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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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書目名稱Water-Rock Interaction
編輯Ingrid Stober,Kurt Bucher
視頻videohttp://file.papertrans.cn/1022/1021162/1021162.mp4
叢書名稱Water Science and Technology Library
圖書封面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

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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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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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