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High-resolution X-ray texture goniometry

dc.contributor.authorvan der Pluijm, Ben A.en_US
dc.contributor.authorHo, Nei-Cheen_US
dc.contributor.authorPeacor, Donald R.en_US
dc.date.accessioned2006-04-10T18:03:26Z
dc.date.available2006-04-10T18:03:26Z
dc.date.issued1994-07en_US
dc.identifier.citationvan der Pluijm, Ben A., Ho, Nei-Che, Peacor, Donald R. (1994/07)."High-resolution X-ray texture goniometry." Journal of Structural Geology 16(7): 1029-1032. <http://hdl.handle.net/2027.42/31487>en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/B6V9D-48C8RS4-63/2/6f29ec3339ca682d9c08ce16af0884dben_US
dc.identifier.urihttps://hdl.handle.net/2027.42/31487
dc.description.abstractHigh-resolution X-ray texture goniometry (HRXTG) significantly improves peak/background ratios and allows for the determination of crystallographic preferred fabrics of small regions (2) in heterogeneously deformed rocks. The basic instrument is a commercially available automated single-crystal X-ray diffractometer equipped with a Mo source. A stage for transmission mode was constructed that is driven by the original motors, so the unit is fully computer controlled. Absorption corrections are calculated, which removes the need for generally difficult to obtain empirical corrections. This, combined with equipment optimization, enables us to use small irradiated volumes of rocks with variable compositions. The advantage of HRXTG in heterogeneously deformed rocks is demonstrated in a cleaved mudstone. Analysis of 2 areas in a 2 cm bed showing a gradation from micaceous sandstone to slate reveals that fabric intensity of both mica and chlorite increases significantly (dM from 0.64 to 1.03 and from 0.45 to 0.78, respectively), without appreciable change in the oblate shape (kM) of the fabric. Thus, HRXTG can record a strain state at the mm-scale of heterogeneously deformed rocks.en_US
dc.format.extent403297 bytes
dc.format.extent3118 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherElsevieren_US
dc.titleHigh-resolution X-ray texture goniometryen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelGeology and Earth Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumDepartment of Geological Sciences, University of Michigan, 1006 C.C. Little Building, Ann Arbor, MI 48109, U.S.A.en_US
dc.contributor.affiliationumDepartment of Geological Sciences, University of Michigan, 1006 C.C. Little Building, Ann Arbor, MI 48109, U.S.A.en_US
dc.contributor.affiliationumDepartment of Geological Sciences, University of Michigan, 1006 C.C. Little Building, Ann Arbor, MI 48109, U.S.A.en_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/31487/1/0000409.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1016/0191-8141(94)90084-1en_US
dc.identifier.sourceJournal of Structural Geologyen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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