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(Table 1) Chemical composition and CIPW norms of basalts at DSDP Site 61-462
Analyst: H. Haramura. -
Estimating carbon contents in historical European blades through neutron diff...
Previous studies have attempted to correlate the results of metallography with neutron diffraction studies on the very high-carbon steels used in Oriental blades. Japanese sword... -
Determination of the detection limits and quantitative analysis reliability o...
Neutron diffraction offers one of the most interesting and meaningful methods for non destructive quantitative determination of the phase composition of materials. However, it... -
Compositional and microstructural analysis of iron meteorites through time of...
Iron meteorites consist overwhelmingly of nickel-iron alloys. The metal taken from these meteorites is known as meteoric iron and was one of the earliest sources of usable iron... -
(Table 1) Chemistry of olivine from ODP Hole 118-735B plutonic rocks
This dataset has no description
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(Table T5) Geochemical composition of olivine from ODP Hole 118-735B
Number of ions is calculated on the basis of 4 oxygen atoms. -
(Table 3) Representative amphibole and olivine compositions from basaltic and...
This dataset has no description
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(Table 2) Chemistry of olivine from ODP Holes 134-832B and 134-833B
Calculated on the basis of 4 O. -
(Table 3) Chemistry of olivines from ODP Holes 134-828A and 134-832A ash layers
This dataset has no description
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(Appendix E) Major element composition of olivine from ODP Leg 135 holes
This dataset has no description
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(Table 1) Major elements and CIPW norms at DSDP Hole 84-567A basalts compared...
The CIPW norms are calculated with 85% total iron as FeO and 15% as Fe2O3. -
(Table 6) Geochemistry and minerals at DSDP Leg 81 Holes
CIPW norms are calculated with 85% of total iron as FeO and 15% as Fe2O3. -
(Table 2) Geochemistry of olivine at DSDP Hole 81-555
Concentrations lower than 0.3% are not considered representative. -
(Table 1) Geochemistry and minerals at DSDP Holes 80-550B and 80-551
The CIPW norms are calculated with 85% of total iron as FeO and 15% as Fe2O3. -
(Table 1) Geochemistry and minerals in basalts at DSDP Hole 78-543A
The CIPW norms are calculated with 85% of total iron as FeO and 15% as Fe2O3. -
(Table 3) Geochemistry of olivine at DSDP Leg 73 Holes
This dataset has no description
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(Table 4) Normative mineralogy of basalts at DSDP Hole 73-519A
This dataset has no description
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(Table 6) Normative mineralogy of basalts at DSDP Hole 73-520
This dataset has no description
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(Table 13) Normative mineralogy of basalts from upper part of DSDP Hole 73-524
This dataset has no description
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(Table 8) Normative mineralogy of basalts at DSDP Hole 73-522B
This dataset has no description
