Normal faulting and block tilting in Lofoten and Vesteralen constrained by Apatite Fission Track data

Mesozoic and possibly younger normal faulting and block tilting in the Lofoten-Vesteralen archipelago can be constrained by Apatite Fission Track data. Previous studies have documented the polyphase structural evolution of the archipelago, based on field data and onshore-offshore correlations. Our new AFT data document vertical movements on a more regional scale, with kilometer-scale offset on some faults. Below Sortlandsundet, the Hadselfjord Fault Zone forms the eastern limit of the Sortlandsundet half-graben and our data reveal latest Cretaceous and younger half-dome shaped uplift of the footwall. East of the Western Lofoten Border Fault, on Vestvagoya, southeastward tilting is indicated both by the pattern of AFT ages, ranging from 81 +/- 7 Ma to in the NW to 167 +/- 16 Ma in the SE, and tilted paleosurfaces. AFT ages immediately east of Sortlandsundet (72 +/- 5 Ma) and on Vestvagoya (81 +/- 7 Ma) are among the youngest ones found on the Norwegian mainland. The present-day landscape of the Lofoten-Vesteralen archipelago does not represent a re-exposed and glacially modified Mesozoic landscape. Although most of our data indicate cooling to below similar to 60 degrees C took place during the Mesozoic, the youngest footwall ages are hard to explain without alluding to Cenozoic normal faulting. A Cenozoic structural control on the landscape can thus be inferred for Lofoten and Vesteralen. (C) 2010 Elsevier B.V. All rights reserved. Mesozoic and possibly younger normal faulting and block tilting in the Lofoten-Vesteralen archipelago can be constrained by Apatite Fission Track data. Previous studies have documented the polyphase structural evolution of the archipelago, based on field data and onshore-offshore correlations. Our new AFT data document vertical movements on a more regional scale, with kilometer-scale offset on some faults. Below Sortlandsundet, the Hadselfjord Fault Zone forms the eastern limit of the Sortlandsundet half-graben and our data reveal latest Cretaceous and younger half-dome shaped uplift of the footwall. East of the Western Lofoten Border Fault, on Vestvagoya, southeastward tilting is indicated both by the pattern of AFT ages, ranging from 81 +/- 7 Ma to in the NW to 167 +/- 16 Ma in the SE, and tilted paleosurfaces. AFT ages immediately east of Sortlandsundet (72 +/- 5 Ma) and on Vestvagoya (81 +/- 7 Ma) are among the youngest ones found on the Norwegian mainland. The present-day landscape of the Lofoten-Vesteralen archipelago does not represent a re-exposed and glacially modified Mesozoic landscape. Although most of our data indicate cooling to below similar to 60 degrees C took place during the Mesozoic, the youngest footwall ages are hard to explain without alluding to Cenozoic normal faulting. A Cenozoic structural control on the landscape can thus be inferred for Lofoten and Vesteralen. (C) 2010 Elsevier B.V. All rights reserved.