Figure 12. Columnar sections of the Ugab Subgroup in the Vrede domes. Sections 1–12 are ordered anticlockwise around the domes (see inset map and Fig. 10 for locations), minimizing the separation of adjacent sections. There is a major facies change from coarse-grained alluvial clastics

Figure 7. Columnar sections of the DX B and DX C sections. Star points show the location of a fossil-like structure. Numbers denote sample locations.

FIG. 10 —Columnar sections: ribbon rock and grainstone sequences. Sections A, B, Maryville limestone at localities 21 and 19 respectively ( Fig. 3 ); section C, Nolichucky lower limestone member at locality 17 ( Fig. 3 ); section D, Widener limestone, at locality 8 ( Fig. 3 ); section E

FIG. 1. —Columnar sections at southeast end of Nuka Ridge. Sections originally reported ( Tailleur and Sable, 1963 ) are shown in column I; section A was designated type section for Nuka Formation. Sections measured or reexamined in 1971 are shown in column II; as plotted on Figure 2 , line

FIG. 3. —Columnar sections projected to a NE.-SW. line and schematic sections across axis of Central Colorado trough.

Fig. 3. A) Simplified sedimentary columnar sections of the Crato Member in the Batateira Creek area and PS09, PS11, and AB well cores. The highlighted horizon marks the position of the studied interval. B) Geographic indication of each studied well core and outcrop section.

Fig. 2 Columnar sections along the surveyed routes and interpretation of the sedimentary environment. The rose diagrams of paleocurrents were based on current ripples. The numbers in squares to the left of the columnar sections are equivalent to the outcrop numbers (Online Supplemental File Fig

Fig. 3 Correlation between Kuh-e- Soukhteh and North Gahrou columnar sections showing the different lithological units in the study area.

Fig. 3 Measured columnar sections of the Posse Formation in the study area. c, clay; s, silt; fs, fine sand; ms, medium sand; cs, coarse sand; g, granule.

Fig. 4 Columnar sections of cores 14DH-C04, 14DH-C05, 15DH-C02, and 15DH-C03, and their stratigraphic correlation. Age data are listed in Tables 2 and 3 . Blue-color ages indicate OSL age and black-color ages indicate 14 C-AMS age. The core image shown above the legend represents pre-Holocene

Figure 2. Columnar sections of the complex outcrop Bardo IV, near a road to the Opolnica village, SW Poland, logged in 2017 (see Figs. 1B , 3 , 4A, and 4B ), ordered in the succession according to field logging, i.e., in inverted order in light of biostratigraphic datings. The variation

Figure 2. Columnar sections, biostratigraphic succession of ammonoids, and the biostratigraphic framework of the lowermost part of the Teradani Formation, Kuruma Group, exposed along the Sakai River. The horizon numbers beside the columnar sections correspond to the horizon numbers in Table 1

Figure 3.  Stratigraphic columnar sections and outcrop photos showing the sedimentary and structural features of the synextensional, lower and upper ophiolitic breccias of the Internal Ligurian Units in the Graveglia ( A ) and Bracco ( E ) sections (Northern Apennines). B , Polymictic clasts

Figure 4.  Stratigraphic columnar sections of igneous and sedimentary rock units in different mafic massifs in the Rif Belt. The 20-m scale bar applies to all columns, except where we show specific scale intervals within certain lithological units. See the text for the description of different

Figure 5. Late Tonian(?)−early Cryogenian columnar sections in Toekoms sub-basin (modified after Hoffman et al., 2017 ). Section locations shown on inset map (lower right) and Figure 4 . Unit 1 (blue number) is provisionally pre-Sturtian and units 2−5 belong to Chuos Formation, deposited

Figure 6. Cryogenian columnar sections from the autochthonous panel of Bethanis and Soutput sub-basins ( Hoffman et al., 2021 ). See Figure 4 for section locations. Note thickening of Chuos (Ac), Berg Aukas (Aa), Okonguarri (Ao), Narachaams (An) and lower Ghaub (Tg) formations toward Soutput

Fig. 7.— Columnar sections and bed-by-bed correlation of turbidite beds across localities. Columnar sections are arranged from upstream (left) to downstream (right) regarding paleocurrent direction. Distances between localities are described in the figure. All columnar sections are aligned

Figure 3.  Synthetic stratigraphic-lithological columnar sections of Purang, Dongbo, Daba Qu, Dongsha, East Daba, and Labuzha massifs cropping out along southern belt, southern Tibet. Sample locations are shown in figure 2 . E-MORB = enriched mid-ocean ridge basalt-like; OIB = oceanic island