According to sedimentological and geochronological data, the section is subdivided into three units which correlate with environmental conditions of the early, middle, and late MIS3 period.
The post-Eemian sequence is subdivided into three units, beginning with a mixture of aeolian and gelifluction deposits, which are also modified by cryostructures.
Each structure was subdivided into three units, each of which was separated by four ropes measuring 1 m in length.
Most of the above package is a progradational deltaic sequence that could be subdivided into three units, corresponding to three phases of delta evolution (Fig. 1).
In Thailand, the Upper Sandstone Formation is subdivided into three units, from bottom to top, these are the Preah Vihear (Phra Wihan), Sao Khua, and Phu Phan Formations.
Close inspection of the lower Eagle Ford (Fig. 6a) shows that it can be subdivided into three units, and some stratigraphic interpretations can be deduced on the basis of the AI values.
The ~300 m thick sediment sequence drilled at C0018 is subdivided into two lithological units (U1a and U1b) that correlate with seismic units SU1a and SU1b, respectively, (Figs. 2 and 3; Strasser et al. 2012).
Note three-fourth-order bounding surfaces outlined by A to C, two-third-order bounding surfaces recognized within the 1-IVF unit, three identified channel-fills, and 1-IVF subdivided into three sedimentary units.
The Río Pedregoso Formation can be subdivided into three formal units, namely the Quilmahue Member, Rucañanco Member, and Bío-Bío Member.
The flood plain sediments in Sohag Governorate, Upper Egypt can be subdivided into three distinctive units: inorganic clays (CL), well-graded sand (SW) and channel gravels (GW).
The flood plain sediments in Sohag Governorate, Upper Egypt can be subdivided into three distinctive units: inorganic clays (CL), well-graded sand (SW) and channel gravels (GW). 2.
