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• W2000821321 abstract "Research Article| October 01, 2002 Glarus overthrust: A major pathway for the escape of fluids out of the Alpine orogen Nicolas P. Badertscher; Nicolas P. Badertscher 1Institut de Géologie, Université de Neuchâtel, Emile-Argand 11, 2007 Neuchâtel, Switzerland Search for other works by this author on: GSW Google Scholar Georges Beaudoin; Georges Beaudoin 2MEDEF, Département de Géologie et de Génie Géologique, Université Laval, Québec G1K 7P4, Canada Search for other works by this author on: GSW Google Scholar René Therrien; René Therrien 2MEDEF, Département de Géologie et de Génie Géologique, Université Laval, Québec G1K 7P4, Canada Search for other works by this author on: GSW Google Scholar Martin Burkhard Martin Burkhard 3Institut de Géologie, Université de Neuchâtel, Emile-Argand 11, 2007 Neuchâtel, Switzerland Search for other works by this author on: GSW Google Scholar Geology (2002) 30 (10): 875–878. https://doi.org/10.1130/0091-7613(2002)030<0875:GOAMPF>2.0.CO;2 Article history received: 23 Jan 2002 rev-recd: 10 Jun 2002 accepted: 18 Jun 2002 first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Nicolas P. Badertscher, Georges Beaudoin, René Therrien, Martin Burkhard; Glarus overthrust: A major pathway for the escape of fluids out of the Alpine orogen. Geology 2002;; 30 (10): 875–878. doi: https://doi.org/10.1130/0091-7613(2002)030<0875:GOAMPF>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Thrust-related fluid flow coupled with isotopic exchange between fluid and rock is simulated in a three-dimensional finite-element model of the Glarus nappe, eastern Swiss Alps. Numerical simulations are matched against well-established oxygen isotope gradients on the kilometer scale along the thrust. At internal southern locations, strongly channelized thrust-parallel fluid flow requires a high permeability contrast of >100:1 between the mylonite zone and country rocks and a high hydraulic head in the hinterland and footwall. In contrast, isotopic patterns ∼5–10 km farther north indicate a predominantly vertical, upward drainage of fluids. We propose a situation in which the Glarus thrust evolved northward across the boundary between the lithostatic and hydrostatic fluid- pressure regimes—the “impermeable cap.” A cyclic behavior of fluid-pressure buildup, fracturing, channelized fluid escape, and sealing explains structural and geochemical observations and the best-fit three-dimensional fluid-flow model parameters. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2000821321 title "Glarus overthrust: A major pathway for the escape of fluids out of the Alpine orogen" @default.
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