Long-term evolution of Fe oxyhydroxide mineralogy and potentially toxic element partitioning in mining-impacted sediments of the Lower Doce River fluvial-estuarine system. [PDF]
Environ Geochem HealthCamêlo DL +6 more
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Subsurface microbiology and the pressing societal need to support future exploration. [PDF]
FEMS Microbiol EcolSheik CS +9 more
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Mangrove sediments as carbon sinks: a global analysis of research patterns, trends and future directions. [PDF]
Environ Sci Pollut Res IntCavalcante-Silva M +5 more
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On engineering-geological properties of fine-grained sediments in Finland: Dissertation
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The Journal of the Acoustical Society of America, 2022Marine muds, or “muddy” sediments, represent a broad range of sediments containing a mix of clay and silt size components, often with some smaller amount of sand sized and larger material. Sediments characterized by these broad definitions comprise most of the modern global seafloor, except for areas proximal to terrigenous inputs, such as continental ...
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Improvement of Geological Models Using Sedimentation Data
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Earth-Science Reviews, 1966Summary The more common types of deep-sea sediments are pelagic clays and calcareous or siliceous lutites rich in the remains of planktonic Protozoa and Protophyta. Accumulation of the various biogenous and mineral elements may take place by settling from the water column above; by transport along the bottom by submarine solifluction, slumping and ...
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Constraining flow and sediment transport intermittency in the geological past
Geological Society of America Bulletin, 2022Quantitative investigations of ancient rivers usually provide insights into either instantaneous or mean flow conditions. There is a critical gap between these time scales of investigation, which reflects the intermittency of flow and sediment transport, and closing this gap is crucial to fully explore the dynamics and evolution of ancient fluvial ...
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The Geological Deformation of Sediments
1994Introduction and overview. Mechanical principles of sediment deformation. Glacial deformation. Sedimentary deformational structures. Mass movements. Tectonic deformation - stress paths and strain histories. Fluids in deforming sediments. Melanges - illustrations of the dewatering, deformation, diagenesis interplay.
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