Mean MORB and Bulk
Mantle compositions
The Mean MORB compositions were calculated from ~5000 glass analyses
downloaded from the PetDB data base (thanks to K. Lehnert for her help). Oxides in percent and traces in ppm. The data are first corrected to 8
percent MgO by plotting log Ci vs
[MgO]. I provide an arithmetic mean (normal
distribution), a geometric mean (log-normal distribution) and a mode (most
frequent value) for each histogram. 2s stands for the relative uncertainty on
the geometric mean at the 95 percent confidence level.
|
Element1 |
data # |
rMgO2 |
arith. |
geom. |
2s (rel)5 |
Mode 6 |
HOF887 |
SUN898 |
|
|
|
|
mean3 |
mean4 |
|
|
|
|
|
|
|
|
|
recom. |
|
|
|
|
|
SiO2
|
4838 |
-0.51 |
50.89 |
50.89 |
0.001 |
51.04 |
50.45 |
|
|
TiO2
|
4832 |
-0.76 |
1.73 |
1.73 |
0.017 |
1.84 |
1.615 |
|
|
Al2O3
|
4832 |
0.53 |
14.47 |
14.47 |
0.004 |
14.69 |
15.255 |
|
|
FeOT |
4143 |
-0.69 |
10.8 |
10.8 |
0.007 |
10.14 |
10.426 |
|
|
MgO |
4876 |
|
8 |
8 |
|
8 |
7.576 |
|
|
CaO |
4832 |
0.7 |
10.95 |
10.95 |
0.005 |
11.41 |
11.303 |
|
|
Na2O
|
4828 |
-0.55 |
2.78 |
2.78 |
0.007 |
2.91 |
2.526 |
|
|
K2O |
4793 |
-0.56 |
0.16 |
0.16 |
0.047 |
0.17 |
|
|
|
|
|
|
|
|
|
|
|
|
|
87Sr/86Sr
|
540 |
0.01 |
0.70279 |
0.70279 |
0.00006 |
0.70303 |
|
|
|
143Nd/144Nd |
424 |
0.01 |
0.51307 |
0.51307 |
0.00002 |
0.51323 |
|
|
|
eps(Nd) |
|
|
8.5 |
8.4 |
|
11.5 |
|
|
|
206Pb/204Pb |
421 |
-0.16 |
18.458 |
18.459 |
0.002 |
18.38 |
|
|
|
207Pb/204Pb |
421 |
-0.1 |
15.518 |
15.518 |
0.0003 |
15.496 |
|
|
|
208Pb/204Pb |
421 |
-0.11 |
38.092 |
38.093 |
0.001 |
38.187 |
|
|
|
(3He/4He)A |
180 |
0.2 |
8.1 |
8.1 |
0.047 |
7.7 |
|
|
|
|
|
|
|
|
|
|
|
|
|
U |
538 |
-0.39 |
0.333 |
0.138 |
0.112 |
0.233 |
0.0711 |
|
|
Rb |
661 |
-0.43 |
3.9 |
2.83 |
0.116 |
2.98 |
1.262 |
0.56 |
|
K |
4798 |
-0.56 |
1465 |
1328 |
0.026 |
1375 |
883.7 |
|
|
Th |
615 |
-0.44 |
0.508 |
0.383 |
0.115 |
0.363 |
0.1871 |
0.12 |
|
Pb |
406 |
-0.26 |
2.57 |
0.657 |
0.075 |
0.662 |
0.489 |
0.3 |
|
Ba |
925 |
-0.37 |
42.7 |
25.9 |
0.093 |
14.4 |
13.87 |
6.3 |
|
Sr |
1218 |
-0.13 |
133 |
126 |
0.017 |
115 |
113.2 |
90 |
|
La |
826 |
-0.57 |
5.87 |
5.35 |
0.065 |
4.09 |
3.895 |
2.5 |
|
Ce |
816 |
-0.77 |
15.9 |
15.6 |
0.056 |
12.8 |
12 |
7.5 |
|
Nd |
840 |
-0.82 |
12.3 |
12.3 |
0.042 |
10.8 |
11.18 |
7.3 |
|
Sm |
987 |
-0.8 |
3.9 |
3.94 |
0.031 |
3.67 |
3.752 |
2.63 |
|
Eu |
805 |
-0.86 |
1.39 |
1.42 |
0.028 |
1.35 |
1.335 |
1.02 |
|
Gd |
563 |
-0.8 |
5.07 |
4.99 |
0.029 |
4.73 |
5.08 |
3.68 |
|
Dy |
595 |
-0.8 |
5.84 |
5.7 |
0.031 |
5.18 |
6.304 |
4.55 |
|
Y |
1049 |
-0.69 |
35.7 |
36.1 |
0.023 |
32.6 |
35.82 |
28 |
|
Er |
590 |
-0.74 |
3.6 |
3.46 |
0.032 |
3.14 |
4.143 |
2.97 |
|
Yb |
795 |
-0.71 |
3.53 |
3.44 |
0.028 |
3.13 |
3.9 |
3.05 |
|
Lu |
378 |
-0.78 |
0.552 |
0.556 |
0.05 |
0.495 |
0.589 |
0.46 |
|
P |
4533 |
-0.68 |
753 |
783 |
0.016 |
860 |
|
510 |
|
Zr |
1182 |
-0.77 |
116 |
118 |
0.031 |
119 |
104.24 |
74 |
|
Hf |
298 |
-0.84 |
3.41 |
3.54 |
0.086 |
2.88 |
2.974 |
2.05 |
|
Ta |
478 |
-0.53 |
0.428 |
0.368 |
0.113 |
0.277 |
0.192 |
0.13 |
|
Nb |
778 |
-0.52 |
6 |
4.89 |
0.088 |
6.98 |
3.507 |
2.33 |
|
Co |
353 |
0.24 |
43.2 |
42.2 |
0.01 |
43.8 |
47.07 |
|
|
Cr |
799 |
0.78 |
253 |
191 |
0.07 |
255 |
|
|
|
Cu |
517 |
0.38 |
73.7 |
68 |
0.016 |
66.8 |
74.4 |
|
|
Ni |
945 |
0.83 |
91.8 |
74.8 |
0.04 |
77.4 |
149.5 |
|
|
Sc |
841 |
0.12 |
40.6 |
40 |
0.007 |
41.4 |
41.37 |
|
|
Zn |
522 |
-0.55 |
92.1 |
93.1 |
0.025 |
89.7 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
1
major elements in percent, trace elements in ppm |
|
|
|
|
||||
|
2
correlation coefficient between concentration or ratio and ln [MgO] |
|
|
||||||
|
3
arithmetic mean (normal density) |
|
|
|
|
|
|||
|
4
geometric mean (log-normal density) |
|
|
|
|
|
|||
|
5
2 standard deviation / (geom. mean sqrt(n)) |
|
|
|
|
||||
|
6
2nd derivative of the 4th-degree best-fit polynomial through the
cumulated distribution between 10 and 90 percent is set to zero |
||||||||
|
7
N-MORB Hofmann (1988) EPSL 90, 297-314. |
|
|
|
|
||||
|
8 N-MORB Sun and McDonough (1989) Geol. Soc.
Spec. Pub. 42, 313-345 |
|
|
||||||
The Bulk Mantle concentrations (ppm) are calculated by subtracting Continental
Crust from the Bulk Silicate Earth. Continental Crust
compositions from Rudnick and Fountain (1995) and from Taylor and McLennan
(1995). Bulk Silicate Earth composition from Sun and
McDonough (1989).
|
Element |
mean
mantle composition |
|
|
(ppm) |
RFa |
TM b |
|
|
|
|
|
U |
0.00988 |
0.0137 |
|
Rb |
0.174 |
0.367 |
|
K |
125 |
174 |
|
Th |
0.0385 |
0.0541 |
|
Pb |
0.0576 |
0.0917 |
|
Ba |
3.75 |
4.79 |
|
Sr |
17.6 |
18.1 |
|
La |
0.519 |
0.534 |
|
Ce |
1.38 |
1.44 |
|
Nd |
1.11 |
1.14 |
|
Sm |
0.38 |
0.383 |
|
Eu |
0.146 |
0.147 |
|
Gd |
0.521 |
0.524 |
|
Dy |
0.653 |
0.652 |
|
Y |
4.19 |
4.19 |
|
Er |
0.425 |
0.425 |
|
Yb |
0.429 |
0.427 |
|
Lu |
0.0656 |
0.0658 |
|
P |
84.2 |
|
|
Zr |
9.63 |
9.8 |
|
Hf |
0.258 |
0.263 |
|
Ta |
0.0293 |
0.0301 |
|
Nb |
0.573 |
0.581 |
|
Co |
106 |
106 |
|
Cr |
2644 |
2643 |
|
Cu |
30 |
29.7 |
|
Ni |
1974 |
1974 |
|
Sc |
16.2 |
16.1 |
|
Zn |
54.9 |
54.8 |
|
Continental
crust composition from |
||
|
(a)
Rudnick and Fountain (1995) Rev. Geophys., 33,
267-309. |
||
|
(b)
Taylor and McLennan (1995) Rev. Geophys., 33,
241-265. |
||
Details and histograms in:
Albarède, F. (2005). The survival of mantle geochemical
heterogeneities. In Earth's Deep
Mantle: Structure, Composition, and Evolution. Geophys. Monogr. R. D. van der Hilst, J. Bass, J. Matas and J. Trampert.