Dataset - B2FIND

Range table from nannofossils in ODP Hole 179-1105A

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Moisture and density measured on ODP Hole 179-1105A

Method A: wet-bulk volume measured with special volume sampler; method B: wet-bulk volume measured by gas pycnometry; method C: dry volume measured by gas pycnometry

Core/Section summary of ODP Hole 179-1105A

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Hole/Core summary of ODP Site 179-1105

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X-ray fluorescence on samples of ODP Hole 179-1105A

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Paleontological investigation on nannofossils of ODP Hole 179-1105A

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Magnetic susceptibility on ODP Hole 179-1105A

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Point susceptibility (MS2F) on ODP Hole 179-1105A

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Natural gamma radiation of ODP Hole 179-1105A

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Mineral composition and major element oxides of gabbros from ODP Hole 179-110...

Hole 1105A penetrated 158 m of gabbros at a site offset 1.3 km east-northeast from Hole 735B on the Atlantis Bank near the Atlantis II Fracture Zone. A total of 118 m of...

Geochemical composition of gabbroic rocks from ODP Hole 179-1105A, southwest ...

Oxide-free olivine gabbro and gabbro, and oxide olivine gabbro and gabbro make up the bulk of the gabbroic suite recovered from Ocean Drilling Program (ODP) Leg 179 Hole 1105A,...

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...