Fróðskaparrit - 01.01.1979, Page 102

Fróðskaparrit - 01.01.1979, Page 102
110 Marine Seismic Investigation Himsworth, E. M. 1973: Marine geophysical studies between northwest Scotland and the Faeroe Plateau. Ph. D. thesis, University of Durham, 125 p. Korsakov, O. D. 1974: Tectonics of the Faeroe-Shetland Trench (in Rus- sian). Doklady Akad. Nauk SSSR, v. 214 (3), 647—650. McQuillin, R. and Ardus, D. A. 1977: Exploring the geology of shelf seas. Graham and Trotman Ltd., London, 234 p. Nielsen, P. H. 1976: Seismic refraction measurements around the Faeroe Islands. Fróðskaparrit, v. 24, 9—45. Nielsen, P. H. 1977: A marine geophysical project: Magnetic measurements. Fróðskaparrit, v. 25, 95—100. Rasmussen, J. 1977: Framløga av botnkorti út á 200 m dýpi. Fróðskapar- rit, v. 25, 194—195. Rasmussen, J. and Noe-Nygaard, A. 1969: Beskrivelse til geologisk kort over Færøerne. Danmarks Geologiske Undersøgelse, 1. rk. (Geological Survey of Denmark, 1. series), no. 24, 370 p. English edition: Geology of the Faeroe Islands. Geol. Survey of Denmark, 1. series, no. 25, 142 p, 1970. Schrøder, N. F. 1971: Magnetic anomalies around the Faeroe Islands. Fróðskaparrit, v. 19, 20—29. Stride, A. H., Belderson, R. H., Curray, J. R. and Moore, D. G. 1967: Geophysical evidence on the origin of the Faeroe Bank Channel — I. Continuous reflection profiles. Deep-Sea Res., v. 14, 1—6. Tarling, D. H. and Gale, N. H. 1968: Isotopic dating and paleomagnetic polarity in the Faeroe Islands. Nature, Lond., v. 218, 1043—1044. Talwani, M. (ed.) 1974: Underway marine geophysical data in the north Atlantic June 1961 — January 1971. Lamont-Doherty Geological Ob- servatory of Columbia University, Palisades, New York. Talwani, M. and Eldholm, O. 1972. Continental margin off Norway: a geophysical study. Bull. geol. Soc. Am., v. 83, 3575—3606. Waagstein, R. 1977: The geology of the Faeroe Plateau. Unpubl. lic. sc. thesis, University of Copenhagen, 195 p. Waagstein, R. and Rasmussen, J. 1975: Glacial erratics from the sea floor south-east of the Faeroe Islands and the limit of glaciation. Fróðskapar- rit, v. 23, 101—119. ÚRTAK Saman við Føroya-Islands-Grønlandsrygginum er føroyski landgrunn- urin partur av Norðuratlantska basaltøkinum. I Føroyum eru basalt- fláirnar samanlagdar meira enn 3000 m. Hildið verður at skorpan undir føroyska basaltháslættanum er meginlandsskorpa.
Page 1
Page 2
Page 3
Page 4
Page 5
Page 6
Page 7
Page 8
Page 9
Page 10
Page 11
Page 12
Page 13
Page 14
Page 15
Page 16
Page 17
Page 18
Page 19
Page 20
Page 21
Page 22
Page 23
Page 24
Page 25
Page 26
Page 27
Page 28
Page 29
Page 30
Page 31
Page 32
Page 33
Page 34
Page 35
Page 36
Page 37
Page 38
Page 39
Page 40
Page 41
Page 42
Page 43
Page 44
Page 45
Page 46
Page 47
Page 48
Page 49
Page 50
Page 51
Page 52
Page 53
Page 54
Page 55
Page 56
Page 57
Page 58
Page 59
Page 60
Page 61
Page 62
Page 63
Page 64
Page 65
Page 66
Page 67
Page 68
Page 69
Page 70
Page 71
Page 72
Page 73
Page 74
Page 75
Page 76
Page 77
Page 78
Page 79
Page 80
Page 81
Page 82
Page 83
Page 84
Page 85
Page 86
Page 87
Page 88
Page 89
Page 90
Page 91
Page 92
Page 93
Page 94
Page 95
Page 96
Page 97
Page 98
Page 99
Page 100
Page 101
Page 102
Page 103
Page 104
Page 105
Page 106
Page 107
Page 108
Page 109
Page 110
Page 111
Page 112
Page 113
Page 114
Page 115
Page 116
Page 117
Page 118
Page 119
Page 120
Page 121
Page 122

x

Fróðskaparrit

Direct Links

If you want to link to this newspaper/magazine, please use these links:

Link to this newspaper/magazine: Fróðskaparrit
https://timarit.is/publication/15

Link to this issue:

Link to this page:

Link to this article:

Please do not link directly to images or PDFs on Timarit.is as such URLs may change without warning. Please use the URLs provided above for linking to the website.