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Titlebook: Gemstones and Their Origins; Peter C. Keller Book 1990 Springer Science+Business Media New York 1990 Pegmatit.growth.metamorphism.ocean.oc

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书目名称Gemstones and Their Origins
编辑Peter C. Keller
视频video
图书封面Titlebook: Gemstones and Their Origins;  Peter C. Keller Book 1990 Springer Science+Business Media New York 1990 Pegmatit.growth.metamorphism.ocean.oc
描述Each gem deposit-whether of primary origin in the parent rocks; or secondary as alluvial placers in valley floors, river gravels, or the sand of oceanic shelves­ presents an eloquent chronicle of the Earth‘s life story. It reveals to the expert the prodigious processes which formed the present crust of our planet, of which this volume discloses a small but exciting detail. The materials of the Earth‘s crust are the rocks. In this book, the author expounds on how they were formed, why they altered, why they became the cradles of precious gemstones, how they are categorized, and how they are now exploited by man. What initiates the growth of gemstones? How do they crystallize? Why do gemstones of the same species, originating from different sources, vary? What causes the occurrence of varieties? Why do diamonds, unlike other precious stones, occur not near the Earth‘s surface in its crust, but deep down beneath it in the upper mantle? These are only a few of the entrancing subjects discussed in this enlightening volume. The reader learns that the Earth is surprisingly alive and altering constantly-sometimes through slow and equable changes and at times by violent and tremendous catac
出版日期Book 1990
关键词Pegmatit; growth; metamorphism; ocean; oceanic; water; mineral resources
版次1
doihttps://doi.org/10.1007/978-1-4684-6674-4
isbn_softcover978-1-4684-6676-8
isbn_ebook978-1-4684-6674-4
copyrightSpringer Science+Business Media New York 1990
The information of publication is updating

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Gemstones Formed in Pegmatites: Gem Pegmatites of Minas Gerais, Brazilwn as .. More gemstones are found in pegmatites than in any other type of deposit. Pegmatites yield huge quantities of tourmaline, beryl (aquamarine and morganite), chrysoberyl, kunzite, and topaz, as well as a host of much rarer gems and minerals. Important descriptions of pegmatites are found in S
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Gemstones Formed Directly from Molten Rock: The Ruby Deposits of Chanthaburi-Trat, Thailand ways: (1) Gemstones such as moonstone may be an essential constituent of the lava and crystallize as such as the lava cools; (2) in the final stages of cooling; when much of the magma has solidified, minerals such as topaz may crystallize in lithophysal (gas) cavities formed in the cooling lava; an
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Gemstones Formed by Low-Pressure Regional Metamorphism: The Ruby Deposits of Mogok, Burmaintrudes into the cool surrounding rock, the rock is heated and saturated by hydrothermal fluids and commonly undergoes change in the form of replacement of some of its component minerals or recrystallization of the entire rock mass. The type and degree of change are dependent upon the temperature a
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Diamond Pipes: The Diamond Deposits of Argyle, Western Australiacrust to bring mantle material such as diamond to the surface (Fig. 9–1). Experimental work has shown that most synthetic diamonds generally must have very high temperatures (2,000°C) and pressures (70,000 kg/cm.) to form. In nature these conditions exist only at depths of at least 200 km below the
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