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The Mjølnir Impact Event and its Consequences pp 1–22Cite as

Introduction

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Part of the book series: Impact Studies ((IMPACTSTUD))

Abstract

Impact cratering is one of the fundamental processes in our planetary system and an important factor in forming the lithosphere of the Earth and the planets. The active surface processes on Earth, e.g. weathering, erosion, plate tectonics, and volcanism change the Earth’s surface continuously. Therefore only a modest number of crater structures have been preserved and discovered on the surface of the Earth, compared to what can be seen on the less disturbed surfaces on the Moon and Mars (Melosh 1989; French 1998; Montanari and Koeberl 2000; Koeberl 2007) (Fig. 1.1).

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Authors and Affiliations

  1. Department of Geosciences, University of Oslo, NO-0316, Oslo, Norway

    Henning Dypvik & Filippos Tsikalas

  2. Geological Survey of Norway, NO-7491, Trondheim, Norway

    Morten Smelror

  3. SINTEF Petroleum Research, Trondheim, Norway

    Atle Mørk

  4. Department of Geology and Mineral Resources Engineering, NTNU, NO-7491, Trondheim, Norway

    Atle Mørk

  5. Eni Norge AS, NO-4064, Stavanger, Norway

    Filippos Tsikalas

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  1. Henning Dypvik
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Correspondence to Henning Dypvik .

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Editors and Affiliations

  1. Dept. Geology, University of Oslo, Oslo, Norway

    Filippos Tsikalas

  2. Dept. Geology, University of Oslo, Oslo, Norway

    Henning Dypvik

  3. (NGU), Geological Survey Norway, Trondheim, Norway

    Morten Smelror

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Dypvik, H., Smelror, M., Mørk, A., Tsikalas, F. (2010). Introduction. In: Tsikalas, F., Dypvik, H., Smelror, M. (eds) The Mjølnir Impact Event and its Consequences. Impact Studies. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-88260-2_1

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