Náttúrufræðingurinn

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Náttúrufræðingurinn - 1989, Qupperneq 20

Náttúrufræðingurinn - 1989, Qupperneq 20
Sigurðsson & Þórólfur H. Hafstað 1989. Skilyrði til fiskeldis í Öxarfirði. Ferskvatn, jarðsjór, jarðhiti og rann- sóknarboranir. Orkustofnun. OS-89041/JHD-08. 61 bls. Simoneit, B.R.T. & P.F. Lonsdale 1982. Hydrothermal petroleum in minera- lized mounds at the seabed of Guaym- as Basin. Nature 295. 198-202. Sveinn P. Jakobsson 1979. Petrology of Recent basalts of the Eastern Volcanic Zone, Iceland. Acta Naturalia Island- ica 26. 103 bls. Sveinn P. Jakobsson & Guðmundur Ó. Friðleifsson 1986. Det förste fund af naturlig asfalt i Island. Bls. 61 í 17e Nordiska Geologmötet, Helsingfors. Abstracts. Sveinn P. Jakobsson & J.G. Moore 1986. Hydrothermal minerals and alteration rates at Surtsey volcano, Iceland. Geol. Soc. Amer. Bull. 97. 648-659. Tissot, B.P. & D.H. Welte 1984. Petro- leum formation and occurrence, (2. útg.). Springer-Verlag, Berlin. 699 bls. Walker, G.P.L. & D.H. Blake 1966. The formation of a palagonite breccia mass beneath a valley glacier in Iceland. Qu- art. Journal of the Geological Society, London. 122. 45-61. SUMMARY Asphaltic petroleum in amygdales in Skyndidalur, Lón, SE Iceland. by Sveinn P. Jakobsson Icelandic Museum of Natural History P.O. Box 5320 IS-125 REYKJAVÍK, Iceland and Guðmundur Ó. Friðleifsson National Energy Authority Grensásvegur 9 1S-108 REYKJAVÍK, Iceland. In August 1985 an unusual amygdale was brought to the Icelandic Museum of Natural History by amateur rock collec- tors. The amygdale contained asphaltic- like material which smelled like crude oil. This is the first discovery of petroleum in Iceland. It was found near the centre of a large vesicle which was lined by large clear quartz crystals and calcite (front page). The amygdale was collected in a basaltic lava in a mountainous region in SE Ice- land. The authors of this article made two site visits in 1985. The locality is at the snout of the Lambatungnajökull (glacier) in Skyndi- dalur, in Lónsöræfi, SE Iceland. The as- phaltic petroleum occurs in amygdales in a lava of Miocene age (about 5 m.y.) at the base of Lambatungnatindur (figs. I, 2 & 3). Below the lava a thin lignite bed oc- curs, which, in turn is intruded by a basal- tic sheet (fig. 4). Fig. I shows the regional geology (simplified after Torfason, 1979 and Fridleifsson, 1983a). The asphalt- bearing lava is located on the flanks of the Kollumúli central volcano in the northeast and the Geitafell central volcano in the southwest. Several unconformities are found within the strata, some of which are of importance in relation to the liydro- 186

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