Following this Oligocene deposition of the Kinabatangan Group occurred, which also consisted of turbidites and marine mudstones indicating transition to a deep marine environment Burton-Johnson A., 2013, Origin, emplacement and tectonic relevance of the Mt.
Following this Oligocene deposition of the Kinabatangan Group occurred, which also consisted of turbidites and marine mudstones. This uplift began to change sedimentary deposits from deep marine turbidites and cherts to shallowing coastal marine sediments during the Miocene and into the Pliocene Burton-Johnson A., 2013, Origin, emplacement and tectonic relevance of the Mt.