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(Table 1) Chemical composition of minerals from IODP Hole 305-U1309D
Samples taken between 746.2 and 751.0 mbsf. -
(Table 1) Major and trace element analyses of serpentinized peridotites and o...
This dataset has no description
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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... -
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... -
Trace element contents in zircons from oceanic crust
We present newly acquired trace element compositions for more than 300 zircon grains in 36 gabbros formed at the slow-spreading Mid-Atlantic and Southwest Indian Ridges. Rare... -
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... -
Geochemistry of IODP Hole 305-U1309D
Analysis of an in situ fault zone within the Atlantis Massif oceanic core complex (Mid-Atlantic Ridge) provides clues to the relevant deformation mechanisms and their temporal... -
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... -
(Table 2) Laboratory-derived permeability for IODP Hole 305-U1309D samples
Samples taken between 746.2 and 751.0 mbsf. -
(Table 2) Sulphur geochemistry of bulk-rock and extracted sulphide and sulpha...
This dataset has no description
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(Table 1) Sulphide assemblges of serpentinized harzburgites and olivine-rich ...
This dataset has no description
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(Table 5) Water-rock ratios for representative samples of Atlantis Massif IOD...
This dataset has no description
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(Table 3) Sr and Nd isotope composition, and Sr and carbonate contents of Atl...
This dataset has no description
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(Table A8) Major element analyses of spinel of IODP Holes 204-U1309D and 305-...
Sediment depth is given in mbsf. Standard deviation = 1 sigma of multiple determinations. -
(Table A7, Table 3) Major element analyses of olivine of IODP Holes 204-U1309...
Sediment depth is given in mbsf. Standard deviation = 1 sigma of multiple determinations. -
(Table A6) Major element analyses of plagioclase of IODP Holes 204-U1309D and...
Sediment depth is given in mbsf. Standard deviation = 1 sigma of multiple determinations. -
(Table A5, Table 2) Major and trace element analyses of plagioclases of IODP ...
Sediment depth is given in mbsf. Standard deviation = 1 sigma of multiple determinations, # = below detection limits. -
(Table A4, Table 1) Major and trace element analyses of clinopyroxenes of IOD...
Sediment depth is given in mbsf. Standard deviation = 1 sigma of multiple determinations.
