Thursday, July 25, 2013

Basin-plain turbidites (Lower Eocene), Zumaya beach, northern Spain, and Contourites, Off Great Bahama Bank


GEOLOGY (1985, April, v. 13, No. 4)

Caption: Thin-bedded, calcareous, turbidite sandstones, and inter-bedded hemipelagic mudstones of basin-plain facies. Lower Eocene, Zumaya beach, northern Spain. Photo by G. Shanmugam

 


 
GEOLOGY (1983, January, v. 11, No. 1)
 
Caption: SEM photograph of a contourite sample showing clean planktonic formainiferal surface caused by winnowing away of muddy sediment by vigorous bottom currents (see Geology, v. 10, p. 231-235 and this issue p. 58). Growth of halite crystals is due to evaporation when sample was brought to surface from seafloor. Off Great Bahama Bank. University of North Carolina Collection. SEM photograph by G. Shanmugam and J.J. Porter, Mobil Research and Development Corporation, Dallas, Texas.



 

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