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《Acta Geological Sinica》 1974-01
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ON THE ZONING OF COUNTRY ROCK ALTERATION AND ITS GENESIS OF AN IRON DEPOSIT

CHANG JUNG-HUA  
In this paper are given the characteristics of the vertical and lateral zoning formed by the pneumato-hydrothermal mctasomatic alteration of the country rocks of an iron ore supposed to be deposited during post-volcanic action. According to the mineral assemblages present in a state of equilibrium and their transformation, there are several different kinds of alteration recognized i.e. melano-, leuco-, retrogressive and superposed alterations. The stages of alteration are accordingly defined. Based upon the evolution of the altered mineral assemblages, their chemical compositions and the data of mineral forming temperature as revealed by homogenizing void inclusions in certain minerals and geothermometer, the alteration phases are discussed and preliminarily established. The alteration zoning is believed to be of significance to mineral prospecting.
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