Devonian-Carboniferous extension and Eurekan inversion along an inherited WNW-ESE-striking fault system in Billefjorden, Svalbard.

Open Res Eur · 2023 · PMC10646348 · PMID 37969247

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a pronounced trendno p-value reported

Comment 34: You can map these through the moraine? Response: If there is a pronounced trend of WNW–ESE-striking faults in Billefjorden, it is possible that some of these are actually newly formed Cenozoic (Quaternary?) faults forming due to minor adjustments in the crust and therefore partly cut through the moraine.

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