-
(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. -
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...
