Carbon isotope ratios in dolostones: some implications concerning the genesis of secondary and "primary" dolostones

Details Carbon isotope ratios in dolostones: some implications concerning the genesis of secondary and "primary" dolostones Carbon isotope ratios in dolostones: some implications concerning the genesis of secondary and "primary" dolostones

Aug 1964

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1964gecoa..28.1257w&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 28, Issue 8, pp.1257-1265

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Scientific paper

C 12 /C 13 ratios in conjunction with aluminium and chloride ion contents of some Paleozoic dolostones suggest that some of the fine-grained, so-called "primary" dolostones may have originated in areas receiving appreciable terrestrial detrital material, whereas other fine-grained dolostones originated in evaporitic basins. Coarse-grained, so-called "secondary" dolostones appear to have formed in normal marine environments where conditions of normal salinity and low clay mineral content permitted the formation of bioclastic limestones.

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