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The document summarizes preliminary research on gravity-driven sedimentation processes in the lower Kebo Formation in Mojosari, Bayat, Central Java. Structures like slumping and sliding are common in the lower part of the Kebo Formation, indicating local instability of the depositional basin slopes during sedimentation. Various lithology types were found as clasts in the sedimentary rock mass, including quartzite conglomerate and nummulitic limestone, suggesting the Kebo Formation had a non-conformable cont
- Author
- SunDievas Lee
- Language
- EN