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Titlebook: Gold metallogeny and exploration; R. P. Foster Book 1991 Blackie and Son Ltd 1991 chemistry.database.deposits.distribution.environment.gol

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发表于 2025-3-21 17:41:19 | 显示全部楼层 |阅读模式
书目名称Gold metallogeny and exploration
编辑R. P. Foster
视频video
图书封面Titlebook: Gold metallogeny and exploration;  R. P. Foster Book 1991 Blackie and Son Ltd 1991 chemistry.database.deposits.distribution.environment.gol
描述Within the last decade, the high and continuing demand for gold has prompted a global gold rush on a scale never before seen, not even in the heady days of Ballarat, California and the Yukon. Gold is being sought on every continent and, with very few exceptions, in every country around the world. Such interest and fierce competition has demanded considerable innovation and improvement in exploration techniques paralleled by a rapid expansion of the geological database and consequent genetic modelling for the many different types of gold deposits now recognized. This proliferation of data has swamped the literature and left explorationist and academic alike unable to sift more than a small proportion of the accumulating information. This new book represents an attempt to address this major problem by providing succinct syntheses ofall major aspects ofgold metallogeny and exploration, ranging from the chemical distribution of gold in the Earth‘s crust, and the hydrothermal chemistry of gold, to Archaean and Phanerozoic lode deposits, epithermal environments, chemical sediments, and placer deposits, and culminates in chapters devoted to geochemical and geophysical exploration, and the
出版日期Book 1991
关键词chemistry; database; deposits; distribution; environment; gold; information; innovation; inorganic chemistry
版次1
doihttps://doi.org/10.1007/978-1-4613-0497-5
isbn_ebook978-1-4613-0497-5
copyrightBlackie and Son Ltd 1991
The information of publication is updating

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https://doi.org/10.1007/978-3-319-04984-7e Earth’s crust. Deposition of elemental gold and gold–containing minerals occurs in response to changes in the chemical and physical environment through which the hydrothermal ore fluid is migrating. For example, a buoyantly ascending hydrothermal fluid may encounter a permeable zone which induces
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https://doi.org/10.1007/978-94-011-2860-5’s crust. The choice of such a broad definition reflects (a) the wide use of the term ‘epithermal’ in contemporary mineral exploration and (b) the recognition that active geothermal systems in volcanic terranes are the present day . of the epithermal systems responsible for ore formation in the geol
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https://doi.org/10.1007/978-1-4684-2250-4osits (Figure 6.1). Here the spectrum is subdivided into: (a) intrusion-hosted stock-work/disseminated deposits of both porphyry and non-porphyry types, the former possessing all the essential geological attributes (especially multidirectional stock-works) of typical porphyry copper and/or molybdenu
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