Gilmour, I.; French, B.M.; Franchi, I.A.; Abbott, J. I.; Hough, R. M.; Newton, J. and Koeberl, C.
|DOI (Digital Object Identifier) Link:||http://doi.org/10.1016/S0016-7037(03)00213-8|
|Google Scholar:||Look up in Google Scholar|
The Gardnos impact structure in southern Norway is one of only two known impact structures (among ~175) whose impactites contain significant amounts (typically 0.2-1.0 wt.%) of carbon, or 5 to 10 times the amount present in the target rocks; Sudbury, Canada is the other. This study extends a previous investigation of the geochemistry and petrology of Gardnos impactites with additional sampling and a detailed investigation of the nature and possible origin of the carbonaceous material present.Two principal carbon components have been identified in Gardnos impactites: (1) impact-produced diamonds, 0.5 to 1 m in size, with a cubic crystal structure, predominantly hexagonal morphologies with platey layers and an estimated concentration of < 0.19 ppm in Gardnos suevites and (2) graphitic carbon ranging from poorly ordered to moderately crystalline.Geochemical data suggests that there are no suitable target rocks that could provide a single source for the carbon in Gardnos impactites. However, Raman spectroscopy, stable isotope analysis and transmission electron microscopy of the impact diamonds and graphitic carbon suggests that there were at least two episodes of C emplacement in Gardnos impactites: an impact-related incorporation and shock transformation of graphitic material from target rocks followed by later mobilization of C, possibly during postimpact cooling or later regional metamorphism.
|Item Type:||Journal Article|
|Academic Unit/Department:||Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Users 6044 not found.|
|Date Deposited:||17 Jul 2006|
|Last Modified:||04 Oct 2016 09:54|
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