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A Turbidite Limestone-Shale Rhythmite of Sirban Limestone of Raisi, Northwest India
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The couplet thickness of Raisi limestone-shale rhythmite is trend-free and non-oscillatory. The couplet thickness are log-normally distributed. These characters suggest, Raisi rhythmite is of episodic as against diagenetic and seasonally-controlled origin of the rhythmites. Among the options available for episodic origin (inundites. tempestites, turbidites) evidences suggest a turbidite origin for Raisi rhythmite.
Keywords
Sirban Limestone, Rhythmite, Sedimentology, Turbidite, NW India.
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