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Titlebook: Water-Rock Interaction; Ingrid Stober,Kurt Bucher Book 2002 Springer Science+Business Media Dordrecht 2002 environment.formation.mineral.m

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發(fā)表于 2025-3-21 18:32:52 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱(chēng)Water-Rock Interaction
編輯Ingrid Stober,Kurt Bucher
視頻videohttp://file.papertrans.cn/1022/1021162/1021162.mp4
叢書(shū)名稱(chēng)Water Science and Technology Library
圖書(shū)封面Titlebook: Water-Rock Interaction; Ingrid Stober,Kurt Bucher Book 2002 Springer Science+Business Media Dordrecht 2002 environment.formation.mineral.m
描述The chemical interaction of water and rock is one of the most fascinating an d multifaceted process in geology. The composition of surface water and groundwater is largely controlled by the reaction of water with rocks and minerals. At elevated temperature, hydrothermal features, hydrothermal 0 re deposits and geothermal fields are associated with chemical effects of water-rock interaction. Surface outcrops of rocks from deeper levels in the crust, including exposures of lower crustal and mantle rocks, often display structures that formed by interaction of the rocks with a supercritical aqueous fluid at very high pT- conditions. Understanding water-rock interaction is also of great importance to applied geology and geochemistry, particularly in areas such as geothermal energy, nuclear waste repositories and applied hydrogeology. The extremely wide-ranging research efforts on the universal water-rock interaction process is reflected in the wide diversity of themes presented at the regular International Symposia on Water-Rock Interaction (WRI). Because of the large and widespread interest in water-rock interaction, the European Union of Geosciences organized a special symposium on "w
出版日期Book 2002
關(guān)鍵詞environment; formation; mineral; mineral deposits; ore deposit; water
版次1
doihttps://doi.org/10.1007/978-94-010-0438-1
isbn_softcover978-94-010-3906-2
isbn_ebook978-94-010-0438-1Series ISSN 0921-092X Series E-ISSN 1872-4663
issn_series 0921-092X
copyrightSpringer Science+Business Media Dordrecht 2002
The information of publication is updating

書(shū)目名稱(chēng)Water-Rock Interaction影響因子(影響力)




書(shū)目名稱(chēng)Water-Rock Interaction影響因子(影響力)學(xué)科排名




書(shū)目名稱(chēng)Water-Rock Interaction網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱(chēng)Water-Rock Interaction網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱(chēng)Water-Rock Interaction被引頻次




書(shū)目名稱(chēng)Water-Rock Interaction被引頻次學(xué)科排名




書(shū)目名稱(chēng)Water-Rock Interaction年度引用




書(shū)目名稱(chēng)Water-Rock Interaction年度引用學(xué)科排名




書(shū)目名稱(chēng)Water-Rock Interaction讀者反饋




書(shū)目名稱(chēng)Water-Rock Interaction讀者反饋學(xué)科排名




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Groundwater Evolution in an Arid Coastal Region of the Sultanate of Oman based on Geochemical and Isnd temporal variability of hydrological parameters. Alternatively, this study from the Sultanate of Oman utilizes a combination of geochemical and isotopic tracers (O, H, C, Sr) for the identification of aquifer units, recharge areas, groundwater flow paths and residence times in a coastal alluvial
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A combined isotopic tool box for the investigation of water-rock interaction: An overview of Sr, B, s on the origin deep groundwaters from the crystalline basement of the Vienne region in France..For deep groundwaters from the Vienne granitoid, the conclusions drawn from Sr and B isotope compositions converge towards a marine origin modified by water rock interaction (WRI). The B isotope (δ.B) com
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The distribution of rare earth elements and yttrium in water-rock interactions: field observations a°C. Rare earth elements (REE) and Y abundances in aqueous fluids show a variability over 6 orders of magnitudes. For grouping of waters according to their source rocks, the patterns of REY/Ca ratio are much more appropriate than the conventional REY abundance patterns. Waters from mafic igneous rock
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A Case Study of Gas-Water-Rock Interaction in a Volcanic Aquifer: The South-Western Flank of Mt. Etnonsiderable chemical heterogeneity displayed by groundwaters were identified through factor analysis and by the use of mass balance calculations. A general hydrogeochemical model, concerning the interactions between the shallow volcanic aquifer, deep magma-derived fluids and the underlain sedimentar
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