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. 2019 Dec 5;10:5547. doi: 10.1038/s41467-019-12957-1

Table 2.

Sill intrusion density observations.

Basin location ID Survey name Distance (km) Area (km2) Nobs Ncorr Area density, ρ
(10–3 sills km–2)
Rockall 1 NEROCK 280 ± 50 493 36 73
Faroe-Shetland 2 Judd 200 ± 80 1330 62 47
Møre (47) 3 Edvarda 630 ± 20 1440 27 30
Rockall 4 INROCK 800 ± 100 8077 98 290–340 39 ± 3
Vøring & Møre (17) 5 Various 750 ± 250 80,000 735 2205–3675 37 ± 9
Rockall 6 DGER96 850 ± 150 38,500 191 545–610 15 ± 1
Rockall 7 DGWH96 650 ± 150 19,090 85 190–230 11 ± 1
Rockall 8 OGA 475 ± 325 145,000 920 2786–2970 20 ± 1
Rockall 9 ISROCK 1100 ± 200 41,167 46 108–139 3 ± 0.5
Porcupine 10 Various 1500 ± 300 75,868 112 240–310 4 ± 0.5

All area density data based on our own seismic interpretations except where a reference number is given next to the basin location. ID numbers show location on Fig. 6. Distance is relative to the plume centre in Figs. 6 and 8. Nobs is the number of sills observed on the seismic data. Ncorr is the number of sills after correction for missing sills on 2D surveys (Supplementary Fig. 4); a dash in this column indicates a 3D survey that does not require a missing sills correction