-
(Fig. 6) Distribution of detrital minerals, authigenic minerals, and biogenic...
A = abundant (>30 %), C = common, (15-30 %), F = few (3-15 %), R = rare (<3 %), - = absent -
(Table 3) Distribution of detrital minerals, authigenic minerals, and biogeni...
A = abundant (>30 %), C = common, (15-30 %), F = few (3-15 %), R = rare (<3 %), - = absent. Core 107-652A-36R Subunit IVb, 14 pebbles. -
(Table 2) Distribution of detrital minerals, authigenic minerals, and biogeni...
A = abundant (>30 %), C = common, (15-30 %), F = few (3-15 %), R = rare (<3 %), - = absent -
(Table 1) Distribution of detrital minerals, authigenic minerals, and biogeni...
A = abundant (>30 %), C = common, (15-30 %), F = few (3-15 %), R = rare (<3 %), - = absent -
Geochemical and isotope data from shallow aquifers in the Bas-Saint-Laurent a...
In this study, we combined radon in water activity (222Rn), stable isotopes of inorganic carbon (δ13CDIC), water stable isotopes (δ18O; δ2H) as well as major and trace ions... -
Pore water saturation index at Hole 310-M0025A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0022A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0019A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0014A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0013A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0012A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0010A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0009B
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0009A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0008A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0007B
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0006A
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0005E
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0005D
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base... -
Pore water saturation index at Hole 310-M0005C
Calculated for pE = 4 and T = 28 °C from pore water chemistry data with PHREEQCI version 2.12.5 using the PHREEQC.DAT thermodynamic data base...
