Sifat Fisik Fragmen Endapan Olistostrome Di Karangsambung

Karangsambung and Totogan formation are an olistostrome sediment, the differences of these based of rock fragment contains. Twelve routes at north and south of geological Karangsambung camp have cerefully examined to knows type and variant of fragment, shape, dimension, sortation, fabric and matrix.

Based of data analysis at buttom, middle and top of section there isn’t special fragment characteristics between Karangsambung and Totogan formation. Both olistostrome sediment formation have similarity fragment, so to be doubtful separeted it as two difference stratigraphic unit. This paper will discuss research background, field observating result (with route map), discussion, interpretasion and conclusion. </p> <p>IAGI Yogyakarta 2002 </p>