Table 7. Leg 152 dacites and comparisons.
| Granophyre | Gneiss | Exp. melt | Exp. melt | Exp. melt | |||||
|---|---|---|---|---|---|---|---|---|---|
Unit 47* |
Unit 55* |
Rockall |
Vøring |
CL87-52E** |
324721 |
1000ēC 0.1 GPa |
1000ēC 0.3 GPa*** |
925ēC 0.3 GPa |
|
SiO2 |
60.50 |
64.89 |
64.52 |
63.78 |
74.85 |
63.26 |
64.21 |
60.77 |
75.90 |
TiO2 |
0.99 |
0.74 |
0.90 |
1.38 |
0.34 |
0.78 |
0.28 |
1.53 |
0.32 |
Al2O3 |
14.86 |
13.32 |
16.08 |
16.85 |
12.30 |
17.25 |
16.46 |
14.07 |
13.04 |
FeO |
7.07 |
5.19 |
6.03 |
5.21 |
1.96 |
2.11 |
5.56 |
9.58 |
1.27 |
MnO |
0.14 |
0.14 |
0.14 |
0.06 |
0.03 |
0.06 |
0.22 |
0.37 |
0.03 |
MgO |
2.67 |
3.04 |
1.53 |
0.62 |
0.59 |
1.60 |
2.13 |
3.08 |
0.37 |
CaO |
4.78 |
4.42 |
2.22 |
4.64 |
1.07 |
3.30 |
3.99 |
6.35 |
0.64 |
Na2O |
4.21 |
3.62 |
2.12 |
2.35 |
3.53 |
3.99 |
4.88 |
2.41 |
2.07 |
K2O |
1.57 |
2.99 |
2.57 |
1.38 |
4.34 |
3.94 |
1.27 |
0.88 |
6.36 |
P2O5 |
0.27 |
0.07 |
0.16 |
0.61 |
0.07 |
0.30 |
0.96 |
||
Total |
97.06 |
98.44 |
96.27 |
96.88 |
99.08 |
96.59 |
100.00 |
100.00 |
100.00 |
Notes: * = Site 917 dacite from Fitton et al. (1998b). Unit 47 = Sample 152-917A-32R-4, 76-60 cm. Unit 55 = Sample 152-917A-51R-1, 42-45 cm. = Dacite from the Rockall trough, well 163/6-1A (Morton et al.,1988, table 4, analysis C7.1). = Dacite from the lower series at Site 642 on the Vøring Plateau (Parson et al., 1989, table 1, analysis of flow F112). ** = Granophyre component in the hybridized zone of the saddle part of the Miki Fjord macrodike (Blichert-Toft et al., 1992). = Agmatitic gneiss from the late Archean Skjoldungen alkaline igneous province, SE Greenland (Blichert-Toft et al., 1995). = Experimental melt in dehydration melting of basalt at 0.1 GPa and 1000ēC (Beard and Lofgren, 1991). *** = Experimental melt in dehydration melting of basalt at 0.3 GPa and 1000ēC (Beard and Lofgren, 1991). = Experimental melt in dehydration melting of biotite gneiss at 0.3 GPa and 925 ēC (Patiņo Douce and Beard, 1995). Iron = total FeO. The experimental melts are calculated anhydrous to 100%.