EXPERIMENTAL INVESTIGATION OF THE DISSOLUTION OF QUARTZ BY A MUSCOVITE MICA SURFACE: IMPLICATIONS FOR PRESSURE SOLUTION

dc.contributor.author	Meyer E.E.
dc.contributor.author	Israelachvili J.N.
dc.contributor.author	Greene G.W.
dc.contributor.author	Alcantar N.A.
dc.contributor.author	Boles J.R.
dc.date.accessioned	2025-02-22T06:17:58Z
dc.date.available	2025-02-22T06:17:58Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=28524644
dc.identifier.citation	Journal of Geophysical Research: Solid Earth, 2006, 111, 8, B08202
dc.identifier.issn	2169-9313
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/48083
dc.description.abstract	Using the surface forces apparatus, which can measure small changes in thickness occuring even at essentially geological timescales, we have measured dissolution of quartz sheets when pressed against muscovite mica surfaces in aqueous electrolyte solution, but no dissolution is observed under dry conditions. It is postulated that the dissolved quartz may reprecipitate outside the contact junction as a fragile silica gel, which could be the main factor limiting the rate of further dissolution. Copyright 2006 by the American Geophysical Union.
dc.title	EXPERIMENTAL INVESTIGATION OF THE DISSOLUTION OF QUARTZ BY A MUSCOVITE MICA SURFACE: IMPLICATIONS FOR PRESSURE SOLUTION
dc.type	Статья
dc.identifier.doi	10.1029/2005JB004010

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