Earthquake-induced deformation structures in glacial sediments—evidence on fault reactivation and instability at the Vaalajärvi fault in northern Fennoscandia-Reference-Cited by-同舟云学术

Earthquake-induced deformation structures in glacial sediments—evidence on fault reactivation and instability at the Vaalajärvi fault in northern Fennoscandia

Published:2020-04-21 Issue:3 Volume:24 Page:549-571
ISSN:1383-4649
Container-title:Journal of Seismology
language:en
Short-container-title:J Seismol

Author:

Ojala A.E.K.,Mattila J.,Middleton M.,Ruskeeniemi T.,Palmu J.-P.,Nordbäck N.,Kirsch M.,Lorenz S.,Zimmermann R.,Andreani L.,Jackisch R.,Unger G.,Gloaguen R.,Sutinen R.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

https://link.springer.com/content/pdf/10.1007/s10950-020-09915-6.pdf

Reference48 articles.

1. Ahjos T, Uski M (1992) Earthquakes in northern Europe in 1375-1989. Tectonophysics 207:1–23

2. Arvidsson R (1996) Fennoscandian earthquakes: whole crustal rupturing related to postglacial rebound. Science 274:744–746

3. Green AA, Bergman M, Switzer P, Craig MD (1988) A transformation for ordering multispectral data in terms of image quality with implications for noise removal. IEEE trans. Geosci. Remote Sens 26:65–74

4. Grützner C, Fischer P, Reicherter K (2016) Holocene surface ruptures of the Rurrand fault, Germany—insights from palaeoseismology, remote sensing and shallow geophysics. Geophys J Int 204:1662–1677

5. Hirvas H (1991) Pleistocene stratigraphy of Finnish Lapland. Geological Survey of Finland, Bulletin 354,123 pp

Cited by 3 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Porttipahta end moraine in Finnish Lapland is constrained to Early Weichselian (MIS 5d, Herning stadial);Geomorphology;2021-11

2. Subglacial squeeze-up moraines adjacent to the Vaalajärvi-Ristonmännikkö glacially-induced fault system, Finnish Lapland;Geomorphology;2021-07

3. Pattern recognition of LiDAR data and sediment anisotropy advocate a polygenetic subglacial mass-flow origin for the Kemijärvi hummocky moraine field in northern Finland;Geomorphology;2020-08