Table 2 Parameters used for Fe-Mg diffusion modeling on olivine crystals with estimation of timescales and their relative uncertainties.

From: Violent paroxysmal activity drives self-feeding magma replenishment at Mt. Etna

Date

Crystal

T (°C)

P (MPa)

fO2 (bar)

Mi

Δt ± σ

Feb-28

ol4_28/02/17

1108

140

10−9.28

M1b-M1a (r)

209 ± 64

ol7_28/02/17

1084

30

10−9.65

M2-M1a (r)

256 ± 81

ol8_28/02/17

1084

30

10−9.65

M2-M1a (r)

282 ± 89

Mar-19

ol3_19/03/17

1131

260

10−8.92

M1a-M2 (n)

14 ± 4

ol12_19/03/17

1108

140

10−9.28

M1b-M1a (r)

98 ± 30

Mar-25

ol1_25/03/17

1108

140

10−9.28

M1b-M1a (r)

30 ± 9

 

1108

140

10−9.28

M1b-M2 (n)

5 ± 2

ol3_25/03/17

1084

30

10−9.65

M2-M1a (r)

23 ± 7

ol4_25/03/17

1084

30

10−9.65

M2-M1a (r)

44 ± 14

ol6_25/03/17

1084

30

10−9.65

M2-M1a (r)

34 ± 11

ol10_25/03/17

1108

140

10−9.28

M1b-M1a (r)

36 ± 11

 

1108

140

10−9.28

M1a-M2 (n)

2 ± 1

ol12_25/03/17

1108

140

10−9.28

M1b-M1a (r)

34 ± 10

ol13_25/03/17

1164

390

10−8.49

M0-M1b (n)

8 ± 2

Apr-11

ol1_11/04/17

1084

30

10−9.65

M2-M1a (r)

34 ± 12

ol2_11/04/17

1084

30

10−9.65

M2-M1a (r)

26 ± 8

 

1084

30

10−9.65

M1a-M2 (n)

14 ± 4

ol4_11/04/17

1084

30

10−9.65

M2-M1a (r)

38 ± 12

ol5_11/04/17

1164

390

10−8.49

M0-M1a (n)

8 ± 2

ol7_11/04/17

1084

30

10−9.65

M2-M1a (r)

30 ± 10

ol9_11/04/17

1084

30

10−9.65

M2-M1a (r)

24 ± 8

 

1084

30

10−9.65

M2-M1a (r)

11 ± 4

ol10_11/04/17

1084

30

10−9.65

M2-M1a (r)

34 ± 7

ol11_11/04/17

1084

30

10−9.65

M2-M1a (r)

34 ± 11

Apr-19

ol1_19/04/17

1084

30

10−9.65

M2-M1a (r)

53 ± 17

ol2_19/04/17

1084

30

10−9.65

M2-M1a (r)

45 ± 14

ol3_19/04/17

1108

140

10−9.28

M1b-M1a (r)

45 ± 14

ol4_19/04/17

1084

30

10−9.65

M2-M1a (r)

60 ± 19

ol5_19/04/17

1108

140

10−9.28

M1b-M1a (r)

43 ± 16

 

1108

140

10−9.28

M1a-M2 (n)

8 ± 2

ol7_19/04/17

1084

30

10−9.65

M2-M1a (r)

48 ± 15

ol8_19/04/17

1084

30

10−9.65

M2-M1a (r)

30 ± 10

ol9_19/04/17

1084

30

10−9.65

M2-M1a (r)

48 ± 15

ol10_19/04/17

1108

140

10−9.28

M1b-M1a (r)

39 ± 12

ol11_19/04/17

1108

140

10−9.28

M1b-M1a (r)

30 ± 9

ol12_19/04/17

1084

30

10−9.65

M2-M1a (r)

34 ± 11

ol13_19/04/17

1108

140

10−9.28

M1b-M1a (r)

55 ± 17

  1. Δt refers to the time of diffusion calculated for a single zoning type, i.e., normal zoning (n) or reverse zoning (r). Note that crystals characterized by complex zoning patterns have been modeled in multiple steps, and Δt is therefore defined for each step modeling.