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Titlebook: Gold; History and Genesis Robert W. Boyle Book 1987 Van Nostrand Reinhold 1987 economic geology.geology.mining.reef

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tween those supporting A. G. Werner (1750–1817) in his Neptunist theory of the sedimentary origin of granitic rocks and those who followed J. Hutton (1726–1797) in his Plutonist theory of the igneous (magmatic) origin of granites. During the early part of the nineteenth century the controversy was p
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https://doi.org/10.1057/9780230510203he theory has been revived from time to time. Its most recent rebirth, concerning mainly the origin of massive sulfide deposits and iron-formations (both of which may be auriferous), is due to Oftedahl (1958), followed later by Stanton (1959, 1960), Sangster (1972), Hutchinson (1973), and numerous o
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Prevention and Intervention Approaches,ins began with Agricola in the sixteenth century. Since then secretion theories have undergone considerable modification and embellishment. Two general concepts implicit in secretion theories are extant: lateral secretion (.), which postulates that the ore and gangue constituents were derived direct
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https://doi.org/10.1007/978-0-387-69039-1d production. Some of these deposits also contain economic concentrations of uranium, thorium, and rare earths, and minor amounts of recoverable platinoids. The largest economic gold deposits in quartz-pebble conglomerates are those of the Witwatersrand (Rand) in the Republic of South Africa; during
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Biotechnology Intelligence Unit Witwatersrand and other quartz-pebble conglomerates as fossil placers or modified placers, the placer type of auriferous deposit has provided more than two thirds of the world’s store of gold, about 80 × 10. grams (2.6 × 10. oz).
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