且充满了争论。在以前的研究中非常依赖于一些非常主观的特点,如抗浪性等来判断是否为生物礁,因此在生物礁100多年的研究中始终都存在着礁与非礁的尖锐争论。这一问题实际上涉及到生物礁的基本概念、定义以及各种术语的含义。这些方面的混乱严重的影响了生物礁的研究与发展。经过最近20年的研究,生物礁的国内外研究取得了很大的进展。对生物礁的判断现在主要根据生物礁客观和固有的特点,如生物礁内部的构造支撑以及构造支撑所决定的内部成分。这在很大程度上扩展了生物礁研究的广度和深度。对最新的研究成果的总结和介绍必将推动我国生物礁研究的发展。本文在参考国内外大量文献的基础上,主要介绍了生物礁研究的历史与最新成果;总结了生物礁概念与定义的最新认识以及建立在构造基础上的分类方案;对生物礁生长的过程与影响因素以及与环境的关系进行了论述;介绍了造礁生物在地质历史时期中的发展与演化,以及生物礁地化研究的成果与意义。 相似文献