Dataset - B2FIND

Chemical compositions of representative lithologies from IODP Hole 357-M0075B

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Chemical compositions of representative lithologies from IODP Hole 357-M0072B

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Chemical compositions of representative lithologies from IODP Hole 357-M0071C

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Chemical compositions of representative lithologies from IODP Hole 357-M0071A

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Chemical compositions of representative lithologies from IODP Hole 357-M0069A

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Chemical compositions of representative lithologies from IODP Hole 357-M0068B

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Chemical compositions of representative lithologies from IODP Hole 357-M0068A

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(Table 1) Determined and theoretical chemical composition of thaumasite of OD...

Hole 841B was drilled in the forearc region of the Lau Basin at a water depth of 4810 m. The hole penetrated a roughly 500-m-thick series of Miocene volcanic sediments with a...

(Table 1) Geochemistry of ODP Hole 128-798B

Because of heterogeneity, average values of sediment composition can be difficult to establish accurately in fine-grained rocks. As a result, derived values (such as biogenic...

(Table 1) Composition of selected ash layers in ODP Site 126-792

Glass shards from 26 megascopic tephras (1-29 cm thick) were separated and analyzed for 26 elements and 87Sr/86Sr and 143Nd/144Nd isotope ratios. The isotope data allowed us to...

Major and trace element analyses of ODP Leg 120 volcanic rocks (Table 1)

Widespread Lower Cretaceous magmatism occurred along the Indian-Australian/Antarctic margins, and in the juvenile Indian Ocean, during the rifting of eastern Gondwana. The...

Major and trace element abundance in sediment samples from ODP Hole 121-758B ...

Major and trace element analyses of 30 sediment samples from ODP Core 758B across the Brunhes-Matuyama geomagnetic polarity reversal and the Australasian microtektite-bearing...