API src

Found 11 results.

Major composition (wt.%) of concretions, ICP-AES measurements

In order to get a complete geochemical signature, 14 P-rich concretions, chosen among the different cores, were acid digested (Table 3a and Table 3b). In a clean laboratory, 1.7 to 36 mg of concretions were digested overnight in a concentrated mixture of Suprapur acid (3 ml HCl/2 ml HNO3/1 ml HF) at 90 °C in sealed Teflon beakers. After evaporation to dryness, the residue was dissolved in 2.5 ml of 2% HNO3 Suprapur and diluted to 12 ml with Milli-Q water. During the same procedure, we have also dissolved and analysed, for comparison, a pure vivianite from Anlua, Cameroon (tubular crystals, MRAC collection).

Geochemical Analysis of Cations of Mud Samples of the KTB Main Hole HB1g.

Geochemical Analysis of Cations of Mud Samples of the KTB Main Hole HB1a.

Geochemical Analysis of Cations of Mud Samples of the KTB Main Hole HB1h.

Geochemical Analysis of Cations of Mud Samples of the KTB Pilot Hole VB1b.

Geochemical Analysis of Cations of Mud Samples of the KTB Pilot Hole VB1.

Geochemical Analysis of Cations of Mud Samples of the KTB Pilot Hole VB1a.

Geochemical Analysis of Cations of Mud Samples of the KTB Main Hole HB1d.

Geochemical Analysis of Cations of Mud Samples of the KTB Main Hole HB1.

Geochemical Analysis of Cations of Mud Samples of the KTB Main Hole HB1i

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