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(Table 5) Heavy metal contents and geochemical characteristics in Cretaceous ...
This dataset has no description
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(Table 4) Chemical composition of Cretaceous volcanoclastic rocks from DSDP H...
This dataset has no description
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(Table 85) Trace element contents in basalts of the Nauru Basin at DSDP Site ...
Analyses have been carried out by T.V. Sverkunova and T.K. Babova in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 82) Chemical composition of basalts from the Nauru Basin at DSDP Site ...
Analyses have been carried out by S.P. Batalova and L.V. Shkodyuk (samples marked by *) in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of... -
(Table 81) Chemical composition of vein celadonite from basalts of the Nauru ...
Analyses have been carried out by I. Romanenko in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 80) Chemical composition of vein Fe-hydroxides from basalts of the Nau...
Analyses have been carried out by I. Romanenko in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 79) Chemical composition of apophyllite from basalts of the Nauru Basi...
Analyses have been carried out by T.N. Bortina and I. Romanenko in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 78) Chemical composition of okenite from basalts of the Nauru Basin, D...
Analyses have been carried out by T.N. Bortina and I. Romanenko in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 77) Chemical composition of heulandite from basalts of the Nauru Basin...
Analyses have been carried out by I. Romanenko in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 74) Parameter b of clay minerals from veins and pore fillings of basal...
Analyses have been carried out by T.N. Vortina in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 72) Chemical composition of size fraction <0.002 mm from basalts of th...
Analyses have been carried out by T.N. Vortina in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 76) Trace element contents in vein clay minerals from basalts of the N...
Analyses have been carried out by T.V. Sverkunova in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 75) Chemical composition of vein smectites from basalts of the Nauru B...
Analyses have been carried out by T.N. Vortina and I. Romanenko in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. Empty cells =... -
(Table 73) Vein minerals from basalts of the Nauru Basin, DSDP Site 61-462
This dataset has no description
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(Table 71) Parameter b of clay minerals from the main basalt mass of the Naur...
Analyses have been carried out by N.Yu. Tseitlin in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. -
(Table 70) Secondary minerals from the main basalt mass of the Nauru Basin, D...
In the samples marked (a) secondary minerals have been studied in size fractions <0.002 mm, 0.002-0.02 mm, >0.02 mm and non-fractionated. -
(Table 34) Chemical composition of basalt glasses, DSDP Holes 61-462A and 70-...
Analyses have been carried out by T.Gulyaeva and S.P. Batalova in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. In samples II... -
(Table 77) Distribution of trace elements in <0.002 mm grain size fraction fr...
Type II - semiordered alternation of smectite layers, according to J. Mering. -
(Table 76) Distribution of trace elements in <0.002 mm grain size fraction fr...
Type II - semiordered alternation of smectite layers, according to J. Mering. -
(Table 75) Chemical composition of <0.002 mm grain size fraction from volcano...
Type II - semiordered alternation of smectite layers, according to J. Mering.