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Faults and faulting in the Horn Graben area, Danish North Sea

Ole Rønø Clausen, John A. Korstgård

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Abstract

The Horn Graben transects the Ringkobing-Fyn High-North Sea High system which is a WNW-ESE trending series of highs with a generally thin cover of Mesozoic and Tertiary sediments. This positive feature was formed during a major phase of regional tectonic activity in the Late Carboniferous-Early Permian. The paper reports the mapping of faults from seismic reflection surveys. -from Authors

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What this paper is about

The Horn Graben transects the Ringkobing-Fyn High-North Sea High system which is a WNW-ESE trending series of highs with a generally thin cover of Mesozoic and Tertiary sediments. This positive feature was formed during a major phase of regional tectonic activity in the Late Carboniferous-Early Permian. The paper reports the mapping of faults from seismic reflection surveys. -from Authors

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OpenAlex reports 14 citations for this work. Citation counts describe recorded attention and do not establish research quality.

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Available abstract

The Horn Graben transects the Ringkobing-Fyn High-North Sea High system which is a WNW-ESE trending series of highs with a generally thin cover of Mesozoic and Tertiary sediments. This positive feature was formed during a major phase of regional tectonic activity in the Late Carboniferous-Early Permian. The paper reports the mapping of faults from seismic reflection surveys. -from Authors

Key concepts: Geology, Graben, Telmatology, French horn, Metamorphic petrology, Paleontology, Seismology, Regional geology

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