The quantification of crystallographic preferred orientation using magnetic anisotropy
dc.contributor.author | Richter, Carl | en_US |
dc.contributor.author | van der Pluijm, Ben A. | en_US |
dc.contributor.author | Housen, Bernard A. | en_US |
dc.date.accessioned | 2006-04-10T15:56:51Z | |
dc.date.available | 2006-04-10T15:56:51Z | |
dc.date.issued | 1993-01 | en_US |
dc.identifier.citation | Richter, Carl, van Der Pluijm, Ben A., Housen, Bernard A. (1993/01)."The quantification of crystallographic preferred orientation using magnetic anisotropy." Journal of Structural Geology 15(1): 113-116. <http://hdl.handle.net/2027.42/31050> | en_US |
dc.identifier.uri | http://www.sciencedirect.com/science/article/B6V9D-4887Y3V-65/2/c491930814c0ddbabed70bf38efa5d73 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/31050 | |
dc.description.abstract | Magnetic anisotropy analysis presents an alternative and fast method for obtaining and quantifying crystallographic preferred orientations in rocks, using relatively simple equipment. Two natural examples and numerical modeling demonstrate that magnetic anisotropy increases with increasing degree of crystallographic preferred orientation. The normalized magnetic parameters Mi = ln(ki/(kmax * kint * kmin)1/3) (kmax >= kint >= kmin are the principal magnetic susceptibilities) correlate directly with March `strains' obtained from X-ray texture goniometry. The additional advantage of our method is that the preferred fabrics are determined from large sample volumes (typically about 11 cm3) rather than the essentially two-dimensional slice used in optical and X-ray methods. Thus, magnetic anisotropy provides a reliable measure of bulk crystallographic preferred orientation in rocks. | en_US |
dc.format.extent | 343487 bytes | |
dc.format.extent | 3118 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Elsevier | en_US |
dc.title | The quantification of crystallographic preferred orientation using magnetic anisotropy | en_US |
dc.type | Article | en_US |
dc.rights.robots | IndexNoFollow | en_US |
dc.subject.hlbsecondlevel | Geology and Earth Sciences | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, U.S.A. | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, U.S.A. | en_US |
dc.contributor.affiliationum | Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, U.S.A. | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/31050/1/0000727.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1016/0191-8141(93)90082-L | en_US |
dc.identifier.source | Journal of Structural Geology | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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