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Frontiers of Earth Science

ISSN 2095-0195

ISSN 2095-0209(Online)

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Front Earth Sci    2011, Vol. 5 Issue (2) : 138-149    https://doi.org/10.1007/s11707-011-0169-y
RESEARCH ARTICLE
Understanding the transportational and depositional setting of Panchet Formation, Purulia and Bankura districts of West Bengal, India---- Evidence from grain size analysis
Bapi GOSWAMI(), Dipsikha GHOSH
Department of Geology, University of Calcutta, Kolkata 700029, India
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Abstract

The rocks of Triassic Panchet Formation (TPF) of West Bengal, India, predominantly include sandstones of medium to fine grain-size, with subordinate shale and pebble horizons. Textural parameter like mean, standard deviation, skewness and kurtosis are calculated using standard methods to understand the transportation and the depositional environment of the sediments in a part of Panchet Formation. Granulometric analyses indicate the presence of fluvial environment interrupted with aeolian, beach and tidal environments prevailed during the time of deposition of the sediments in this part of Gondwanaland during the Triassic time.

Keywords gondwanaland      panchet      textural parameters      environment      West Bengal     
Corresponding Author(s): GOSWAMI Bapi,Email:bapigoswami69@gmail.com   
Issue Date: 05 June 2011
 Cite this article:   
Bapi GOSWAMI,Dipsikha GHOSH. Understanding the transportational and depositional setting of Panchet Formation, Purulia and Bankura districts of West Bengal, India---- Evidence from grain size analysis[J]. Front Earth Sci, 2011, 5(2): 138-149.
 URL:  
https://academic.hep.com.cn/fesci/EN/10.1007/s11707-011-0169-y
https://academic.hep.com.cn/fesci/EN/Y2011/V5/I2/138
Fig.1  (a) Map of Gondwana basins of India after Bandyopadhyay (), (b) disposition of Raniganj Basin in Damodar valley and (c) geological map of the study area (after ). Please note the location of samples analyzed in the study
AgeGroupFormation
Lower CretaceousLamprophyre and Dolerite Intrusive
JurassicUpperUpper GondwanaNon-deposition
Middle
Lower
TriassicUpper RhaeticSupra-panchet Formation
Middle NoricInfra-Norian erosional surface
LowerPanchet Formation
Carnic
PermianUpperRaniganj Formation
Barren Measures Formation
LowerRaniganj FormationBarakar Formation
Karharbari Formation
Talchir Formation
Tab.1  Stratigraphic succession of Gondwana sediments in Damodar Valley (after Raja Rao, 1987)
Sl. No.Sample No.Sample typeTextural groupMeanSortingSkewnessKurtosis
1DGD-5BUnimodal, Well SortedSand1.810.282-0.0181.313
2DG 5Polymodal, Poorly SortedMuddy Sand3.891.7530.4970.967
3DG6Trimodal, Poorly SortedMuddy Sand4.2591.8360.4510.741
4DG 1Bimodal, Poorly SortedMuddy Sand3.2321.0010.2851.722
5DG9Polymodal, Poorly SortedMuddy Sand3.8771.7850.5260.842
6DG 2Trimodal, Poorly SortedMuddy Sand3.5421.1330.2742.133
7DG8Polymodal, Poorly SortedMuddy Sand3.6211.640.481.362
8DG7Bimodal, Poorly SortedMuddy Sand4.0111.4840.5891.414
9DG10Trimodal, Poorly SortedSand2.9371.0380.1471.128
10DG 4Bimodal, Moderately SortedSand3.0180.7370.2681.685
11DGB-3aBimodal, Well SortedSand2.0490.415-0.1731.294
12DGB-1dUnimodal, Well SortedSand1.8540.329-0.2160.85
13DGB-1cTrimodal, Moderately Well SortedSand1.8020.493-0.3511.113
14DGB-1bBimodal, Moderately Well SortedSand2.0610.5-0.1851.068
15DGT-1aBimodal, Well SortedSand1.4960.4650.1981.032
16DGT-1bBimodal, Moderately Well SortedSand2.3890.5110.0891.141
17DGS1Trimodal, Moderately SortedSand1.5130.5-0.1711.282
18DGP5Trimodal, Poorly SortedSand3.1920.498-0.240.931
19DGP2Bimodal, Well SortedSand2.610.536-0.3980.769
20DGJ1Polymodal, Moderately SortedSlightly Gravelly Sand0.8260.75-0.071.136
Tab.2  Grain size characteristics of Panchet sediments (Method after )
Fig.2  Variation of textural components of the sandstone samples of the Panchet Formation along a hypothetical vertical profile section. (a) Graphic mean; (b) standard deviation; (c) skewness and (d) kurtosis. All parameters are calculated following formulations of Folk and Ward ()
Fig.3  (a) Scatter plot of mean size versus standard deviation (sorting) of sandstones of Panchet Formation (after ). Fields of river, beach and dune environments in the diagram is drawn by Martins () modified after Friedman (). Most of the values indicate fluvial environment of deposition followed by dune and beach environments. (b) Scatter plot of mean size versus skewness of sandstones of Panchet Formation (after ). Note that most of the samples are positively skewed within a mean grain-size of 2-4 Φ. (c) Scatter plot of mean size versus kurtosis of sandstones of Panchet Formations (after ). Note that the samples ranges from leptokurtic – platykurtic, most of the samples are leptokurtic followed by mesokurtic. (d) Scatter plot of skewness versus standard deviation of sandstones of Panchet Formations (after ). The fields of river, dune and beach environments are given by Martins () modified after Friedman (). Note that most of the samples are positively skewed and clustering of grains in one sector indicating dominance of sand mode having subordinate silt. Because of the silt the skewness values deviates into the negative sector. Most of the samples plot in the depositional environment of river, followed by dune and beach environments. (e) Scatter plot of standard deviation versus kurtosis of sandstones of Panchet Formations (after ). Note an increase in size, samples follow a regular progression on this diagram, from silty sands (A) to pure sands (B) to sub equal mixtures of sand and silt (C). (f) Scatter plot of kurtosis versus skewness of sandstones of Panchet Formation (after ). Note that most of the present values dominantly fall within the range of the normal curve (shaded area) with regard to both skewness and kurtosis. Values which fall out of the range of normal curve are due to wide separation between the modes of silty sands and the ineffective sorting of depositional environment
Fig.4  (a) Plots of sandstones of Panchet Formation in CM diagram of Passega (). Note that the sediments of present study mostly fall in fields IV and V which are suspension sediments that may contain rolled grains smaller than 1 mm. These rolled grains may have been transported long distances in suspension before being rolled. (b) Plots of Panchet sandstones in the CM diagram modified by Peiry (). According to this plot sandstones of present study deposited mostly in the emerged bar facies followed by topset fill of a dead arm of a channel and submerged bank facies in a fluvial environment
Sample No.Saltation populationSuspension populationTraction populationEnvironmentSorting
%C.T. phiF.T, phiF.T. phiC.T. phi
Limits given by Visher (1969)65-1.52.75
98-13.5>4.5No limitFluvial
022
3013.5>4.5Natural levee
201.51.5
8023.53.5–4.51.5Tidal inlet
500.53
9924.253.5–4.51Beach
3523
903>4.5>4.5No limitWave zone
9713
99244–>4.51Dune
Panchet Formation
601.252.5Well sorted
DGD-5B992.53.253.250.75Tidal channel
101.53.75Poorly sorted
DG 5653.75451.25Dune
51.753Poorly sorted
DG65033.7551.25Dune
351.52.75Poorly sorted
DG 1652.753.551.25Natural levee
161.752.75Poorly sorted
DG9402.753.551.25Natural levee
101.752.75Poorly sorted
DG 2502.753.7551Natural levee
11.52.5Poorly sorted
DG8702.53.551Natural levee
513Poorly sorted
DG7653450.75Dune
51.252.75Poorly sorted
DG10702.753.2550.75Dune
152.53.25Moderately sorted
DG 4703.254.2551.75Wave zone
51.52Well sorted
DGB-3a35233.50.25Tidal channel
101.52.75Well sorted
DGB-1d952.7533.251Wave zone
50.252Moderately well sorted
DGB-1c9022.7530Beach
522.75Moderately well sorted
DGB-1b752.7533.750.75Natural levee
51.252.25Moderately well sorted
DGT-1a702.2533.250Tidal inlet
101.753Moderately well sorted
DGT-1b9033.253.50.25Tidal inlet
10.253.75Moderately sorted
DGS1843.7543.750Beach
52.252.75Poorly sorted
DGP5452.75451.75Wave zone
51.252.75Well sorted
DGP2842.753.253.251Fluvial
5-0.251.75Moderately sorted
DGJ1751.7533.25-1.25Fluvial
Tab.3  Environment of deposition of Panchet Samples (after )
Fig.5  Cumulative Frequency Curve plotted at Probability scale of sediments of Panchet Formation after Visher ()
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