| Reference Type | Journal (article/letter/editorial) |
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| Title | Investigations on the deformation of experimentally shock-loaded biotites using X-ray single crystal diffraction techniques |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Schneider, Hartmut | Author |
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| Year | 1978 (March) | Volume | 42 |
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| Issue | 321 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_42/42-321-41.pdf+ |
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| DOI | doi:10.1180/minmag.1978.042.321.05Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 2856 | Long-form Identifier | mindat:1:5:2856:5 |
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| GUID | 0 |
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| Full Reference | Schneider, Hartmut (1978) Investigations on the deformation of experimentally shock-loaded biotites using X-ray single crystal diffraction techniques. Mineralogical Magazine, 42 (321) 41-44 doi:10.1180/minmag.1978.042.321.05 |
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| Plain Text | Schneider, Hartmut (1978) Investigations on the deformation of experimentally shock-loaded biotites using X-ray single crystal diffraction techniques. Mineralogical Magazine, 42 (321) 41-44 doi:10.1180/minmag.1978.042.321.05 |
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| In | (1978, March) Mineralogical Magazine Vol. 42 (321) Mineralogical Society |
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| Abstract/Notes | SummaryThe deformation of biotite single crystals submitted to experimental shock-pressures of about 200 and 400 kb with direction of the shock wave parallel to [001] was investigated by X-ray precession and Weissenberg techniques. The X-ray analysis reveals a ‘fracturing’ of the biotite crystals upon pressure release into relatively large lattice blocks (> 1000 Å), which increases with the degree of shock compression. Deformation is inferred to take place by gliding and/or microfracturing processes parallel to the (010) and (110) lattice planes. Chains of tetrahedra running parallel to [100] and [110] probably exert a controlling influence on shock deformation mechanisms. |
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