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Mineralogy of Bakken Petroleum System cores
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(Table 3) Occurrence of secondary minerals in in veins and vesicles of basalt...
Sediment depth is given in mbsf. P = present; ? = uncertanty. -
(Table T4) Mineralogical assemblages of the clay fraction of ODP Site 180-110...
Sediment depth is given in mbsf. Abundance estimate as follows: xxx = abundant, xx = common, x = rare, t = trace. (P) = including feldspar. -
(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. -
(Table 6) Geochemistry of spinels and ilmenite from ODP Holes 107-651A
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(Table 3) Geochemistry of clinopyroxenes from ODP Holes 107-651A and 107-655B
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(Table 28) Minerals from veins in basalts of the Costa Rica Rift
X - mixed-layer chlorite-montmorillonite mineral; X* - analysis of thomsonite has been obtained from N.N. Pertsev. -
(Fig. 7) Distribution of secondary minerals in basalts of the Costa Rica Rift...
This dataset has no description
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Carbonate stable and clumped isotope data, calculated carbonate formation tem...
Carbonate was micro-sampled from representative listvenite and serpentinite core sections of Hole BT1B for carbonate stable isotope analysis (δ13C, δ18O) and clumped isotope... -
Abundance of minerals in the rocks of the post impact formations from IODP Ho...
This dataset has no description
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(Table 1) Peak intensities and stable carbon and oxygen isotope ratios of var...
Abundant and various diagenetic carbonates were recovered from a 1084-m-thick, Quaternary to lower Miocene section at ODP Site 799 in the Japan Sea. Petrographic, XRD, SEM,...
