An intensive mineralogic and geochemical investigation was conducted on sediments recovered during Ocean Drilling Program Leg 166 from the western Great Bahama Bank at Sites 1006, 1008, and 1009. Pleistocene through middle Miocene sediments recovered from Site 1006, the distal location on the Leg 166 transect, are a mixture of bank-derived and pelagic carbonates with lesser and varying amounts of siliciclastic clays. A thick sequence of Pleistocene periplatform carbonates was recovered near the platform edge at Sites 1008 and 1009. Detailed bulk mineralogic, elemental (Ca, Mg, Sr, and Na), and stable isotopic (d18O and d13C) analyses of sediments are presented from a total of 317 samples from all three sites
Stable isotopic and minor element compositions were measured on the fine fraction of pelagic carbona...
This report presents mineralogic and geochemical data from Ocean Drilling Program Leg 182 Site 1128 ...
To date, work on the Great Bahama Bank's western, leeward margin has centred chiefly on seismic-scal...
The carbon-isotopic composition (d13C) of bulk carbonates, obtained from a transect of sites drilled...
The stable isotope geochemistry of Miocene sediments from the leeward margin of the Great Bahama Ban...
In order to investigate the spatial distribution of δ13C and δ18O of modern carbonate sediments on G...
Abstract: Ocean Drilling Program (ODP) Leg 166 cored a transect of holes through the prograding carb...
In order to investigate the spatial distribution of ö13C and 8180 of modern carbonate sedirnents on ...
The stable isotope geochemistry of Miocene sediments from the leeward margin of the Great Bahama Ban...
International audienceThe western flank of the Great Bahama Bank, drilled during ODP Leg 166 at seve...
A detailed geochemical investigation was conducted of Upper Cretaceous to Holocene sediments recover...
The western flank of the Great Bahama Bank, drilled during ODP Leg 166 at seven sites, represents a ...
The stable isotope geochemistry of Miocene sediments from the leeward margin of the Great Bahama Ban...
Site 716 is a continuous sequence (upper Miocene to Holocene) of periplatform oozes and chalks from ...
Isotopic signature of burial diagenesis and primary lithological contrasts in periplatform carbonate
Stable isotopic and minor element compositions were measured on the fine fraction of pelagic carbona...
This report presents mineralogic and geochemical data from Ocean Drilling Program Leg 182 Site 1128 ...
To date, work on the Great Bahama Bank's western, leeward margin has centred chiefly on seismic-scal...
The carbon-isotopic composition (d13C) of bulk carbonates, obtained from a transect of sites drilled...
The stable isotope geochemistry of Miocene sediments from the leeward margin of the Great Bahama Ban...
In order to investigate the spatial distribution of δ13C and δ18O of modern carbonate sediments on G...
Abstract: Ocean Drilling Program (ODP) Leg 166 cored a transect of holes through the prograding carb...
In order to investigate the spatial distribution of ö13C and 8180 of modern carbonate sedirnents on ...
The stable isotope geochemistry of Miocene sediments from the leeward margin of the Great Bahama Ban...
International audienceThe western flank of the Great Bahama Bank, drilled during ODP Leg 166 at seve...
A detailed geochemical investigation was conducted of Upper Cretaceous to Holocene sediments recover...
The western flank of the Great Bahama Bank, drilled during ODP Leg 166 at seven sites, represents a ...
The stable isotope geochemistry of Miocene sediments from the leeward margin of the Great Bahama Ban...
Site 716 is a continuous sequence (upper Miocene to Holocene) of periplatform oozes and chalks from ...
Isotopic signature of burial diagenesis and primary lithological contrasts in periplatform carbonate
Stable isotopic and minor element compositions were measured on the fine fraction of pelagic carbona...
This report presents mineralogic and geochemical data from Ocean Drilling Program Leg 182 Site 1128 ...
To date, work on the Great Bahama Bank's western, leeward margin has centred chiefly on seismic-scal...