Abstract
The gross enistal structure of the Makassar basin has been interpreted from gravity anomalies in confunction with bore hole information and seismic reflection data, Considerubly attenuated conrinental crust appears to underline the basin which reflect a single episode of continental rifring, that has been active in the area during Eocene. Lower Miocene times. The implication of that interpretation for tectonic model are discussed and the overall evolution of the basin from Middle Jurassic onward proposed.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
