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(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. -
Abundance of minerals in the rocks of the upper peak ring from IODP Hole 364-...
This dataset has no description
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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-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. -
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...
