Observations in sedimentary basins affected by deformation show that the fault-induced
depositional accommodation, at various spatial and temporal scales, is closely linked to …

Circulation of water masses, sediment, and biotope between the sub-basins of the
Mediterranean Sea strongly depends on morphological oceanic gateways. These …

Subsidence and uplift patterns and thermal history of sedimentary basins are controlled by
tectonics, mantle dynamics and surface processes, such as erosion, sediment transport and …

Young rifts are shaped by combined tectonic and surface processes and climate, yet few
records exist to evaluate the interplay of these processes over an extended period of early …

Understanding the interactions between surface and deep Earth processes is important for
research in many diverse scientific areas including climate, environment, energy …

The stratigraphic architecture of Early Jurassic strata exposed along a> 10 km long transect
in the Chachil Graben, an exhumed marine rift depocentre in the Neuquén Basin …

The integrated understanding of processes and mechanisms driving the coupled evolution
of orogens and sedimentary basins and the underlying lithosphere-mantle system, requires …

Distinguished from most existing rift basin evolutionary models, the succession of deep-
water deposits in the Guaizihu sag were mainly developed during rift initiation instead of the …

Presented work focuses on the importance of unconformity that separates the Neogene infill
from older Palaeozoic and Mesozoic rocks in the Croatian part of Pannonian Basin …

Morphological sills condition sedimentary, water and fauna exchanges between different
domains. In particular, sills are crucial factors to consider during the Messinian Salinity Crisis …