Dataset - B2FIND

XRF logging data from Nussloch loess cores

The Nussloch Drilling Campaign (NUSS) involved drilling three loess sediment cores (85 mm in diameter) on April 21-25, 2019, on top of a loess hill at 49.31°N, 8.73°E, at an...

XRF derived elemental ratios and carbon content from ODP Site 177-722

Data included in this entry was sampled from ODP Site 722 (16.6218°N/59.7953°E). Original drilling was carried out by E/V JOIDES Resolution as part of ODP leg 117 between 6th...

(Table 1) Chemistry of two samples of the red weathered layer at DSDP Hole 55...

One argument for the subaerial formation of Nintoku Seamount in the Emperor chain is the occurrence of a red claystone interlayered between two basalt flows in Hole 432A....

(Table 1) Elemental mean values of the upper Paleocene and lower Eocene in IO...

We reconstruct the latest Paleocene and early Eocene (~57-50 Ma) environmental trends in the Arctic Ocean and focus on the Paleocene-Eocene thermal maximum (PETM) (~55 Ma),...

(Table 1) Element enrichment in dark versus light layers of the ''Zebra'' int...

Analysis focuses on the upper part of subunit 1/6, subunit 1/5, and the lower part of subunit 1/4 (cores M0002A-47X 3W to M0002A-44X 1W) extending from 203.70 to 191.99 mcd.

Chemical composition of clinoptilolite crystals from ODP Hole 108-661A (Table 2)

At ODP Site 661 from the continental margin of Northwest Africa, authigenic clinoptilolites were investigated in detail. Based on chemical data, crystal size and shape and their...

Geochemistry of black-shale cycles at Hole 159-959D

This dataset has no description

(Table 19) Chemical composition of grain size fraction <0.001 mm from sedimen...

Analyses have been carried out by S.P. Batalova and G.I. Makarova (Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences).