-
(Table 10) Variations in mineralogy of ultramafic rocks in ODP Hole 125-780C
X = definitely present, x = probably present, ? = possible present, - = absent. -
(Table 9) Variations in mineralogy of ultramafic rocks in ODP Hole 125-779A
X = definitely present, x = probably present, ? = possible present, - = absent. -
(Table 8) Variations in mineralogy of ultramafic rocks in ODP Hole 125-778A
X = definitely present, x = probably present, ? = possible present, - = absent. -
(Table 7) Mineralogy results of group 3 ODP Leg 125 samples
Group 3 = 90 % secondary minerals. X = definitely present, x = probably present, ? = possible present, - = absent. -
(Table 6) Mineralogy results of group 2 ODP Leg 125 samples
Group 2 = 45-89 % secondary minerals. X = definitely present, x = probably present, ? = possible present, - = absent. -
(Table 5) Mineralogy results of group 1 samples of ODP Hole 125-779A
Group 1 = <45 % secondary minerals. X = definitely present, x = probably present, ? = possible present, - = absent. -
(Table 4) Reconstructed primary mineralogy, composition, and mass change duri...
For the modal data, 1000 points have been counted in the thin sections on a 0.2x0.2 mm grid. The modal data are given in vol. %. Modal proportions of primary minerals are given... -
Heavy mineral composition of 0.100-0.050 mm size fraction of sediments and se...
This dataset has no description
-
Heavy mineral composition of 0.100-0.050 mm size fraction of sediments and se...
Method used - binocular counting -
Mineralogy of serpentine muds of ODP Leg 125 holes (Table 1)
Large serpentinite seamounts are common in the forearc regions between the trench axis and the active volcanic fronts of the Mariana and Izu-Bonin intraoceanic arcs. The... -
High resolution INS spectra of hydrocarbonaceous overlayers formed on novel m...
For the first time, the research team aim to use INS to characterise a series of new high specification methane reforming catalysts. The enhanced performance of these catalysts... -
The application of INS to investigate the active phase of methane steam refor...
A previous allocation of beamtime on MAPS [RB720354] revealed the vibrational fingerprint of methane reforming catalysts operating under so-called ¿dry¿ reforming conditions.... -
Analysing intermediates of a CO2 insertion reaction using simultaneous operan...
Atmospheric levels of CO2 are increasing at uncontrolled levels and as such methods of CO2 utilisation are being researched. A key reaction for this purpose is the coupling of... -
Quantification of Brønsted acid site densities in zeolites: an INS investigation
As part of an on-going industrial/academic collaboration in to the application of neutron spectroscopy to probe commercially relevant zeolites, this proposal seeks to use the... -
Local structure and proton sites in proton conducting brownmillerites
This proposal requests 3 days on Maps to investigate the nature of local structure and proton sites in the proton conducting brownmillerite system Ba2In1.85M0.15O6H2 (M = In,... -
The application of INS to examine high specification Fe Fischer-Tropsch catal...
Over the last 4-5 years the research team have been developing INS methodology that can be applied to investigate Fe Fischer-Tropsch (F-T) catalysts. The first stage of that... -
Analysing intermediates of a CO2 insertion reaction using simultaneous operan...
Atmospheric levels of CO2 are increasing at uncontrolled levels and as such methods of CO2 utilisation are being researched. A key reaction for this purpose is the coupling of... -
Mineral chemistry data from batch experiments simulating hydrothermal troctol...
1XMg = Mg / (Mg + Fe)2XCa = Ca / (Ca + Na) *Initial characterization of the reactants -
Modes calculated on a Cr and spinel-free basis of Hole CM2B
This dataset has no description
