Jökull


Jökull - 01.12.2006, Side 56

Jökull - 01.12.2006, Side 56
Kristjánsson et al. REFERENCES Björnsson, B. J. 1975. Villinganesvirkjun. Jarðfræðiyfir- lit. Orkustofnun, Reykjavík, Report OS-ROD-7501, 13 pp. and drawings. Harðarson, B. A. and Á. Guðmundsson 1986. Stafnsvat- navirkjun. Mannvirkjajarðfræði. Orkustofnun, Reyk- javík, Report OS-86039/VOD-14B, 63 pp. and maps. Hardarson, B. S., J. G. Fitton, R. H. Ellam and M. S. Pringle 1997. Rift relocation – a geochemical and geochronological investigation of a paleo-rift in north- west Iceland. Earth Planet. Sci. Lett. 153, 181–196. Harðarson, B. S., M. S. Pringle, L. Kristjánsson and Á. Guðmundsson 1999. Stratigraphy and paleomag- netism of a 2.8 km lava succession in central north- ern Iceland. XXII General Assembly of the I.U.G.G., Birmingham. Abstracts volume B, 326. Hjartarson, Á. 2003. The Skagafjörður Unconformity North Iceland and its Geological History. Ph.D. The- sis, Geological Museum, University of Copenhagen, 248 pp. and map. Hjartarson, Á. 2005. The Late Miocene Tinná Central Vol- cano, North Iceland. Jökull 55, 33–48. Hjartarson, Á., G. Ó. Friðleifsson and Þ. H. Hafstað 1997. Berggrunnur í Skagafjarðardölum og jarðgangaleiðir. Orkustofnun, Reykjavík, Report OS-97020, 55 pp. and maps. Hjartarson, Á., G. Ó. Friðleifsson and Þ. H. Hafstað 2003a. Skagafjarðardalir. Berggrunnskort (Bedrock map), 1:50,000. Orkustofnun, Reykjavik. Hjartarson, Á., B. S. Hardarson and M. S. Pringle 2003b. 40Ar/39Ar-dates from the Skagafjörður Valleys, N- Iceland. – Implications for rift relocations and the deep sea sedimentary record. In: Á. Hjartarson: The Skaga- fjörður Unconformity North Iceland and its Geologi- cal History. Ph.D. Thesis, 81–94. Jóhannesson, H. 1991. Yfirlit um jarðfræði Tröllaskaga (Miðskaga). Árbók Ferðafélags Íslands 1991, 38–56. Kaldal, I. and S. Víkingsson 1978. Jökulsár í Skagafirði I. Jarðfræði. Orkustofnun, Reykjavík, Report OS-ROD- 7805, 28 pp. plus photos and drawings. Kristjánsson, L. 1985. Bergsegulmælingar – nytsöm tækni við jarðfræðikortlagningu. (English summary: Pale- omagnetic polarity measurements in stratigraphy). Náttúrufræðingurinn 54, 119–130. Kristjánsson, L. 2002. Estimating properties of the geo- magnetic field from Icelandic lavas. Phys. Chem. Earth 27, 1205–1213. Kristjánsson, L. and G. Jónsson 2006. Paleomagnetism and magnetic anomalies in Iceland. J. Geodyn. 43 (in press). Kristjánsson, L., Á. Guðmundsson and B. S. Harðarson 2004. Stratigraphy and paleomagnetism of a 2.9-km composite lava section in Eyjafjördur, Northern Ice- land: a reconnaissance study. Internat. J. Earth Sci. 93, 582–595. Ogg, J. and A. Smith 2004. The geomagnetic polarity time scale. In: A Geologic Time Scale 2004 (Gradstein, F., J. Ogg and A. Smith, eds.). Cambridge University Press, Cambridge, 63–86. Saemundsson, K. 1979. Outline of the geology of Iceland. Jökull 29, 7–28. Saemundsson, K., L. Kristjansson, I. McDougall and N. D. Watkins 1980. K-Ar dating, geological and paleo- magnetic study of a 5-km lava succession in northern Iceland. J. Geophys. Res. 85, 3628–3646. Watkins, N. D. and G. P. L. Walker 1977. Magnetostratig- raphy of Eastern Iceland. Am. J. Sci. 277, 513–584. Appendix Profile locations, tectonic tilt corrections, and geolog- ical notes. – Staðsetningar, áætlaður halli jarðlaga og stuttar lýsingar. TD is on the west side of the gully Garðsgil crossing Highway #1 in Norðurárdalur, beginning just below the road. Coordinates: 65◦25’.78N, 19◦04’.26W. The profile was first mapped by Á. G. and J. Helgason in 1976. Tectonic tilt decreases from 8◦ at base to 6◦ at top, downdip 200◦E. As in the other profiles of this project, the lavas sampled are mostly tholeiites with- out appreciable interbasaltic sediments. The stratigra- phy and geological setting indicates that the sequence belongs to the lower part of the Sólheimar formation of Hjartarson (2003). TB: The major part of the profile lies northeast of the gully Geldingsgil on the southeastern slopes of Norðurárdalur. Coordinates: 65◦25’.9N, 19◦02’.1W. Tilt decreases from 7◦ at base to 3◦ at top, downdip 200◦E. The stratigraphy of the profile as mapped by Á. G. and J. Helgason (Saemundsson et al. 1980) has now been slightly revised on the basis of new map- ping by H. H. There are about 10 m of sedimentary rocks overlying flow 62. After flow 68 the profile moves 200 m to the east where it continues up to the 54 JÖKULL No. 56
Side 1
Side 2
Side 3
Side 4
Side 5
Side 6
Side 7
Side 8
Side 9
Side 10
Side 11
Side 12
Side 13
Side 14
Side 15
Side 16
Side 17
Side 18
Side 19
Side 20
Side 21
Side 22
Side 23
Side 24
Side 25
Side 26
Side 27
Side 28
Side 29
Side 30
Side 31
Side 32
Side 33
Side 34
Side 35
Side 36
Side 37
Side 38
Side 39
Side 40
Side 41
Side 42
Side 43
Side 44
Side 45
Side 46
Side 47
Side 48
Side 49
Side 50
Side 51
Side 52
Side 53
Side 54
Side 55
Side 56
Side 57
Side 58
Side 59
Side 60
Side 61
Side 62
Side 63
Side 64
Side 65
Side 66
Side 67
Side 68
Side 69
Side 70
Side 71
Side 72
Side 73
Side 74
Side 75
Side 76
Side 77
Side 78
Side 79
Side 80
Side 81
Side 82
Side 83
Side 84
Side 85
Side 86
Side 87
Side 88
Side 89
Side 90
Side 91
Side 92
Side 93
Side 94
Side 95
Side 96
Side 97
Side 98
Side 99
Side 100
Side 101
Side 102
Side 103
Side 104
Side 105
Side 106
Side 107
Side 108

x

Jökull

Direkte link

Hvis du vil linke til denne avis/magasin, skal du bruge disse links:

Link til denne avis/magasin: Jökull
https://timarit.is/publication/1155

Link til dette eksemplar:

Link til denne side:

Link til denne artikel:

Venligst ikke link direkte til billeder eller PDfs på Timarit.is, da sådanne webadresser kan ændres uden advarsel. Brug venligst de angivne webadresser for at linke til sitet.