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A TEM investigation of shock metamorphism in quartz from the Vredefort dome, South Africa
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“planar deformation features (PDFs) in quartz (e.g., Carter 1965; Leroux et al. 1994)”
From Observations and interpretations at Vredefort, Sudbury, and Chicxulub: Towards an empirical model of terrestrial impact basin formation (2008) · cites this paper as Leroux et al. 1994
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Research works printed but not linked: 33
- Albat, 1988, Shatter cone/bedding inter-relationship in the Vredefort structure: evidence for meteorite impact?, S. Afr. J. Geol., 91, 106
- Alexopoulos, 1988, Microscopic lamellar deformation features in quartz: discriminative characteristics of shock-generated varieties, Geology, 16, 796, 10.1130/0091-7613(1988)016<0796:MLDFIQ>2.3.CO;2 · DOI · Paper page
- Bisschoff, 1988, The history and origin of the Vredefort dome, S. Afr. J. Sci., 84, 413
- Brandl, 1990, The structural setting and deformation associated with pseudotachylite occurrences in the Palala shear belt and Sand River gneiss, Northern Transvaal, Tectonophysics, 171, 201, 10.1016/0040-1951(90)90099-T · DOI
- Carter, 1965, Basal quartz deformation lamellae—a criterion for recognition of impactites, Am. J. Sci., 263, 786, 10.2475/ajs.263.9.786 · DOI · Paper page
- Chopin, 1984, Coesite and pure pyrope in high-grade blueschists of the Western Alps: a first record and some consequences, Contrib. Mineral. Petrol., 86, 107, 10.1007/BF00381838 · DOI · Paper page
- Dietz, 1961, Vredefort ring structure: meteorite impact scar?, J. Geol., 69, 169, 10.1086/626768 · DOI
- Doukhan, 1985, Plastic deformation of quartz single crystals, Bull. Mineral., 108, 97
- Fricke, 1990, Fluid inclusions, planar elements and pseudotachylites in the basement of the Vredefort structure, South Africa, Tectonophysics, 171, 169, 10.1016/0040-1951(90)90097-R · DOI
- Goltrant, 1991, Planar deformation features in shocked quartz: a transmission electron microscopy investigation, Earth Planet. Sci. Lett., 106, 103, 10.1016/0012-821X(91)90066-Q · DOI
- Goltrant, 1992, Formation mechanisms of planar deformation features in shocked quartz, Phys. Earth Planet. Inter., 74, 219, 10.1016/0031-9201(92)90012-K · DOI
- Gratz, 1992, Shock metamorphism of quartz with initial temperatures — 170 to 1000°C, Phys. Chem. Miner., 19, 267, 10.1007/BF00204005 · DOI
- Grieve, 1990, Shocked minerals and the K/T controversy, Eos, 71, 1792, 10.1029/90EO00344 · DOI
- Grieve, 1990, Microscopic planar deformation features in quartz of the Vredefort structure: anomalous but still suggestive of an impact origin, Tectonophysics, 171, 185, 10.1016/0040-1951(90)90098-S · DOI
- Halvorson, 1992, Vredefort coesite confirmed with Raman spectroscopy, Lunar Planet. Sci., XXIII, 477
- Hart, 1991, Aspects of the dynamic and thermal metamorphic history of the Vredefort structure: implications for its origin, Tectonophysics, 192, 313, 10.1016/0040-1951(91)90106-3 · DOI
- Hobbs, 1968, Recrystallization of single crystals of quartz, Tectonophysics, 6, 353, 10.1016/0040-1951(68)90056-5 · DOI
- Kieffer, 1976, Shock processes in porous quartzite: transmission electron microscope observations and theory, Contrib. Minera. Petrol., 59, 41, 10.1007/BF00375110 · DOI
- Killick, 1990, Review of the pseudotachylites in and around the Vredefort Dome, S. Afr. J. Geol., 93, 350
- Lilly, 1981, Shock metamorphism in the Vredefort collar: evidence for internal shock sources, J. Geophys. Res., 85, 10689, 10.1029/JB086iB11p10689 · DOI
- Martini, 1978, Coesite and stishovite in the Vredefort Dome, South Africa, Nature, 272, 715, 10.1038/272715a0 · DOI · Paper page
- Martini, 1991, The nature, distribution and genesis of the coesite and stishovite associated with the pseudotachylite of the Vredefort Dome, South Africa, Earth Planet. Sci. Lett., 10, 285, 10.1016/0012-821X(91)90167-G · DOI
- McHone, 1988, Vredefort stishovite confirmed using solid-state silicon-29 nuclear magnetic resonance, Meteoritics, 23, 289
- McLaren, 1967, Transmission electron microscope study of Brazil twins and dislocations experimentally produced in natural quartz, Phys. Status Solidi, 19, 631, 10.1002/pssb.19670190216 · DOI
- McLaren, 1983, The mechanism of the formation and growth of water bubbles and associated dislocation loops in synthetic quartz, Phys. Chem. Miner., 9, 79, 10.1007/BF00308151 · DOI
- 1990, 171, 422
- Reimold, 1990, The controversial microdeformations in quartz from the Vredefort structure, South Africa—a discussion, S. Afr J. Geol., 93, 645
- Reimold, 1991, The geochemistry of pseudotachylites from the Vredefort dome, South Africa, Neues Jahrb. Miner. Abh., 162, 151
- Schreyer, 1983, Metamorphism and fluid inclusions in the basement of the Vredefort Dome, South Africa: guidelines to the origin of the structure, J. Petrol., 24, 26, 10.1093/petrology/24.1.26 · DOI
- Schwarzman, 1983, Pseudotachylite from the Vredefort ring, South Africa, and the origin of some lunar breccias, Bull. Geol. Soc. Am., 94, 926, 10.1130/0016-7606(1983)94<926:PFTVRS>2.0.CO;2 · DOI
- Smyth, 1977, A coesite-sanidine grospydite from the Roberts Victor Kimberlite, Earth Planet. Sci. Lett., 34, 284, 10.1016/0012-821X(77)90012-7 · DOI
- Stöffler, 1971, Coesite and stishovite in shocked crystalline rocks, J. Geophys. Res., 76, 5474, 10.1029/JB076i023p05474 · DOI
- Stöffler, 1972, Deformation and transformation of rockforming minerals by natural and experimental shock processes, 1. Behavior of minerals under shock compression, Fortschr. Miner., 49, 50
Cited by
Sorted by citations
GRIEVE, R. A. F., REIMOLD, W. U., MORGAN, J., RILLER, U., & PILKINGTON, M. (2008) · Meteoritics & Planetary Science · doi:10.1111/j.1945-5100.2008.tb01086.x · Cited by 90
Self-citation
Metadata
- Authors
- Leroux, H., Reimold, W. U., & Doukhan, J.-C.
- Venue
- Tectonophysics
- Publisher
- Elsevier BV
- Published
- 1994-02
- Volume
- 230
- Issue
- 3-4
- Pages
- 223-239
- ISSN
- 0040-1951
- Cited by
- 111
- References
- 0
- Language
- en
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
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