Table 1 Results of least-squared mass balance calculations.
From: Gravity modeling finds a large magma body in the deep crust below the Gulf of Naples, Italy
Transition from shoshonitic basalt to trachy-basalt (step 1) | |||||
|---|---|---|---|---|---|
Sample | APR 22 | APR 19 | |||
Composition | Shoshonitic basalt parent magma measured wt.% | Trachy-basalt daughter magma measured wt.% | Difference between parent and daughter magmas: | ||
observed | calculated | obs.-calc. (residuals) | |||
SiO2 | 46.22 | 49.04 | 1.43 | 1.31 | 0.12 |
TiO2 | 1.20 | 1.28 | 0.04 | 0.25 | −0.21 |
Al2O3 | 15.05 | 17.19 | 1.68 | 1.70 | −0.02 |
Fe2O3tot | 8.72 | 8.68 | −0.31 | −0.23 | −0.08 |
MnO | 0.14 | 0.14 | 0.00 | −0.40 | 0.40 |
MgO | 9.71 | 6.33 | −3.68 | −3.66 | −0.02 |
CaO | 11.46 | 11.37 | −0.44 | −0.33 | −0.11 |
Na2O | 2.80 | 3.10 | 0.22 | 0.63 | −0.41 |
K2O | 1.45 | 2.44 | 0.95 | 0.60 | 0.35 |
P2O5 | 0.31 | 0.43 | 0.11 | 0.11 | 0.00 |
H2O | 2.49 | ||||
CO2 | 0.46 | ||||
Total | 100.01 | 100.01 | |||
Sum of the squares of residuals | 0.52 | ||||
Subtracted minerals | Amounts relative to initial magma vol.% | Absolute amounts vol.% | |||
Clinopyroxene (Wo47En46) | 10.72 | 41.38 | |||
Olivine (Fo89) | 7.44 | 28.72 | |||
Plagioclase (An72Ab25) | 5.55 | 21.44 | |||
Cr-spinel (Cr# 0.53) | 2.19 | 8.46 | |||
Total relative to initial magma | 25.90 | 100.00 | |||
Transition from trachy-basalt to shoshonite (step 2) | |||||
Sample | APR 19 | 97 119 21a | |||
Composition | Trachy-basalt parent magma measured wt.% | Shoshonite daughter magma measured wt.% | Difference between parent and daughter magmas | ||
observed | calculated | obs.-calc. (residuals) | |||
SiO2 | 49.04 | 49.69 | 2.35 | 1.92 | 0.42 |
TiO2 | 1.28 | 0.82 | −0.43 | −0.03 | −0.40 |
Al2O3 | 17.19 | 15.80 | −0.85 | −0.97 | 0.12 |
Fe2O3tot | 8.68 | 7.91 | −0.50 | −0.82 | 0.32 |
MnO | 0.14 | 0.13 | −0.01 | −0.33 | 0.32 |
MgO | 6.33 | 5.53 | −0.61 | −0.69 | 0.08 |
CaO | 11.37 | 10.40 | −0.61 | −0.63 | 0.02 |
Na2O | 3.10 | 2.09 | −0.94 | −0.49 | −0.45 |
K2O | 2.44 | 3.79 | 1.49 | 1.74 | −0.25 |
P2O5 | 0.43 | 0.52 | 0.12 | 0.29 | −0.17 |
H2O | 3.27 | ||||
CO2 | 0.30 | ||||
Total | 100.01 | 100.25 | |||
Sum of the squares of residuals | 0.86 | ||||
Subtracted minerals | Amounts relative to initial magma vol.% | Absolute amounts vol.% | |||
Plagioclase (An46Ab47) | 29.77 | 56.02 | |||
Clinopyroxene (Wo48En41) | 15.41 | 28.98 | |||
Olivine (Fo89) | 3.22 | 6.06 | |||
Ti-magnetite (Usp27) | 3.15 | 5.92 | |||
Cr-spinel (Cr# 0.53) | 1.61 | 3.02 | |||
Total relative to initial magma | 53.16 | 100.00 | |||
Transition from shoshonite to latite (step 3) | |||||
Sample | 97 119 21a | 97 101 FRb | |||
Composition | Shoshonite parent magma measured wt.% | Latite daughter magma measured wt.% | Difference between parent and daughter magmas | ||
observed | calculated | obs.-calc. (residuals) | |||
SiO2 | 49.69 | 53.05 | 4.00 | 4.11 | −0.11 |
TiO2 | 0.82 | 0.75 | −0.07 | −0.08 | 0.01 |
Al2O3 | 15.80 | 17.42 | 1.84 | 1.87 | −0.03 |
Fe2O3tot | 7.91 | 7.01 | −0.86 | −0.79 | −0.07 |
MnO | 0.13 | 0.12 | 0.00 | −0.04 | 0.04 |
MgO | 5.53 | 2.19 | −3.43 | −3.43 | 0.00 |
CaO | 10.40 | 5.26 | −5.27 | −5.28 | 0.01 |
Na2O | 2.09 | 4.03 | 2.05 | 1.87 | 0.18 |
K2O | 3.79 | 5.45 | 1.76 | 1.65 | 0.11 |
P2O5 | 0.52 | 0.50 | −0.03 | 0.12 | −0.15 |
H2O | 3.27 | 4.00 | |||
CO2 | 0.30 | 0.20 | |||
Total | 100.25 | 99.99 | |||
Sum of the squares of residuals | 0.08 | ||||
Subtracted minerals | Amounts relative to initial magma vol.% | Absolute amounts vol.% | |||
Clinopyroxene (Wo48En41) | 25.95 | 41.95 | |||
Plagioclase (An72Ab25) | 17.32 | 27.99 | |||
Alkali-feldspar (Or86Ab13) | 12.16 | 19.66 | |||
Ti-magnetite (Usp27) | 3.07 | 4.96 | |||
Olivine (Fo80) | 2.88 | 4.66 | |||
Apatite | 0.48 | 0.78 | |||
Total relative to initial magma | 61.86 | 100.00 | |||
Transition from latite to trachyte (step 4) | |||||
Sample | 97 101 FRb | SsB2 | |||
Composition | Latite parent magma measured wt.% | Trachyte daughter magma measured wt.% | Difference between parent and daughter magmas | ||
observed | calculated | obs.-calc. (residuals) | |||
SiO2 | 53.05 | 56.75 | 4.66 | 4.66 | 0.00 |
TiO2 | 0.75 | 0.42 | −0.33 | −0.49 | 0.16 |
Al2O3 | 17.42 | 17.58 | 0.42 | 0.41 | 0.01 |
Fe2O3tot | 7.01 | 4.40 | −2.66 | −2.64 | −0.02 |
MnO | 0.12 | 0.12 | 0.00 | −0.03 | 0.03 |
MgO | 2.19 | 0.57 | −1.69 | −1.64 | −0.05 |
CaO | 5.26 | 2.56 | −2.78 | −2.79 | 0.01 |
Na2O | 4.03 | 4.01 | 0.03 | 0.12 | −0.09 |
K2O | 5.45 | 7.97 | 2.74 | 2.75 | −0.01 |
P2O5 | 0.50 | 0.13 | −0.38 | −0.35 | −0.03 |
H2O | 4.00 | 5.00 | |||
CO2 | 0.20 | 0.05 | |||
Total | 99.99 | 99.56 | |||
Sum of the squares of residuals | 0.04 | ||||
Subtracted minerals | Amounts relative to initial magma vol.% | Absolute amounts vol.% | |||
Plagioclase (An32Ab56) | 25.45 | 41.64 | |||
Alkali-feldspar (Or51Ab44) | 16.92 | 27.68 | |||
Clinopyroxene (Wo48En41) | 8.75 | 14.32 | |||
Ti-magnetite (Usp27) | 4.65 | 7.61 | |||
Biotite | 4.31 | 7.06 | |||
Apatite | 1.04 | 1.69 | |||
Total relative to initial magma | 61.12 | 100.00 | |||