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- W2014731203 abstract "Research Article| June 01, 2009 Velocity of vertical fluid ascent within vein-forming fractures Atsushi Okamoto; Atsushi Okamoto * 1Graduate School of Environmental Studies, Tohoku University, Sendai 980-8579, Japan *E-mail: okamoto@mail.kankyo.tohoku.ac.jp. Search for other works by this author on: GSW Google Scholar Noriyoshi Tsuchiya Noriyoshi Tsuchiya 1Graduate School of Environmental Studies, Tohoku University, Sendai 980-8579, Japan Search for other works by this author on: GSW Google Scholar Geology (2009) 37 (6): 563–566. https://doi.org/10.1130/G25680A.1 Article history received: 18 Nov 2008 rev-recd: 05 Feb 2009 accepted: 06 Feb 2009 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Atsushi Okamoto, Noriyoshi Tsuchiya; Velocity of vertical fluid ascent within vein-forming fractures. Geology 2009;; 37 (6): 563–566. doi: https://doi.org/10.1130/G25680A.1 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 Quartz-albite-calcite veins in metamorphic rocks of the Sanbagawa belt, Japan, contain sugary mosaics of equant quartz grains <0.01–1.6 mm in size (blocky texture). The quartz crystals show euhed ral to subhedral double-terminated crystal shape, and concentric growth zoning, indicating suspension in aqueous fluid during crystal growth until formation of a framework within the crack. Such a crystallization process is only possible when downward crystal settling is balanced by upward fluid flow. Application of crystal settling theory to the crystal size distributions within the veins reveals an extremely high rate of fluid ascent during blocky vein formation (10−2 to 10−1 m/s) due to the low viscosity of the hydrothermal fluid (~10−4 Pa·s). Such a high rate of ascent suggests the injection of fluids from mobile hydrofractures within deeper levels of the subduction zone. 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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- W2014731203 title "Velocity of vertical fluid ascent within vein-forming fractures" @default.
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