A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2011; you can also visit the original URL.
The file type is application/pdf
.
A Re-Evaluation of Facies on Great Bahama Bank II: Variations in the δ13C, δ18O and Mineralogy of Surface Sediments
[chapter]
2012
Perspectives in Carbonate Geology
In order to investigate the spatial distribution of 13 C and 18 O of modern carbonate sediments on Great Bahama Bank, ~290 surface samples were collected from a grid of stations approximately 10 km apart between 2001 and 2004. These samples were classifi ed using a modifi ed Dunham scheme, physically separated into six size fractions and subsequently analysed for their mineralogy (aragonite, low-Mg calcite and high-Mg calcite) and 13 C and 18 O values. A striking feature of these data
doi:10.1002/9781444312065.ch4
fatcat:gfjpjjjgcbgqncnw25gcq7w2ne