Åvike Bay — a 10 km Diameter Possible Impact Structure at the Bothnian Sea Coast of Central Sweden
DOI | 10.1007/3-540-27548-7_12 |
---|---|
Aasta | 2005 |
Raamat | Impact Tectonics |
Toimetaja(d) | Koeberl, C., Henkel, H. |
Kirjastus | Springer |
Kirjastuse koht | Berlin, Heidelberg |
Leheküljed | 323-340 |
Tüüp | peatükk raamatus |
Eesti autor | |
Keel | inglise |
Id | 4266 |
Abstrakt
Åvike Bay is a 270° degree wide near-circular, 114 m deep bay on the Swedish coast of the Bothnian Sea, northeast of Sundsvall. The structure has a diameter of about 10 km. It was classified as a probable impact structure because of its extraordinary circular topography in the overwiew of impact structures in Fennoscandia. Recent studies lend further support to this interpretation. The structure has a submarine central mound, which is elevated some 40 m above the adjacent sea floor. It has a very distinct tangential and radial on-shore fracture pattern as seen in the topographic map. Along the southwestern shore of the Bay, an enigmatic quartzite breccia of unknown age occurs as part of a larger outcrop of polymict breccia with clasts of crystalline rocks and quartzite of unknown age. In thin section, planar fractures can be observed in quartz and feldspar grains. A detailed investigation showed that in a few cases the quartz grains contained microdeformation features closely resembling PDFs.