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(Table 3) Lithium concentrations in magmatic ocean-crust zircons from the Mid...
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Trace element composition of IODP Site 304-U1309 and 305-U1309 (Table A2)
IODP Site U1309 was drilled at Atlantis Massif, an oceanic core complex, at 30°N on the Mid-Atlantic Ridge (MAR). We present the results of a bulk rock geochemical study (major... -
(Table S1) Trace element analyses of normal magmatic zircon from ocean crust
Includes SHRIMP-RG data for samples U1309D-588, 3646-1000, 3652-1333, JR31 12-68, and JR31 22-1 that was previously published in Grimes et al. (2007), datasets:... -
(Table 1) Averaged trace element concentrations in zircons from the ocean crust
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(Online Resource 1) Oxygen-isotope ratios in zircon from ocean crust sampled ...
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(Table 1) Stable oxygen isotope ratios and temperture measurements in magneti...
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Trace element geochemistry of zircons frim in situ ocean lithoshere
We characterize the textural and geochemical features of ocean crustal zircon recovered from plagiogranite, evolved gabbro, and metamorphosed ultramafic host-rocks collected... -
Stable oxygen isotope ratios in zircons from oceanic crust
Lower ocean crust is primarily gabbroic, although 1-2% felsic igneous rocks that are referred to collectively as plagiogranites occur locally. Recent experimental evidence... -
Sulphur mineralogy and geochemistry of serpentinites and gabbros from the Atl...
In-situ uplifted portions of oceanic crust at the central dome of the Atlantis Massif (Mid-Atlantic Ridge, 30°N) were drilled during Expeditions 304 and 305 of the Integrated... -
Geochemistry of Atlantis Massif crust
The Atlantis Massif (Mid-Atlantic Ridge, 30°N) is an oceanic core complex marked by distinct variations in crustal architecture, deformation and metamorphism over distances of... -
Geochemistry of the gabbroic lithosphere in IODP Holes 304-U1309D and 305-U1309D
IODP Hole U1309D (Atlantis Massif, Mid-Atlantic Ridge 30°N) is the second deepest hole drilled into slow spread gabbroic lithosphere. It comprises 5.4% of olivine-rich... -
Petrology and geochemistry of peridotites from IODP Site 304-U1309
Peridotite samples recovered from IODP Site U1309 at the Atlantis Massif in the Mid-Atlantic Ridge were examined to understand magmatic processes for the oceanic core complex... -
Carbon geochemistry in serpentinites from and beneath the Lost City Hydrother...
The carbon geochemistry of serpentinized peridotites and gabbroic rocks recovered at the Lost City Hydrothermal Field (LCHF) and drilled at IODP Hole 1309D at the central dome... -
(Table S2) Trace element analyses of porous zircon and luminescent rims on zi...
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(Table 2) Physical properties of IODP rock samples measured under various con...
Measurements were carried out first under loading conditions (up to 50 MPa), then under unloading conditions (under 30 and 10MPa). -
(Table 1) Description of IODP rock samples from the Atlantis Massif, near the...
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(Table 2) Sulphur geochemistry of bulk-rock and extracted sulphide and sulpha...
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(Table 1) Sulphide assemblges of serpentinized harzburgites and olivine-rich ...
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(Table 5) Water-rock ratios for representative samples of Atlantis Massif IOD...
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(Table 3) Sr and Nd isotope composition, and Sr and carbonate contents of Atl...
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