AbstractA combined micropalaeontological and sedimentological investigation of the Early Eocene Naredi Formation (thickness varying between 20m and 60m) reveals a complete third-order cycle and six fourth-order sea level cycles. Within the third-order cycle the foraminiferal abundance and diversity gradually increase upwards and reach their maximum values at about 41m thickness above the base of the formation and subsequently decrease upward and finally give way upward to an unfossiliferous zone at the topmost part. Within a fourth-order cycle foraminiferal abundance and diversity exhibit a similar increasing and decreasing pattern. Bounded between two unconformities the Naredi Formation represents a sequence. A highly fossiliferous Assilin...
Kirthar formation (Middle to Late Eocene) is conformably underlain by Ghazij formation (Early Eocene...
The Cretaceous of NW India is poorly known from sparse outcrops in Rajasthan and Gujarat. Here, we d...
A 105 m early Eocene section exposed in the Gurha mine in the Nagaur-Ganganagar Basin, Rajasthan, In...
A combined micropalaeontological and sedimentological investigation of the Early Eocene Naredi Forma...
AbstractA combined micropalaeontological and sedimentological investigation of the Early Eocene Nare...
Various Eocene hyperthermal events have been recorded from lignite sections of western India in the ...
The sedimentary sequence exposed in the erstwhile Tiruchirapalli district hosts a more or less compl...
The Paleogene sections of Kutch are the reference for the regional chronostratigraphic units of Indi...
Middle Eocene Fulra Limestone and Oligocene Maniyara Fort Formation represent platform carbonate dep...
Fluvial strata of the Lower Cretaceous Ghaggar-Hakra Formation are exposed in fault blocks on the ce...
Type section of Pabdeh Formation (Late Paleocene- Early Oligocene) is located in the Gurpi anticline...
AbstractThe lignite deposits of Kutch, India are stratigraphically referred to the Naredi Formation ...
An integrated study based on field observation, petrography, and scanning electron microscopy (SEM) ...
Stable isotope analyses have been carried out on rocks and fossils of the Palaeogene carbonate-clast...
Analysis of the foraminiferal assemblages of the Chari Formation (Middle-Upper Jurassic transition) ...
Kirthar formation (Middle to Late Eocene) is conformably underlain by Ghazij formation (Early Eocene...
The Cretaceous of NW India is poorly known from sparse outcrops in Rajasthan and Gujarat. Here, we d...
A 105 m early Eocene section exposed in the Gurha mine in the Nagaur-Ganganagar Basin, Rajasthan, In...
A combined micropalaeontological and sedimentological investigation of the Early Eocene Naredi Forma...
AbstractA combined micropalaeontological and sedimentological investigation of the Early Eocene Nare...
Various Eocene hyperthermal events have been recorded from lignite sections of western India in the ...
The sedimentary sequence exposed in the erstwhile Tiruchirapalli district hosts a more or less compl...
The Paleogene sections of Kutch are the reference for the regional chronostratigraphic units of Indi...
Middle Eocene Fulra Limestone and Oligocene Maniyara Fort Formation represent platform carbonate dep...
Fluvial strata of the Lower Cretaceous Ghaggar-Hakra Formation are exposed in fault blocks on the ce...
Type section of Pabdeh Formation (Late Paleocene- Early Oligocene) is located in the Gurpi anticline...
AbstractThe lignite deposits of Kutch, India are stratigraphically referred to the Naredi Formation ...
An integrated study based on field observation, petrography, and scanning electron microscopy (SEM) ...
Stable isotope analyses have been carried out on rocks and fossils of the Palaeogene carbonate-clast...
Analysis of the foraminiferal assemblages of the Chari Formation (Middle-Upper Jurassic transition) ...
Kirthar formation (Middle to Late Eocene) is conformably underlain by Ghazij formation (Early Eocene...
The Cretaceous of NW India is poorly known from sparse outcrops in Rajasthan and Gujarat. Here, we d...
A 105 m early Eocene section exposed in the Gurha mine in the Nagaur-Ganganagar Basin, Rajasthan, In...