HALITE TREND IN HYDROTHERMAL SOLUTIONS.

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作者：
Cloke, Paul L.
Kesler, Stephen E.
机构：
来源：
Economic geology Lancaster, Pa. | 1979年 / 74卷 / 08期
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ORE DEPOSITS - SALT DEPOSITS;
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摘要：
Observations of halite and sylvite disappearance temperatures in fluid inclusions from high-temperature deposits indicate that the trapped solutions have compositions lying on linear trends in the NaCl-KCl-H//2O system. These trends were formed by crystallization of KCl-bearing halite from the hydrothermal solutions before the liquid was trapped in fluid inclusions. It is concluded that solutions at high-temperature end of the halite trend originated by exsolution from a granitic magma.
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页码：1823 / 1831
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