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(Article of periodic en Anglais - 2002)

Document title

Stream response to repeated coseismic folding, Tiptonville dome, New Madrid seismic zone

Abstract

Active folding in the New Madrid seismic zone (NMSZ) forms the Tiptonville dome, a 15 km long and 5 km wide surface fold with up to 11 m of late Holocene structural relief. The fold is crossed by streams of varying size, from the Mississippi River to small floodplain streams. The aim of this paper is threefold : to determine the style and amount of response of small- and large-scale rivers to well-dated earthquakes in the Reelfoot Lake area; to further constrain the style and timing of surface folding produced by these earthquakes; and to partition the amount of deformation produced by individual events

Source

Article of periodic

published at : Geomorphology / ISSN 0169-555X

Editor : Elsevier, Amsterdam - PAYS-BAS (1987)

Millesime : 2002, vol. 43, no3-4 [pp. 313-349]

Bibliographic references : 71 ref.

Collation : Illustration ;

Language

Anglais

INIST-CNRS, Cote INIST : 21151

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2003.
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