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Age model and Nd isotope ratios of DSDO Hole 43-386 and ODP Hole 210-1276A
Modern thermohaline circulation plays a role in latitudinal heat transport and in deep-ocean ventilation, yet ocean circulation may have functioned differently during past... -
Palynology and sea surface temperature reconstruction for the mid-Cretaceous ...
The mid-Cretaceous is thought to be a greenhouse world with significantly higher atmospheric pCO2 and sea-surface temperatures as well as a much flatter latitudinal thermal... -
Geochemistry of ocean floor and forearc serpentinites
We provide new insights into the geochemistry of serpentinites from mid-ocean ridges (Mid-Atlantic Ridge and Hess Deep), passive margins (Iberia Abyssal Plain and Newfoundland)... -
Nannofossil biostratigraphy of ODP Site 210-1276 sediments
Ocean Drilling Program (ODP) Leg 210 is one of very few deep-sea legs drilled along the eastern Canadian continental margin. Most other drilling on this margin has been carried... -
Paleomagnetic and rock magnetic characterization of ODP Leg 210 cores
We conducted an integrated paleomagnetic and rock magnetic study on cores recovered from Ocean Drilling Program Sites 1276 and 1277 of the Newfoundland Basin. Stable components... -
Geochemical composition of ODP Site 210-1276 shales
During Ocean Drilling Program Leg 210, a greatly expanded sedimentary sequence of continuous Cretaceous black shales was recovered at Site 1276. This section corresponds to the... -
Major, trace and rare earth element concentration of ODP Site 210-1277 basalt...
Drilling of the distal Newfoundland margin at Ocean Drilling Program Site 1277 recovered part of the transition between exhumed sub-continental mantle lithosphere and normal... -
Ripple migration directions and grain fabric measurements on ODP Hole 210-127...
Albian turbidites and intercalated shales were cored from ~1145 to 1700 meters below seafloor at Site 1276 in the Newfoundland Basin. Strata at this level dip ~2.5° seaward... -
Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites
Sand detrital modes of Albian-Eocene clastic gravity-flow deposits cored and recovered at Ocean Drilling Program Site 1276 reflect the postrift geologic evolution of the... -
Ar and U-Th-Pb age determinations for minerals from ODP Holes of ODP Legs 173...
We report U-Pb and 39Ar-40Ar measurements on plutonic rocks recovered from the Ocean Drilling Program (ODP) Legs 173 and 210. Drilling revealed continental crust (Sites 1067 and... -
Major element concentrations in spinel, olivine and pyroxene from peridotites...
Serpentinized spinel peridotites of the Newfoundland margin drilled during ODP Leg 210 at Site 1277 have preserved, relic mineral compositions similar to the most depleted... -
Chemical and isotopic compositions of volcanics from ODP Hole 210-1276
Site 1276, Leg 210 of the Ocean Drilling Program, was located on the Newfoundland margin in a seismically-defined ~128 Ma "transitional" crust just west of the presumed oceanic...
