Greinar (Vísindafélag Íslendinga) - 01.01.1977, Qupperneq 70

Greinar (Vísindafélag Íslendinga) - 01.01.1977, Qupperneq 70
68 Nevada trend in Carboniferous, Permian, and Mesozoic mate- rial. For this and further reasons, we have since then con- sidered the magnetization of old sedimentary rocks to be a tectonic phenomenon, not one caused directly by a geomagnetic field, unless the latter interpretation is in certain cases proved to be correct. But it was an overwhelmingly sedimentary material with which the two famous “pole”-curves for Europe and America were constructed, and by so many taken to be a proof of conti- nental drift. We think, it is on the basis of shear planes in global stress fields, not on geomagnetic basis, that these cur- ves should be interpreted. But as to basalts, we have shared uncritically the general opinion for 20 years: that their magnetization is geomagneti- cally significant and trustworthy. Now, we must doubt this view in light of the above facts, which should have been ob- vious all the time. These facts about age and deep burial, we consider to be more fundamental than the criteria used for significance in paleomagnetic work. To give examples, the Coal Measures of Scotland must have been kept at temperatures of 100—150° C under the load of 3—4 km of rocks for times of the order of 100 million years. The enclosed basalt lavas must have been subjected to the same conditions. What do we really know about viscous change of magne- tization under such pressure-temperature conditions for times which are at least a factor of million longer than any intervals possible in a laboratory? And here we mean not least the change due to non-hydrostatic stress. It seems to us that there are no laboratory tests of such a process. Can we then deny to take that process into account, when its effects seem to be clear where geological time intervals were available? On the other hand, there may be field circumstances which show in some cases that basalts have very probably retained their original direction of magnetization after such a burial history, as we shall mention later. Let us consider the Deccan Traps. Their age is Paleocene
Qupperneq 1
Qupperneq 2
Qupperneq 3
Qupperneq 4
Qupperneq 5
Qupperneq 6
Qupperneq 7
Qupperneq 8
Qupperneq 9
Qupperneq 10
Qupperneq 11
Qupperneq 12
Qupperneq 13
Qupperneq 14
Qupperneq 15
Qupperneq 16
Qupperneq 17
Qupperneq 18
Qupperneq 19
Qupperneq 20
Qupperneq 21
Qupperneq 22
Qupperneq 23
Qupperneq 24
Qupperneq 25
Qupperneq 26
Qupperneq 27
Qupperneq 28
Qupperneq 29
Qupperneq 30
Qupperneq 31
Qupperneq 32
Qupperneq 33
Qupperneq 34
Qupperneq 35
Qupperneq 36
Qupperneq 37
Qupperneq 38
Qupperneq 39
Qupperneq 40
Qupperneq 41
Qupperneq 42
Qupperneq 43
Qupperneq 44
Qupperneq 45
Qupperneq 46
Qupperneq 47
Qupperneq 48
Qupperneq 49
Qupperneq 50
Qupperneq 51
Qupperneq 52
Qupperneq 53
Qupperneq 54
Qupperneq 55
Qupperneq 56
Qupperneq 57
Qupperneq 58
Qupperneq 59
Qupperneq 60
Qupperneq 61
Qupperneq 62
Qupperneq 63
Qupperneq 64
Qupperneq 65
Qupperneq 66
Qupperneq 67
Qupperneq 68
Qupperneq 69
Qupperneq 70
Qupperneq 71
Qupperneq 72
Qupperneq 73
Qupperneq 74
Qupperneq 75
Qupperneq 76
Qupperneq 77
Qupperneq 78
Qupperneq 79
Qupperneq 80
Qupperneq 81
Qupperneq 82
Qupperneq 83
Qupperneq 84
Qupperneq 85
Qupperneq 86
Qupperneq 87
Qupperneq 88
Qupperneq 89
Qupperneq 90
Qupperneq 91
Qupperneq 92
Qupperneq 93
Qupperneq 94
Qupperneq 95
Qupperneq 96
Qupperneq 97
Qupperneq 98
Qupperneq 99
Qupperneq 100
Qupperneq 101
Qupperneq 102
Qupperneq 103
Qupperneq 104
Qupperneq 105
Qupperneq 106
Qupperneq 107
Qupperneq 108
Qupperneq 109
Qupperneq 110
Qupperneq 111
Qupperneq 112
Qupperneq 113
Qupperneq 114
Qupperneq 115
Qupperneq 116
Qupperneq 117
Qupperneq 118
Qupperneq 119
Qupperneq 120
Qupperneq 121
Qupperneq 122
Qupperneq 123
Qupperneq 124
Qupperneq 125
Qupperneq 126
Qupperneq 127
Qupperneq 128
Qupperneq 129
Qupperneq 130
Qupperneq 131
Qupperneq 132
Qupperneq 133
Qupperneq 134
Qupperneq 135
Qupperneq 136
Qupperneq 137
Qupperneq 138
Qupperneq 139
Qupperneq 140
Qupperneq 141
Qupperneq 142
Qupperneq 143
Qupperneq 144

x

Greinar (Vísindafélag Íslendinga)

Direct Links

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

Link til denne avis/magasin: Greinar (Vísindafélag Íslendinga)
https://timarit.is/publication/1732

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.