Item talk:Q239021

From geokb

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   "abstract": "Drill core FC 77\u20101 on the flank of the central uplift, Flynn Creek impact structure, Tennessee, contains 175\u00a0m of impact breccia lying upon uplifted Lower Paleozoic carbonate target stratigraphy. Sedimentological analysis of this 175\u2010m interval carbonate breccia shows that there are three distinct sedimentological units. In stratigraphic order, unit 1 (175\u2013109\u00a0m) is an overall coarsening\u2010upward section, whereas the overlying unit 2 (109\u201332\u00a0m) is overall fining\u2010upward. Unit 3 (32\u20130\u00a0m) is a coarsening\u2010upward sequence that is truncated at the top by postimpact erosion. Units 1 and 3 are interpreted as debris or rock avalanches into finer sedimentary deposits within intracrater marine waters, thus producing progressively coarser, coarsening\u2010upward sequences. Unit 2 is interpreted to have formed by debris or rock avalanches into standing marine waters, thus forming sequential fining\u2010upward deposits. Line\u2010logging of clasts ranging from 5\u00a0mm to 1.6\u00a0m, and thin\u2010section analysis of selected drill core samples (including clasts < 5\u00a0mm), both show that the Flynn Creek impact breccia consists almost entirely of dolostone clasts (90%), with minor components of cryptocrystalline melt clasts, chert and shale fragments, and clastic grains. Cryptocrystalline melt clasts, which appear isotropic in thin section, are in fact made of exceedingly fine quartz crystals that exhibit micro\u2010Fourier transform infrared (FTIR ) and micro\u2010Raman spectra consistent with crystalline quartz. These cryptocrystalline melt clasts are the first melt clasts of any kind to be reported from Flynn Creek impact structure.",
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