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出 处:《地质科学》1997年第1期56-64,共9页Chinese Journal of Geology(Scientia Geologica Sinica)
基 金:国家自然科学基金
摘 要:多硅白云母b_0值作为相对地质压力计的理论和方法,已受到各国地质学家的普遍重视。本文以澜沧群多硅白云母作为研究对象,提出运用多硅白云母b_0值区分不同压力变质的方法。研究结果表明澜沧群经历了中压和高压变质作用,两期变质的多硅白云母b_0值分别为9.027A和9.047A。The theory and method of b_0 values of phengites regarded as a relative geobarometer have been valued by geologists of the world. There is no research on polymetamorphism reflected by b_0 values of phengites reported in the world today. We think that the populations of b_0 values must be distinguished in the study of b_0 values of phengites of low grade metamorphic rocks occurred in ancient orogenic belts, especially, for the polycyclic orogenesis in China. In this paper, the authors put forward a method of distinguishing polymetamorphism by statistical analyses of b_0 values of phengites on the basis of research on phengites of Lancang Group. Statistical analyses of 486 b_0 values of phengites show that there are medium-and high-pressure metamorphisms in Lancang Group. The intersection of two straight lines representing bi-nomal distributions is situated at the point corresponding to b_0=9.040A in probability graph. The mean b_0 value of high-pressure is 9.047, the standard deviation and cumulative probability are 0.005 and 55% respectively. The average b_0 value of medium-pressure metamorphism is 9.027A, its standard deviation is 0.010. The cumulative frequency curve of medium-pressure metamorphism is situated between cumulative frequency curves of Ryoke and Easterm Alps. The cumulative frequency curve of high-pressure is similar to that of Sanbagawa.
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