16 research outputs found
Post-rift uplift of the Dhofar margin (Gulf of Aden)
International audienceAn investigation of the sedimentation pattern along the Dhofar margin allows us to describe its late-stage evolution. After the accumulation of a thick post-rift sedimentary succession, two debris flow events occurred at the foot of the slope. The first event, affecting a wide area of the margin, marks a major change in sedimentation. The second event is associated with a shift of sedimentary deposition from the slope toward the basin. This latter debris flow was caused by an uplift phase, and highlights two distinct deformational styles in the eastern and western part of the Dhofar margin. Both events occurred very late in the history of the margin, at least 7.6 Ma after the end of the rifting phase (35-17.6 Ma)
Conversion of forest to arable land in Southern Brazil has led to an increase in dissolved silicon flux
status: publishe
The impact of land use changes on water pathways, soil formation and soil functioning
status: publishe
Mapping patterns of soil properties and soil moisture using electromagnetic induction to investigate the impact of land use changes on soil processes
status: publishe
Has Land Use/Cover Change affected the soil weathering degree in Southern Brazil?
status: publishe
Ge/Si ratios record the impact of forest conversion to cropland on soil chemical weathering processes and solutes export to rivers
Topographic control on soil depth and chemical weathering in subtropical Brazil
status: publishe