摘要
Some profile of a rock section and some isopleth of a fractured surface of the rock were divided each into three parts. Then three parts were measured by dividers method and lattice method. It was discovered that the fractal dimensions of the three parts were remarkably different, so the fractured surface of rock was not simple fractal but multi range fractals.
Ｉｔｉｓｂｅｌｉｅｖｅｄｉｎｆｒａｃｔａｌｇｅｏｍｅｔｒｙｔｈａｔｔｈｅｒｅｉｓｆｒａｃｔａｌｉｎｔｈｅｆｒａｃｔｕｒｅｄｓｕｒｆａｃｅｏｆｒｏｃｋ．Ｔｈｅｓｈａｐｅａｎｄｆｒａｃｔａｌｄｉｍｅｎｓｉｏｎｏｆｆｒａｃｔｕｒｅｓｕｒｆａｃｅｄｅｐｅｎ...
