Sentence examples for sediment strata from inspiring English sources

Intermediate-type drumlins are those that demonstrate a coupling between underlying Palaeozoic sediment strata in areas of shallow drift sheet.

It has been shown, beyond any doubt, that infaunal irrigation increases the availability of oxygen as an electron acceptor in deep sediment strata.

Even concepts more complex than standard studies, such as pedocomplex and welded soils, are considered inside the theoretical basis that assumes that a soil (paleosol) is a unique, homogeneous, isolated sheet located on (or between) clearly different sediment strata or other geological bodies, which is in many cases a simplification.

In the Po Plain, lying on four regions of Northern Italy (Piedmont, Lombardy, Emilia-Romagna and Veneto), an impressive set of flood events occurred that resulted in evident, sometimes thick sediment strata, in between the Roman archaeological layers, and after their full deposition.

Evidence for episodic enhancements in the flux level comes from geochemical analysis of cosmic tracers in ancient sediment strata and modeling the temporal variation of the zodiacal dust cloud.

An excavation ∼7 m deep reveals a soil-sediment stratum which formed over the course of ∼115 ka in an accumulative beam-like terrace and consists of five lithological layers and six pedostratigraphical units.

These sediment-restricted faults may have a basal sliding plane between the basement-chert, chert-clay boundaries, and/or within the upper unit, deforming the sediment along strata.

We contend, therefore, that competition between the species used in this study is reduced, at least in part, because of inter-specific differences in feeding and digestion rates [37], although we cannot discount the importance of the occupation of different sediment depth strata as a further mechanism of reducing inter-specific competition for space and resources [23].

The lower facies association, interpreted as a frontal lobe complex, consists of tabular, thick-bedded coarse sandstones interbedded with persistent heterolithic packages of thin-bedded sandstones and mudstones, and minor soft-sediment deformed strata.

Syn-tectonic sediments (growth strata) in compressional structures are three-dimensional (3D) features whose geometry reflects both the style of deformation and the distribution of accommodation space in the system.

Measurements of the EP distribution in the sediments showed that electric fields were present, since the electric potential increased from 1 mm below the sediment to deeper strata (Fig. 4a).