Preservation of Marine Chemical Signatures in Upper Devonian Carbonates of Kinta Valley, Peninsular Malaysia: Implications for Chemostratigraphy
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The Kinta Limestone is an important Silurian to Permian age unit in the Western Belt of Peninsular Malaysia. Diagenetic alteration and thermal alteration, owing to adjacent igneous intrusion, have obscured many primary sedimentary features and primary geochemistry of the Kinta Limestone. Petrographic and geochemical analyses indicate, however, that some locations of this unit may contain textural and chemical indicators of primary marine properties. In particular, nearly pure limestones lacking dolomite and siliciclastic material, and having relatively low Mn/Sr values (1.83–3.14), suggest minor postdepositional alteration and likely preservation of original marine compositions. Those parts of the Kinta Limestone that are relatively unaltered by these criteria may be useful for assembling a data set with chronostratigraphic significance.
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Tsegab, H.; Hunter, Aaron; Pierson, B.; Sum, C. (2011)Kinta valley was a focus of interest in search of geological resources for the last ten decades. Most of those studies were oriented to reveal the genesis of tin mineralization. Few workers including the current authors ...
Pierson, B.; Kassa, S.; Tsegab, H.; Kadir, A.; Sum, C.; Hunter, Aaron; Harith, Z. (2011)The limestone hills of the Kinta Valley are remnants of extensive limestone beds, which are part of a Paleozoic carbonate complex that covered large parts of South-East Asia and south China. The original limestone beds ...
Structural controls on polyphase hydrothermal dolomitization in the Kinta Valley, Malaysia: Paragenesis and regional tectono-magmatismRamkumar, M.; Siddiqui, N.; Mathew, M.; Sautter, B.; Hui, P.; Ramasamy, Nagarajan; Breitfeld, H.; Santosh, M.; Menier, D.; Poppelreiter, M. (2019)© 2019 In the eastern side of the Malay Peninsula, thick successions of limestone formations preserve important records of the Mesozoic and Cenozoic tectonic events. Here we investigate the strata- and fracture-bound ...