Brittle deformation of quartz in a diamond anvil cell

Quartz single crystals were deformed by brittle processes in a diamond anvil cell at high confining pressure (800–1200 MPa) and room temperature in the presence of water.

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Bibliographic Details
Published in:	Journal of structural geology Vol. 27; no. 6; pp. 943 - 947
Main Authors:	Bisschop, J., den Brok, B., Miletich, R.
Format:	Journal Article
Language:	English
Published:	Elsevier Ltd 01-06-2005
Subjects:	Deformation Diamond anvil cell Microcracking Quartz Microcracking Diamond anvil cell Deformation Quartz
Online Access:	Get full text
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Description
Summary:	Quartz single crystals were deformed by brittle processes in a diamond anvil cell at high confining pressure (800–1200 MPa) and room temperature in the presence of water.
Bibliography:	ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23
ISSN:	0191-8141 1873-1201
DOI:	10.1016/j.jsg.2005.03.001