Ophiolit, Molasse. Die pre-neogenen Gesteine im O-Arm werden dominiert von ultrabasischen und basischen Gesteinen; untergeordnet Gabros, gefaltenen Doleriten und Kissen-Basalten im O Teil.
Südost-Sulawesi, Sulawesi, ID
Useful for image descriptions and collection inscriptions
Important: Before entering this or any other place of discovery you should have a permission of the operator and/or owner. Likewise it is to be respected that necessary safety precautions are kept during the visit.
Sarasin, F. u. P. Sarasin (1901). Materialien zur Naturgeschichte der Insel Celebes, Vol.1, G.W. Kreidel’s Verlag, Wiesbaden, Germany.
Koolhoven, W.C.B. (1930). Verslag over een verkenningstocht in den oostarm van Celebes en den Banggai archipel. Jaarb. Mijnwez. Ned. Oost Indië, 59 S.127-52.
Kündig, E. (1956). Geology and ophiolite problems of East Celebes. Verh. K. Ned. Geol. en Mijnbouwkd. Genoot. Geologisch, 210–35.
Silver, E.A., R. McCaffrey, Y. Joyodiwiryo, S. Stevens (1983). Ophiolite emplacement by collision between the Sula Platform and the Sulawesi Island Arc Indonesia. J. Geophys. Res. Solid Earth, 88 (B11)S.9419-35.
Simandjuntak, T.O. (1986). Sedimentology and Tectonics of the Collision Complex in the East Arm of Sulawesi, Indonesia. Univ. London S.374. PhD thesis.
Nugraha, M.S., R. Hall u. M. Boudager-Fadel (2022). The Celebes Molasse: A revised Neogene stratigraphy for Sulawesi, Indonesia. J. Asian Earth Sciences. Vol.228, 105140.