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From the Norwegian name for the plant Sundew (DrГіsera spp.). Larssen et al. (2002) 18 Upper Palaeozoic lithostratigraphy of the southern Norwegian Barents Sea
The type section is defined as the interval from 2503.0 m to 2350.5 m in well 7128/4-1 on the Finnmark Platform (Fig. 8; Table 1), approximating to the base of the “Viséan sandstone unit” of Ehrenberg et al. (1998a). One core, 27.47 m long, was taken from the upper part of the formation (Fig. 11) in this well. The transition from the underlying basement metasediments into the basal beds of the Soldogg Formation is defined by lower GR readings.
Reference sections:
Reference sections are defined as the interval from 2533.5 m to 2358 m in well 7128/6-1 and from 515.5 m to 501.8 m in IKU shallow core 7029/03-U-01 (Fig. 9 & Fig.12; Table 1). Both reference sections are located on the Finnmark Platform. It appears that Ehrenberg et al. (1998a, fig.4) placed the base of their “Viséan sandstone unit” in 7128/6-1 at the transition from basement wash conglomeratic sandstones to cleaner interbedded sandstones, siltstones and interbedded fines at 2488.5 m. In 7128/6-1 and 7029/03-U-1, the transition from basement to the basal Soldogg Formation conglomerates is represented by a marked erosional unconformity.
The formation is 152.5 m thick in the type well, 175.5 m in well 7128/6-1 and approximately the lowermost 13 m are represented by shallow core 7029/03-U-01 (Fig. 12).
Fig. 12. Reference section of the Soldogg Formation and type section of the Blærerot Formation in core 7029/03-U-01. For explanation of symbols see Fig. 3
Sandstones and conglomeratic sandstones with thin beds and laminae of carbonaceous siltstones, shales and coal dominate the formation. The cored interval in well 7128/4-1 (core 4) consists of cross-bedded and laminated sandstones and siltstones with three coal beds, each less than 1 m thick (Fig. 8 & Fig. 13). Coal beds occur most abundantly in the upper part of the formation in this well, but are not as abundant as in the overlying Tettegras Formation. Petrographic examination of sidewall cores and cuttings from well 7128/6-1 shows a dominance of medium- to coarse-grained quartzose sandstones similar to those observed in well 7128/4-1. Shallow core 7029/03-U-01 is dominated by fining-upward units of conglomerates and laminated and trough cross-bedded sandstones (Fig. 14 & Fig. 15). Siltstones are rare in this core.
The Soldogg Formation is only known from the type- and reference wells in the eastern Finnmark Platform. Seismic mapping around the well locations indicates a thickness range of 100-200 m, reflecting deposition prior to or in the early stages of main rifting (c.f. Steel & Worsley 1984; Ehrenberg et al. 1998a). The Soldogg Formation becomes difficult to identify seismically eastward and westward on the Finnmark Platform and northward toward the margins of the Nordkapp Basin. It thins, possibly due to erosional truncation south and southeast of the type well. In 7029/03-U-01 it is capped by an almost 1 m thick calcrete horizon, implying prolonged subaerial exposure and non-deposition in this area during deposition of the Tettegras Formation.
Based on palynological data, the basal Soldogg Formation is no older than the middle VisГ©an TC Miospore Zone in well 7128/4-1 (Geochem Group 1994). The rest of the formation in this well is assigned to the NM Miospore Zone in terms of the NW European Miospore zonation of Clayton et al. (1977). Simon-Robertson (1992) assigned the interval assigned herein to the Soldogg Formation in well 7128/6-1 to the upper part of the TC and the NM Miospore zones and a similar age range is given for the formation in 7029/03-U-01 (Bugge et al. 1995).
The sandstones encountered in well 7029/03-U-01 are interpreted as braided river deposits (Bugge et al. 1995). The sediments in core 4 from well 7128/4-1 are interpreted as representing various environments within a floodplain-dominated environment, including bar units, channel floor and crevasse splay deposits. They formed four general finingupward rhythms of which two are characterised by the formation of coal beds at the top. According to log data, the cored sections are very similar to the uncored intervals and Ehrenberg et al. (1998a) suggested that the entire interval was deposited in an alluvial fan to braided river system, fining up into floodplain-dominated environments.
As described above, a general correlation to the Billefjorden Group on Spitsbergen can be made, although no more detailed correlation at the formation level is appropriate.
