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(Fig. 7) Distribution of secondary minerals in basalts of the Costa Rica Rift...
This dataset has no description
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Mineral composition of sedimentary rocks from Hole VNIIO-1971-01-Rad drilled ...
This dataset has no description
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Light mineral composition of 0.100-0.050 mm and 0.250-0.100 mm size fractions...
Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.626564Method used - binocular counting -
Heavy mineral composition of 0.100-0.050 mm size fraction of sediments and se...
This dataset has no description
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Heavy mineral composition of 0.100-0.050 mm size fraction of sediments and se...
Method used - binocular counting -
Mineral composition of hydrothermal chimneys sampled with ROV during Pourquoi...
Hydrothermal chimneys were collected by a ROV in 2016 from the Kairei and Pelagia vent fields along the Indian Ridge. Major element compositions of the chimney samples were... -
Abundance of minerals in the rocks of the upper peak ring from IODP Hole 364-...
This dataset has no description
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(Supplement) Groundwater quality in Lahore Pakistan: emphasis on Arsenic and ...
The dataset provides detailed information on the study that was conducted in Lahore's 7 major towns. The sample was taken from 472 tubewells and analyzed for major cations and... -
(Table T1) Physical properties of minicores from ODP Leg 193 sites, PACMANUS ...
Permeability of the ocean crust is one of the most crucial parameters for constraining submarine fluid flow systems. Active hydrothermal fields are dynamic areas where fluid... -
Heavy mineral content of ODP Leg 107 holes
Analyses of rock clasts and of heavy minerals in upper Miocene coarse detrital units drilled along the East Sardinia passive-type continental margin (Sites 654, 653, 652, and... -
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...