Sentence examples for deposit unit from inspiring English sources

Customers will probably have to wait a couple of weeks to receive their savings, up to £50,000, a spokesman at the deposit unit said.

A fine-grained pumice fall deposit (unit 1) is overlain by a fine-grained grey ash interpreted as of phreatomagmatic origin (unit 2).

Only the syenite-poor Plinian fall (units 1 to 5) and the overlying pyroclastic density current deposit (unit 6) thicknesses were measured and the findings analysed in this study.

The basic deposit unit, termed collection, is defined to be a hierarchical set of files and folders, reflecting the typical structures used by researchers to store their experimental data.

Cells were sorted by flow cytometry using an automatic cell deposit unit (ACDU) in dry 96-well plates and directly frozen at -80°C overnight.

A FACSARIA II (BD Biosciences) equipped with a 375 nm, 488 nm and 633 nm laser and single cell deposit unit was used for single CTC sorting.

Specifically, the three main deposit units can be classified as follows: The central deposit (OL-A in Fig. 5), originating mainly from the Ophir Labes A scar, traveled southward following a straight path and then impacted with topographic rises F G.

Apart from the ash-rich surface near the breakout fan apex, all deposit units have a variable pumice- or scoria-rich surface with matrix-free lobe margins and are internally matrix supported.

Three stratigraphic units are recognized (from bottom to top): Unit 1 includes an inner estuarine tidal channel complex and tidal flat/salt marsh deposits; Unit 2 consists of estuarine bay/lagoon and flood tidal delta deposits related to the estuary mouth; and Unit 3 includes a tidal channel with a tidal point bar, as well as tidal flat/salt marsh deposits similar to those from Unit 1.

Sand-prone architectural elements identified in this work include: a) axial canyons incising a salt-withdrawal basin (Unit 1), b) turbidite lobes intercalated with heterogeneous mass-transport deposits (Unit 2), and c) channel complexes confined by salt-controlled topography (Unit 3).

The system then moved seaward, with the superposition of inner estuarine deposits (Unit 3) over Unit 2. Facies architecture seems to have been controlled by tectonics, as shown by: the paleovalley orientation according to the main tectonic structures of the basin; the presence of faults and fractures that displace the basal unconformity; and the abundance of soft sediment deformation.