Crevasse-splay deposits form a volumetrically significant component of many fluvial
overbank successions (up to 90% in some successions). Yet the relationships between the …

It has been proposed that the Kosi River continuously migrated> 113 km westward across
the surface of the megafan over the last two centuries. Examination of a number of old maps …

Traditional facies models lack quantitative information concerning sedimentological
features: this significantly limits their value as references for comparison and guides to …

An integrated study of sediments was conducted to examine the facies architecture and
depositional environment of the Cretaceous Pab Formation, Rakhi Gorge, and Suleiman …

This paper focuses on the study of the floodplain and low terrace deposits of the Middle
Sebou Valley, which crosses the south-rif corridor and constitutes the eastern limit of the …

Sedimentological, detrital zircon, and biotic analyses of Cambrian deposits from the Salt
Range of Pakistan show that these southwesternmost Himalayan strata were depositionally …

The present field and petrographic investigations of the Tortonian to Gelasian Siwalik Group
in the core of the Hazara-Kashmir Syntaxis have been carried out to comprehend the middle …

To investigate the importance of crevasse-splay elements for the connectivity of fluvial
sandbodies, an integrated study has been undertaken that combines data from outcropping …

Sedimentary successions provide direct evidence of climate and tectonics, and these give
clues about the causes of the mass extinction around the Permian–Triassic boundary …

This study focuses on the Late Carboniferous− Early Permian coal-bearing successions in
Shandong Province, North China in order to understand the depositional processes and …