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南迦巴瓦峰地区岩石磁性和古地磁特征
THE FEATURES OF ROCK MAGNETISM AND PALEOMAGNETISM IN THE MT.NAMJAGBARWA REGION
【摘要】 <正> 南峰地区地质工作的研究程度甚低,岩石磁性和古地磁工作更属空白。1983年6—9月,作者在区内野外考察期间,沿途采集了定向标本。对定向标本和部分地质手标本进行测定后,研究了当地变质岩的磁性特征和古地磁特征,进而探讨了变质岩年代及有关地质构造问题。
【Abstract】 The features of rock magnetism in the Mt. Namjagbarwa region are as follows;1.The magnetization of hornblende gneiss is strong; next to hornblende gneiss is migmatized plagioclase-gneissetc.; the biotite-plagioc-lase granite is the weakest,2.The magnetization of gneiss would reduce when they were migma-tizated.Measured results or 12 or:entated samples indicated that:Average position of paleomagnetic pole was 205. 0°E, 55.1°N and the paleolatitude was abont 15°N.According to the Precambrian polar andering curve of India,the age of rock in the Mt. Namjagbarwa region is about 1100m.y.
- 【文献出处】 山地研究 ,Journal of Mountain Research , 编辑部邮箱 ,1985年04期
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