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(Table 94) Mineral and chemical compositions of surficial sulfide deposits of...
Mineral contents of crystal phase. -
(Table 93) Mineral and chemical compositions of deposits from a hydrothermal ...
Mineral contents are given in % of crystal phase. -
(Appendix 4) Mineral content from different oceanographic settings
This dataset has no description
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Isotopic data of pyrite (δ34S) and barite (δ34S, δ18O) in the Canol Formation...
The stable isotopic composition of pyrite (δ34Spyrite) and barite (δ34Sbarite, δ18Obarite) in marine sedimentary rocks provides a valuable archive for reconstructing the... -
Heavy mineral composition of 0.100-0.050 mm size fraction of sediments from H...
Method used - binocular counting -
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-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-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-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-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-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-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-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-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-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-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... -
Mineral quantification of a Jordan Cretaceous outcrop (Section GM3, Ghawr Al ...
Cyclic fluctuations in global sea level during epochs of warm greenhouse climate have remained enigmatic, because absence or subordinate presence of polar ice during these... -
Heavy mineral composition of 0.100-0.050 mm size fraction of sediments from H...
Method used - binocular counting -
Heavy mineral composition of 0.100-0.050 mm size fraction of sedimentary rock...
Method used - binocular counting -
Heavy mineral composition of 0.100-0.050 mm grain size fraction of sediments ...
Method used - binocular counting
