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Burks Mt. Ultramafic Complex exposed in serpentinite quarry

View on map:33.618528°N 82.216194°W

Comments

The Burks Mt. Ultramafic Complex in the serpentinite quarry here has a protolith of  olivine and orthpyroxene cut by talc-serpentine veins.  The complex contains  felsic rocks and amphibolies.  The complex may be an ophiolite sequence.  Stop 6 Dennis 

References

  • Page 47 - Dennis, A.J., 2016, Structural analysis of the Kiokee belt and its framing elements: Savannah River transect: Geol. Soc. Am. Field Guide 42, p. 37-51.
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