Geology of the Early Palaeozoic Lockne impact structure, Central Sweden.

Details Geology of the Early Palaeozoic Lockne impact structure, Central Sweden. Geology of the Early Palaeozoic Lockne impact structure, Central Sweden.

Dec 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992tectp.216..169l&link_type=abstract

Tectonophysics, Vol. 216, No. 1/2, p. 169 - 185

Physics

14

Scientific paper

The diameter of the crater at Lockne as seen on topographic maps is 7-8 km. The Tandsbyn Breccia, the principal evidence of impact, consists of strongly crushed local basement. Its distribution follows the crater margin. The Lockne Breccia, together with a less coarsely grained turbidite ("Loftarsten"), which lies immediately above it, predominantly consist of clasts of lower to middle Ordovician limestone and, mainly subordinate, inclusions of Tandsbyn Breccia and isolated clasts of crystalline basement.

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