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

melancholy

書目名稱Gold metallogeny and exploration影響因子(影響力)




書目名稱Gold metallogeny and exploration影響因子(影響力)學科排名




書目名稱Gold metallogeny and exploration網(wǎng)絡公開度




書目名稱Gold metallogeny and exploration網(wǎng)絡公開度學科排名




書目名稱Gold metallogeny and exploration被引頻次




書目名稱Gold metallogeny and exploration被引頻次學科排名




書目名稱Gold metallogeny and exploration年度引用




書目名稱Gold metallogeny and exploration年度引用學科排名




書目名稱Gold metallogeny and exploration讀者反饋




書目名稱Gold metallogeny and exploration讀者反饋學科排名

Adulterate

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

Directed

枕墊

一回合

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

B-cell

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

B-cell

疲憊的老馬

receptors

無王時期,