Jökull

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Jökull - 01.12.1992, Qupperneq 41

Jökull - 01.12.1992, Qupperneq 41
TN ---- 85 8.2 m.y. { a few degrees of arc. The directions hence have to be used with some caution. Virtual geomagnetic poles (VGPs) have been calculated for each lava, using the mean site coordinates 65.55° N, 19.9° W. Paleomagnetic polarities for each sampled lava are shown in Figs. 3-5 along with other information. The VGP latitude has been plotted as a function of strati- graphic height in Fig. 7 for a composite section con- sisting of flows TL 1-33, KL 13-17, KM 1-5, KN 1-23 and TN 0-85. Here, overlaps have been ex- cluded: note that all of profile TM overlaps with TN and KN. The agreement between polarities and even tndividual directions in overlapping profile segments ls good, see for example the low-latitude poles at the toP ofKL and TL (Table 1). The composite profile has a total thickness of 1150 m and includes 139 sampled Fig. 8. Composite strati- graphic diagram of profiles TL through TN, showing pa- leomagnetic polarities and mean ages. Reverse polar- ity is white. Arrows indi- cate extent of sampling for laboratory magnetic mea- surements, with two seg- ments (broken arrows) omit- 100 m ted here. Stars indicate K-Ar dated flows. —Segulpólun og meðaltöl aldursgreininga í samsetta sniðinu. flows which have «95 values less than 60°. Note that in Fig. 6 the total thickness appears to be only 1000 m but this is due to a different arrangement of individual proíiles in the composite section. The mean paleomagnetic direction from those 134 lavas in the composite section which have an a95-value of 23.5°or less, has a declination D = 4°, inclination I = 74.2° with a vector sum R of 124.6 which corre- sponds to a circular standard deviation (c.s.d., uncor- rected for within-site scatter) of 21.7°. The mean of the VGPs from the same collection is at a longitude of 112° E, latitude 86.3°N (a95=5°), which is quite close to the geographic pole indicating that the tilt correc- tion which we have used is reasonable. It is slightly "right-handed" as has been found for some other mean poles from Icelandic lavas (Kristjánsson and Jóhann- JÖKULL, No. 42, 1992 39
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