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Readings and discussions provide preparation for the 12.117B field trip to a modern sedimentary environment.
Readings and discussions provide preparation for the 12.487B field trip to a modern sedimentary environment.
The physical features of a sedimentary environment include water depth and the velocity and persistence of currents.
To address these changes, we investigated the relation between sedimentary environment (facies) and texture with various elastic moduli.
Moreover, porosity spectra in clastic strata is favorable for determining lithology and sedimentary environment when combined with microresistivity images.
The sedimentary environment is the specific depositional setting of a particular sedimentary rock and is unique in terms of physical, chemical, and biological characteristics.
Instead, we propose that the primary determinant of aU abundance at sites 17PC and 31BB is the redox state of the sedimentary environment.
The paper furthermore discusses the influences of sedimentary environment and conditions on geotechnical properties of the sedimentary facies.
Changes are recorded for most of the investigated sedimentary settings, both in terms of sedimentary environment distribution and sediment composition.
In a sedimentary environment, layered models with abrupt boundaries between the different soil units represent the soil profile accurately.
The sedimentary environment and the halophytes coverage were sampled bimonthly during a year in nine intertidal habitats characterized by different plant communities.
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