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Isobaths, 50-m contour intervals, of the top of carbonates in the

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Severe 21st-century ocean acidification in Antarctic Marine

JMSE, Free Full-Text

What could form a 35-km lineament of carbonate mounds on the ocean floor? - ScienceDirect

Limited Mediterranean sea-level drop during the Messinian salinity

A. Map of the Southeastern part of the Bay of Biscay showing the

Geological Society Of London Effect of Dam Emplacement and Water Level Changes on Sublacustrine Geomorphology and Recent Sedimentation in Jackson Lake, Grand Teton National Park (Wyoming, United States)

04 OCE1L Bathymetry Part 1 Ans.docx - OCE-1: Bathymetry Lab The Shape of Ocean Basins and the Bathymetry of the Sea Floor Objectives: Compare and

Isobaths, 50-m contour intervals, of the top of carbonates in the

Frontiers Monitoring of Anthropogenic Sediment Plumes in the

Isobaths (IBCAOv3) every 50 m at depths less than 500 m and every 500 m

2 a Residual Bouguer anomaly map of the whole La Réunion edifice

New evidence of the outer Dinaric deformation front in the Grado area (NE-Italy)

SciELO - Brasil - Santos Basin continental shelf morphology, sedimentology, and slope sediment distribution Santos Basin continental shelf morphology, sedimentology, and slope sediment distribution

Isobaths, 50-m contour intervals, of the top of carbonates in the

Lateral shift from turbidite- to contourite-dominated continental