Use of Sandstone Wanes and Weathered Basaltic Crust in Absolute Chronology
Use of Sandstone Wanes and Weathered Basaltic Crust in Absolute Chronology
复制标题
在绝对年代学中使用砂岩衰变和风化玄武岩地壳
作者：
J. Černohouz;I. Šolc
已经发现，砂岩块边缘的钝化可以用来确定其年龄在200年至105年的范围内。玄武岩碎片的腐蚀也遵循一个规律，可以确定它们的年龄在500年到107年之间。
IT has been found1 that the blunting of the edges of blocks of sandstone can be used to determine their age in a range of 200 to 105 years. The corrosion of basaltic fragments also follows a law, and it is possible to determine their age in a range of about 500 to 107 years.