Physical and chemical differentiation of West Malaysia limestone formations

Hutchison, Charles S.

doi:10.7186/bgsm01196704

Cited by 6 publications

(1 citation statement)

References 8 publications

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“…If these variations represent the original signature of the Paleo-Tethys, it may contribute to define the depositional environment of the sedimentary and metasedimentary successions in the Kinta Valley. These results are consistent and fairly agreed with the work of Hutchison [58]. During the organic synthesis, magnesium and strontium are incorporated into solid solution of calcite and aragonite, respectively [59].…”

Section: Discussionsupporting

confidence: 90%

Chemostratigraphy of Paleozoic Carbonates in the Western Belt (Peninsular Malaysia): A Case Study on the Kinta Limestone

Tsegab¹,

Sum²

2019

New Insights Into the Stratigraphic Setting of Paleozoic to Miocene Deposits - Case Studies From the Persian Gulf, Peninsular M

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The Peninsular Malaysia is divided into Western, Central, and Eastern tectonostratigraphic belts based on major geological and geophysical phenomena. The Kinta Limestone is a Paleozoic succession located within the Western Belt. Due to structural and tectonothermal complexity, the sedimentological and paleontological works in these carbonates have proven to be problematic unless combined with geochemical approach. Thus, the current study has integrated stratigraphical, sedimentological, and geochemical studies to assess the lithofacies variations and to interpret the depositional environments. An intensive fieldwork has been carried out in order to assess the extent of metamorphism and to locate the less altered sections for further studies. Three boreholes have been drilled on N-S transect of the Kinta Valley recovering a 360 m core. The core description, the mineralogical analysis, and the geochemical analyses including major and trace elements and organic carbon contents have allowed for a significant advancement of the knowledge existing on this basin. The obtained results have indicated that the Kinta Limestone is chiefly composed of carbonate mudstones, siltstones, shales, and minor cherty units. It preserves the main sedimentary features from metamorphism, especially in the northern part of the Kinta Valley. The detrital siliciclastic debris is minimum in the limestones. The overall dominance of fine-grained textures, the lacking of detrital siliciclastic deposits, presence of bedded cherts, and high organic carbon content outlined by geochemistry and the occurrence of uncommon benthic fauna have suggested the deposition in a slope environment with low energy and low oxygen content. The lithological changes from carbonate to siliciclastic deposits have outlined the occurrence of sea level fluctuations in the Paleozoic. The various analyses combined with chemostratigraphy, an independent of type locality and stratotype, enable to interpret the depositional environment of the Kinta Limestone. Thus, it can be useful to correlate to other formations in or similar types of basins in the southeast Asia.

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Section: Discussionsupporting

confidence: 90%