This work studies a submarine volcanogenic apron forming the Nagyhársas Andesite Formation (Badenian – Middle Miocene) in Mátra Mountains (North-Eastern Hungary), with aim to identify volcanic processes, from sedimentary bed scale architecture of whole apron. Fieldwork has been carried out two different localities (Tar and Sámsonháza villages), where eighteen logs have measured correlated, reco...

The coast, as the interface between land and sea, is a highly dynamic area, endangered by erosion flooding, particularly at times of sea-level rise. At present context climate change, use scientific knowledge to understand coastal dynamics evolution assessment through time essential find suitable management response for successful adaptive governance. It proposed that obtained high-resolution l...

Fluvially-dominated, fine-grained, shallow-water deltas are more variable than is generally recognized. Studies of the Mississippi River imply rather persistent river-mouth jet dynamics, resulting in either progressive channel bifurcation around middle-ground mouth bars on lobate deltas, or steady progradation to form elongate akin modern Delta. By contrast, satellite imagery and historical map...

The study of paleo shorelines, particularly those formed during the late Quaternary, provides robust insights into past climate variability. Advances in surveying techniques and chronological methodologies have dramatically improved inter-comparability regional basin-wide shoreline surveys. However, these advances been applied unevenly across globe. This is especially true southwestern Madagasc...

River deltas are maintained by a continuous supply of terrestrial sediments that provide critical land building material to help sustain and protect vulnerable ecological communities serve as natural storm protection barriers. Local hydrodynamics important in determining the degree which fluvial removed from water column retained on delta complex. During 2014, we measured sediment transport cha...

A new interpretation of the Middle Jurassic-Early Cretaceous paleogeographic evolution NW sector Latium-Abruzzi carbonate platform facing Umbria-Marche Basin is proposed, based on Monte Giano area (central Apennines, Italy). During Late Triassic-early Bajocian time, was characterized by shallow water sedimentation. Inner and marginal deposits are overlain pelagic (Posidonia level), early p.p. i...

Continental rifted margins are often associated with widespread, thick evaporite (i.e., salt) deposits and pronounced salt tectonics. The majority of basins formed during the latest stages rifting, prior to continental breakup. We use 2D thermo-mechanical finite element modeling lithospheric extension investigate interplay between margin architecture, late syn-rift deposition, post-rift focus o...

Existing barrier island facies models are largely based on modern observations. This approach highlights the heterogeneous and dynamic nature of systems, but it overlooks processes tied to geologic time scales, such as multi-directional motion, erosion, reworking, their expressions preserved strata. Accordingly, this study uses characteristic outcrop from paralic strata Upper Cretaceous Straigh...

Abstract The seismic stratigraphy and sedimentary facies of the Cretaceous Paleogene successions in north-eastern offshore part Taranaki Basin, New Zealand have been investigated order to unravel their depositional evolution identify potential hydrocarbon plays. Interpretation regional lines covering entire shelf-slope deepwater regions as well integrating allows identification several seismic-...