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                                       Details van artikel 2 van 9 gevonden artikelen
 
 
  Bjorko, a possible Middle Proterozoic impact structure west of Stockholm, Sweden
 
 
Titel: Bjorko, a possible Middle Proterozoic impact structure west of Stockholm, Sweden
Auteur: Floden, Tom
Soderberg, Per
Wickman, Frans E.
Verschenen in: GFF
Paginering: Jaargang 115 (1993) nr. 1 pagina's 25-38
Jaar: 1993-03-01
Inhoud: The Bjorko structure in the Bjorkfjarden Bay area of Lake Malaren is one of more than 20 possible impact structures in Sweden. Rasta on Ekeron Island forms the eastern part and the islands of Pingst and Midsommar the southwestern part of this 8 km wide probable impact, which seems to be thoroughly altered by erosion. Despite alteration by erosion and sediment infilling, we tentatively place the location of the central uplift of the impact at Ingaberg on Bjorko Island which is surrounded by a depression in crystalline bedrock. Along parts of the outer rim of the impact we find possible remnants of a wall structure. Nine published papers about the Bjorkfjarden Bay area are reviewed and the numerous observations that, in our opinion, support the impact hypothesis are emphasized. New results in favour of an impact origin of the structure are also presented. Chemical analyses of the claystone which forms the basal part of the Bjorko structure infilling show that it mainly consists of a mica-type mineral. K-Ar datings of the claystone have given Middle Proterozoic 'Jotnian' ages of 1203 and 1216 Ma. It is interpreted here as a possible layer of impact melt. Planar elements in quartz occur in sandstone from Midsommar Island. The surface relief and internal geometry of the Bjorko structure are demonstrated by seismic reflection and refraction soundings, which show that the bedrock of Bjorkfjarden Bay consists almost entirely of sandstone reaching a thickness of some 250 m in its southwestern parts. The solid rock is covered by a fairly even layer of glacial and postglacial deposits 20 to 40 m in thickness. The lake floor is largely depositional with the Recent sediments cut by erosional channels.
Uitgever: Taylor & Francis
Bronbestand: Elektronische Wetenschappelijke Tijdschriften
 
 

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