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(Table 1) Mineralogical assemblages of the clay fraction (<2 µm) of altered f...
This dataset has no description
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(Table 1) Modal abundances of primary and secondary phases in thin sections o...
This dataset has no description
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(Table 1) Mineral composition of clay fractions and bulk rocks, and δ¹⁸O, d2H...
Mineral contents are approximate -
(Table 1) Mineralogical assemblages of unaltered, altered and hydrothermal se...
x = very abundant, a = abundant, f = small quantity, * = allietit - talc-smectite mixed layer. -
X-ray diffraction results from IODP Hole 357-M0076B
= poor data quality. Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized... -
X-ray diffraction results from IODP Hole 357-M0075B
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
X-ray diffraction results from IODP Hole 357-M0075A
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
X-ray diffraction results from IODP Hole 357-M0072B
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
X-ray diffraction results from IODP Hole 357-M0071B
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
X-ray diffraction results from IODP Hole 357-M0071A
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
X-ray diffraction results from IODP Hole 357-M0069A
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
X-ray diffraction results from IODP Hole 357-M0068B
= poor data quality, ** = duplicate sample. Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or... -
X-ray diffraction results from IODP Hole 357-M0068A
Percentages were released by the software, sometimes with excess. Total sum <100% likely reflects the presence of amorphous or poorly crystallized material. -
(Table 1) Mineralogy of veins in basalts at DSDP Hole 61-462A
Numerous veins are present in basalts recovered from Hole 462A, Leg 61 of the Deep Sea Drilling Project. Three mineral assemblages are recognized and stratigraphically... -
(Table 1) Mineralogy of DSDP Leg 65 sediments
During Leg 65, four sites were drilled near the mouth of the Gulf of California where high sedimentation rates made it possible to sample young oceanic crust near the ridge... -
(Table 1) Bulk and clay mineralogy at DSDP Leg 66 Holes
During Leg 66 eight sites on an active margin transect off southern Mexico were drilled in order to determine the nature of ocean-continent transition across a subduction zone.... -
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... -
(Table 1) Rock type and summary of alteration after component minerals in thi...
This dataset has no description
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Methane hydrate formation in the presence of surfactant
In this proposal we wish to study in situ formation of methane hydrates in surfactant solutions. The broad aim of this research is to enable us to understand how we can... -
The use of INS to investigate reactions relevant to Fischer-Tropsch catalysis
In collaboration with an industrial partner, the PI is seeking to use INS to help characterise a series of catalysts active for the important Fischer-Tropsch (F-T) process. As...
