The Peshawar basin is situated along the junction of the northern margin of the IndoGangetic foredeep and the southern margin of the Hindu Rush-Himalayan Ranges. During the late Cenozoic, southward encroachment of tectonic disruption into the foredeep terminated molasse deposition and delineated the Peshawar intermontane basin through uplift of the Attock Range along the southern margin of the ...

Sediment deposited within lake basins can preserve detailed records of past environmental conditions on planetary surfaces, including both Earth and Mars. Establishing how to best characterize these paleoclimate records is thus critical for understanding the evolution of past planetary climates. Here, we present an ~40 k.y. lake sediment record from Lake Towuti, Indonesia, developed using visib...

Understanding the impact of aeolian processes on regional-scale dynamics fluvial systems in semi-arid regions is a major issue framework climate change. Although interactions between and have been studied meter to kilometer scale, few studies upscaled regional scale. Using satellite images SRTM-1 digital elevation models we document formation parabolic dunes foredunes along main rivers southern...

In this study, we analyze the fault and fracture network of Middle Triassic carbonate platform Lastoni di Formin (Italian Dolomites, Italy). The reconstruction deformation history is primary importance for a full comprehension present structural setting platform. huge dimensions body superb exposure its vertical cliffs gently dipping top plateau make an ideal outcrop to integrate traditional fi...