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Titolo:
Salt tectonics as a self-organizing process: A reaction, transport, and mechanics model
Autore:
Tuncay, K; Ortoleva, P;
Indirizzi:
Indiana Univ, Dept Chem, Lab Computat Geodynam, Bloomington, IN 47405 USA Indiana Univ Bloomington IN USA 47405 Geodynam, Bloomington, IN 47405 USA
Titolo Testata:
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
fascicolo: B1, volume: 106, anno: 2001,
pagine: 803 - 817
SICI:
0148-0227(20010110)106:B1<803:STAASP>2.0.ZU;2-H
Fonte:
ISI
Lingua:
ENG
Soggetto:
ROCK-SALT; ORGANIZATION; STYLOLITES; COMPACTION; DIAPIRISM; DYNAMICS; SOLIDS; MEDIA; LAWS;
Tipo documento:
Article
Natura:
Periodico
Settore Disciplinare:
Physical, Chemical & Earth Sciences
Citazioni:
63
Recensione:
Indirizzi per estratti:
Indirizzo: Tuncay, K Indiana Univ, Dept Chem, Lab Computat Geodynam, Chem Bldg, Bloomington, IN47405 USA Indiana Univ Chem Bldg Bloomington IN USA 47405 ton, IN47405 USA
Citazione:
K. Tuncay e P. Ortoleva, "Salt tectonics as a self-organizing process: A reaction, transport, and mechanics model", J GEO R-SOL, 106(B1), 2001, pp. 803-817

Abstract

Salt tectonics is placed within the theory of nonlinear dynamical systems. Features such as waves, diapirs, and tears are viewed as natural consequences of the symmetry breaking instabilities and related self-organized dynamics of the deforming salt body coupled to the reaction, transport, and mechanics of the surrounding sediments. The fundamental nonlinearities are in the surrounding-rock and salt rheology. Our findings are based on a coupled RTM model simulated using finite element techniques. The centerpiece of therheology of both rocks and salt is a nonlinear incremental stress formulation that integrates poroelasticity, continuous irreversible mechanical deformation (with yield behavior), pressure solution, and fracturing. In contrast to previously presented studies, in our approach the descriptive variables of all solid and fluid phases (stress, velocity, concentrations, etc.) and porous media (texture, i.e., volume fractions, composition, etc.) are solved from RTM equations accounting for interactions and interdependencies between them. The role of the coupling between the spatial distribution of sediment input rate and diapir growth and stalling is examined as is the creation of an array of salt tectonic minibasins.

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Documento generato il 13/07/20 alle ore 14:10:27