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Depositional environment of the Fort Member of the Jurasic Jaisalmer Formation, (western Rajasthan,.
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Lithofacies and
granulometric analysis were carried out to decipher the depositional environment of the Fort Member of the Jurassic Jaisalmer Formation. Based on field data nine lithofacies have been identified including
trough cross-bedded sandstones, planar cross-bedded sandstones, matrix supported conglomerates, thinly bedded siltstone and sandstones, herringbone cross-bedded sandstones, wave rippled sandstones, laminated sandstones,
hummocky cross-bedded sandstones, limestones and shales. Granulometric analysis of the sandstones samples has been carried out for their statistical and textural parameters. Bivariant plots of textural parameters such as graphic skewness versus graphic standard deviation and skewness versus standard deviation confirm the high
energy (beach) origin of sandstones. These results suggest a wide spectrum of marine environments ranging from inner shelf to upper shoreface for the Fort Member sandstones.
Edicions de la Universitat de Barcelona
Title: Depositional environment of the Fort Member of the Jurasic Jaisalmer Formation, (western Rajasthan,.
Description:
Lithofacies and
granulometric analysis were carried out to decipher the depositional environment of the Fort Member of the Jurassic Jaisalmer Formation.
Based on field data nine lithofacies have been identified including
trough cross-bedded sandstones, planar cross-bedded sandstones, matrix supported conglomerates, thinly bedded siltstone and sandstones, herringbone cross-bedded sandstones, wave rippled sandstones, laminated sandstones,
hummocky cross-bedded sandstones, limestones and shales.
Granulometric analysis of the sandstones samples has been carried out for their statistical and textural parameters.
Bivariant plots of textural parameters such as graphic skewness versus graphic standard deviation and skewness versus standard deviation confirm the high
energy (beach) origin of sandstones.
These results suggest a wide spectrum of marine environments ranging from inner shelf to upper shoreface for the Fort Member sandstones.
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