Kabuh Formation | |
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Stratigraphic range: Zanclean–Chibanian ~ | |
Type | Geological formation |
Unit of | Kendeng Group |
Lithology | |
Primary | Sandstone, mudstone |
Location | |
Coordinates | 7°30′S 110°00′E / 7.5°S 110.0°E |
Approximate paleocoordinates | 7°36′S 110°24′E / 7.6°S 110.4°E |
Region | Java |
Country | Indonesia |
The Kabuh Formation is a Plio-Pleistocene geologic formation from Central Java, consisting of several unnamed members belonging to the Kendeng Group.[1] Many of the fossils discovered from Sambungmacan belonging to this group were discovered in an accumulated sediment deposit in a flood-controlling canal near the Solo River, including a series of hominin crania that are similar in anatomy and geologically younger than the Ngandong hominins upstream. This area was excavated throughout the 1970s.[2][3][4][5][6]
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