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Glacially-Triggered Faultingкнига
- Авторы: Steffen H., Olesen O., Sutinen R., Steffen R., Wu P., Lund B., Sandersen P.B.E, Müller K., Winsemann J., Pisarska-Jamroży M., Lege T., Spies T., Brandes C., Palmu J.P., Ojala A., Mattila J., Markovaara-Koivisto M., Ruskeeniemi T., Bauer T., Keiding M., Gestermann N., Plenefisch T., Beckel R., Juhlin C., Malehmir A., Ahmadi O., Smith C.A., Grigull S., Mikko H., Ask M., Kukkonen I., Fagereng Å., Rutqvist J., Rosberg J.E., Lorenz H., Gregersen S., Lindholm C., Korja A., Uski M., Oinonen K., Voss P.H., Olsen L., Gibbons S., Ruud B.O., Høgaas F., Johansen T.A., Kværna T., Hyvönen E., Middleton M., Nikolaeva S., Nikonov A., Shvarev S., Voss P., Tanner D., van Loon T., Wozniak P.P., Bitinas A., Lazauskienė J., Adams J., Brooks G., Sauber J., Rollins C., Freymueller J.T., Ruppert N.A., Gradmann S.
- Год издания: 2022
- Издательство: Cambridge University Press
- Местоположение издательства: United Kingdom
- Объём: 460 страниц
- ISBN: 978-1-108-49002-3
- Монография
- Академическое издание
- DOI: 10.1017/9781108779906
- Аннотация: Glacially triggered faulting describes movement of pre-existing faults caused by a combination of tectonic and glacially induced isostatic stresses. The most impressive fault scarpsare found in Northern Europe, assumed to have been reactivated at the end of deglaciation.However, this view has been challenged as new faults have been discovered globally withadvanced techniques such as LiDAR, and fault activity dating has shown several phases ofreactivation thousands of years after deglaciation ended. This book summarizes the currentstate-of-the-art research in glacially triggered faulting, discussing the theoretical aspects thatexplain the presence of glacially induced structures and reviews the geological, geophysical, geodetic and geomorphological investigation methods. Written by a team of international experts, it provides the first global overview of confirmed and proposed glaciallyinduced faults and provides an outline for modelling these stresses and features. It is a go-toreference for geoscientists and engineers interested in ice sheet–solid earth interaction.
- Добавил в систему: Шварев Сергей Валентинович