THE MAGMATIC TO HYDROTHERMAL TRANSITION AND ITS BEARING ON ORE-FORMING SYSTEMS
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dc.contributor.author | Halter W.E. | |
dc.contributor.author | Webster J.D. | |
dc.date.accessioned | 2022-04-18T05:17:22Z | |
dc.date.available | 2022-04-18T05:17:22Z | |
dc.date.issued | 2004 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=14662758 | |
dc.identifier.citation | Chemical Geology, 2004, 210, 1-4, 1-6 | |
dc.identifier.issn | 0009-2541 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/37280 | |
dc.description.abstract | The exsolution of volatile phases from silicate magmas controls physical and chemical magma properties and influences large-scale geologic phenomena and processes having major societal and economic implications including the release of climate-altering gases to the atmosphere, the explosivity of volcanic eruptions, hydrothermal alteration, and the generation of magmatic–hydrothermal mineralization. These volatile phases exsolve from a wide variety of magmas and cover a very broad spectrum of compositions.The transition from the orthomagmatic to the hydrothermal stages has important bearing on these fundamentally important geologic phenomena, and this report summarizes the published results of a dozen scientific investigations on the magmatic–hydrothermal transition as applied to volcanic eruption and magmatic–hydrothermal mineralization. These studies involve a variety of analytical and experimental methodologies, and many focus on fluid and melt inclusions from mineralized magmatic systems. A primary goal of each study is to better understand the role of magmatic volatiles and the importance of the magmatic–hydrothermal transition on these geologic processes. | |
dc.title | THE MAGMATIC TO HYDROTHERMAL TRANSITION AND ITS BEARING ON ORE-FORMING SYSTEMS | |
dc.type | Статья |
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