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The high sedimentation rates and low subsidence rate results in uncompacted, overpressure shales deposited during the transgressive regime resulting in the Akata formation.
Accordingly, a high TPI value suggests a high subsidence rate of basin and dominance of wood derived tissues, and a low TPI suggests a low subsidence rate with high humification.
Such situations prevailed on several occasions during the formation of seams in Tadkeshwar, Rajpardi and Vastan seams of Cambay Basin (Fig. 5) which is a typical of a limno-telmatic swamp having a low subsidence rate and a slow fall in the ground water table.
Similar(57)
Because of low subsidence rates and a warm, wet climate, deposits of the Central subbasin of the Junggar Basin formed from fluvial, deltaic, shallow lake facies.
Such environment prevails in limno-telmatic swamps where low to moderate subsidence rate occurs and there is a slow fall in the ground water table.
This type of environment is prevalent in limno-telmatic swamps where low to moderate subsidence rate occurs and there is a slow fall in the ground-water table.
Valleys, where clastic input was smaller than increment of accommodation space (A/S > 1) due to high subsidence rate or low clastic input, sediments transported by axial drainage were confined to the upper valley parts.
As a result, the cage can provide stability, high fusion rates, and low subsidence.
First, the equations for the subsidence rate extraction at the PTs with low-ADI values are discussed.
The low-frequency stratigraphic sequences are attributed to changes in the long-term regional subsidence rate and regional tilting of foreland basin fill.
High TPI values relate to a high subsidence rate of the basin and dominance of wood-derived tissues, while a low TPI value is seen as a result of a low rate of subsidence and high humification owing to the predominance of herbaceous vegetation in the peat swamp.
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