Preservation of Marine Chemical Signatures in Upper Devonian Carbonates of Kinta Valley, Peninsular Malaysia: Implications for Chemostratigraphy

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. Petrographi...

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Main Authors: Gebretsadik, H., Sum, C., Hunter, Aaron
Format: Book Chapter
Published: Springer Singapore 2015
Online Access:http://hdl.handle.net/20.500.11937/22926
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author Gebretsadik, H.
Sum, C.
Hunter, Aaron
author_facet Gebretsadik, H.
Sum, C.
Hunter, Aaron
author_sort Gebretsadik, H.
building Curtin Institutional Repository
collection Online Access
description 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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publishDate 2015
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spelling curtin-20.500.11937-229262017-09-13T13:57:42Z Preservation of Marine Chemical Signatures in Upper Devonian Carbonates of Kinta Valley, Peninsular Malaysia: Implications for Chemostratigraphy Gebretsadik, H. Sum, C. Hunter, Aaron 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. 2015 Book Chapter http://hdl.handle.net/20.500.11937/22926 10.1007/978-981-287-368-2_28 Springer Singapore restricted
spellingShingle Gebretsadik, H.
Sum, C.
Hunter, Aaron
Preservation of Marine Chemical Signatures in Upper Devonian Carbonates of Kinta Valley, Peninsular Malaysia: Implications for Chemostratigraphy
title Preservation of Marine Chemical Signatures in Upper Devonian Carbonates of Kinta Valley, Peninsular Malaysia: Implications for Chemostratigraphy
title_full Preservation of Marine Chemical Signatures in Upper Devonian Carbonates of Kinta Valley, Peninsular Malaysia: Implications for Chemostratigraphy
title_fullStr Preservation of Marine Chemical Signatures in Upper Devonian Carbonates of Kinta Valley, Peninsular Malaysia: Implications for Chemostratigraphy
title_full_unstemmed Preservation of Marine Chemical Signatures in Upper Devonian Carbonates of Kinta Valley, Peninsular Malaysia: Implications for Chemostratigraphy
title_short Preservation of Marine Chemical Signatures in Upper Devonian Carbonates of Kinta Valley, Peninsular Malaysia: Implications for Chemostratigraphy
title_sort preservation of marine chemical signatures in upper devonian carbonates of kinta valley, peninsular malaysia: implications for chemostratigraphy
url http://hdl.handle.net/20.500.11937/22926