Abstract
The marine sedimentary rocks of the Kampar area, estimated to be more than 5,500 ft thick, can be lithologically divided into six units, which have been dated by means of fossils. These units, with their thicknesses and ages, are as follows (starting with the oldest): Kim Loong No.
Cite
CITATION STYLE
APA
Suntharalingam, T. (1967). Upper Palaeozoic stratigraphy of the west of Kampar, Perak. Bulletin of the Geological Society of Malaysia, 1, 1–16. https://doi.org/10.7186/bgsm01196701
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