Table 1
Paleomagnetic database used in the discussion. N: number of sites used, n: number of samples. D: declination, I: Inclination, α95: 95% confidence cone, K: precision parameter, R: predicted rotation, dR: error on the rotation (calculated after Demarest, 1983). The rotation and its error are calculated taking into account the age of magnetization and the corresponding Torsvik et al. (2012) synthetic APWP reference. (a): combination of data from Crouzet et al., 1996; Dumont et al., 2008; Ménard et Rochette, 1992 and Lamarche et al., 1988.
III. Primary directions with paleohorizontal | ||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Formation | Lat | Long | Age of magnetization (Ma) | N/n | D | I | alpha 95 | K | Rotation | dR | Significant | Age − R | Reference | |
1 | Swiss Molasse | 46.5 | 6 \ 7 | 13-29 | 2412 | 16.4 | 46.7 | 3.3 | 82.9 | 12.4 | 5.0 | Y | 20 | Kempf et al., 1998 |
2 | Savoie Molasse | 46 | 5.9 | 26-23 | 2 | 352.2 | 53.8 | 6.3 | 11.4 | −12.8 | 9.1 | Y | 25 | Burbank et al., 1992 |
3 | Paleocene lacustrine | 43.6 | 5.5 | Paleocene | 10/96 | 9.5 | 46.8 | 8.3 | 33.2 | 9.2 | 10.2 | N | 60 | Westphal and Durand, 1989 |
4 | Paleocene lacustrine | 43.5 | 5.5 | Paleocene | 335 | 5.6 | 52.5 | 1.2 | 23 | 5.3 | 3.8 | Y | 60 | Cojan et al., 2000 |
5 | Continental Oligocene | 43.5 | 5.5 | 30-25 | 41 | 350.6 | 55.1 | 3.5 | 618 | −16.5 | 6.0 | Y | 25 | Kechra et al., 2003 |
6 | Arc de Nice Priabonian | 43.8 | 7.41 | 35 | 2/26 | 229.1 | −36.9 | 2.6 | 452 | 42.0 | 4.4 | Y | 35 | Sonnette, 2012 |
7 | Eo-Oligocene, Ultra helvetic nappes (Dérochoir) | 46 | 6.8 | Eo-Oligocene | 16 | 312.3 | 58.5 | 11.4 | 9.5 | −55.9 | 18.0 | Y | 40 | Piquet et al., 2000 |
8 | Eo-Oligocene, Ultra helvetic nappes (Marais) | 45.9 | 6.4 | Eo-Oligocene | 35 | 243.2 | 48.7 | 6.7 | 26.8 | −125.1 | 8.9 | Y | 40 | Piquet et al., 2000 |
9 | Torino and Monferrato Hills | 45.1 | 8.1 | Miocene | 2/17 | 331.5 | 63.5 | 15.6 | 259.0 | −31.6 | 29.4 | Y | 15 | Bormioli and Lanza (1995) |
10 | Piemonte basin − Northwestern Apennine | 44.8 | 9 | Late Eocene-Early Oligocene | 1/33 | 333.2 | 50.3 | 5.8 | – | −32.8 | 7.3 | Y | 30 | Vandenberg (1979) |
11 | Oligocene Piemonte Basin | 44.8 | 9 | Oligocene | 10 | 318.7 | 53.8 | 6.6 | 55.0 | −46.3 | 9.5 | Y | 25 | Thio, 1988 |
12 | Tertiary Piemonte Basin | 44.5 | 8.5 | Oligocene-lower miocene | 3/31 | 320.2 | 44.5 | – | – | −43.8 | 20 | Carrapa et al. (2003) | ||
13 | Tertiary Piemonte Basin | 44.5 | 8.5 | Oligocene | 23 | 310.6 | 45.6 | 13.7 | 19.7 | −55.5 | 15.7 | Y | 30 | Maffione et al., 2008 |
14 | Sardinia preopening volcanics (synthesys) | 42 | 9 | Late Oligocene-Aquitanian | 59 | 329.2 | 44.7 | 4.9 | 15 | −34.8 | 6.3 | Y | 20 | Muttoni et al., 1998 |
15 | Sardinia sediments | 39.6 | 8.8 | Lower-Middle Miocene | 1/24 | 340.6 | 39.3 | 3.9 | 58.6 | −23.4 | 5.1 | Y | 20 | Speranza et al., 2002 |
16 | Sardinia Volcanics | 40.2 | 8.7 | 20-21 | 35 | 320.6 | 46.4 | 6.4 | 15 | −43.4 | 8.0 | Y | 20 | Gattacceca et al., 2007 |
17 | Corsica St Florent basin | 42.7 | 9.3 | Midlle Miocene | 4 | 342.6 | 47 | 9.3 | 99 | −20.5 | 11.2 | Y | 15 | Vigliotti and Kent, 1990 |
18 | Corsica Balagne sediments | 42.6 | 9 | Midle Eocene | 1/17 | 151 | −47.2 | 4 | 80 | −37.2 | 6.0 | Y | 40 | Vigliotti and Kent, 1990 |
19 | Corsica volcanics | 41.4 | 9.2 | ∼21 | 4 | 343 | 60 | 8.8 | 110 | −21.0 | 14.4 | Y | 20 | Ferrandini et al., 2003 |
20 | Corsica Oligocene Sediments | 41.9 | 8.8 | Chattian | 1/8 | 140 | −31 | 3.1 | 313 | −45.0 | 4.4 | Y | 25 | Ferrandini et al., 2003 |
21 | Epiligurian basins | 44.4 | 10.8 | Late Oligocene-Middle Miocene | 7/62 | 303.5 | 48 | 11.2 | 30 | −61.0 | 14.4 | Y | 25 | Muttoni et al., 1998 |
II. Secondary directions with paleohorizontal | ||||||||||||||
Formation | Lat | Long | Age (Ma) | N | D | I | alpha 95 | K | Rotation | dR | Significant | Age − R | Reference | |
22 | Metasediments Adamello | 46 | 10.6 | 40-30 | 15 | 9.6 | 61.2 | 5.9 | 54.4 | 2.5 | 10.4 | N | 30 | Kipfer and Heller, 1988 |
23 | Chartreuse and Vercors | 45.2 | 5.5 | Tertiary | 119 | 12.6 | 56 | 7 | 42 | 8.6 | 10.5 | N | 30 | Aubourg and Rochette, 1992 |
24 | Berrias normal | 44.4 | 4.3 | Tertiary ? | 83 | 9 | 49.2 | 3.6 | 18.6 | 0.8 | 5.8 | N | 30 | Galbrun, 1985 |
Berrias reverse | 44.4 | 4.3 | Berriasian | 80 | 170.6 | −43.6 | 4.6 | 11.4 | −9.4 | 5.0 | Y | * | Galbrun, 1985 | |
25 | Cevennes | 44.2 | 4.1 | Eocene | 15/244 | 3.1 | 55.7 | 0.8 | 165 | −5.1 | 4.0 | Y | 40 | Henry et al., 2001 |
26 | Cevennes | 44 | 3.8 | 40 | 11/88 | 10.4 | 63.9 | 7.3 | 39.9 | 2.2 | 13.8 | N | 40 | Kechra et al., 2003 |
27 | Ventoux massif | 44.2 | 5.8 | 40 | 10/80 | 355.5 | 55.1 | 7.6 | 41.4 | −12.7 | 11.2 | Y | 40 | Kechra et al., 2003 |
28 | Vocontian basin | 44.4 | 5.6 | 40 | 15/227 | 357.7 | 54.8 | 6 | 42.1 | −10.5 | 9.1 | Y | 40 | Katz et al., 1998, 2000 |
29 | Dévoluy-Diois | 44.6 | 5.7 | Tertiary | 89 | 338.6 | 53.5 | 10.6 | 17.8 | −27.5 | 14.3 | Y | 30 | Aubourg et Chabert-Pelline, 1999 |
30 | Barrot Dôme | 44 | 6.8 | 30 | 4 | 300.9 | 58.0 | 9.9 | 52.1 | −65.1 | 15.0 | Y | 30 | Sonnette et al., 2014 |
31 | Esparon | 44.32 | 6.15 | <10 | 7/62 | 5.1 | 60.9 | 7 | 76.3 | 2.8 | 11.7 | N | 10 | Cairanne, 2004 |
32 | Gaubert | 44.03 | 6.21 | <10 | 3/28 | 14.8 | 58.4 | 5.7 | 475.7 | 12.5 | 8.9 | Y | 10 | Cairanne, 2004 |
33 | Bès | 44.24 | 6.26 | <23 | 4/31 | 347.3 | 60.2 | 9.7 | 91.3 | −17.7 | 16.0 | Y | 25 | Cairanne, 2004 |
34 | Barrème | 43.96 | 6.41 | <23 | 2/21 | 1.8 | 60.1 | 3.8 | 440.7 | −3.2 | 6.9 | N | 25 | Cairanne, 2004 |
35 | Arc de Castellane | 43.92 | 6.8 | <10 | 15 | 355.1 | 63.5 | 7 | 30.8 | −7.2 | 12.7 | N | 10 | Sonnette 2012 |
36 | Arc de Nice | 43.85 | 7.42 | <10 | 3/30 | 349.2 | 62 | 7.1 | 303 | −13.1 | 12.2 | Y | 10 | Sonnette 2012 |
37 | Jura | 47.2 | 7.2 | Miocene | 16/192 | 359.1 | 63.8 | 5.7 | 43 | −3.2 | 10.5 | N | 15 | Johnson et al., 1984 |
38 | Digne nappe | 44 | 6.5 | Tertiary | 80 | 348.4 | 52.5 | 16.6 | 7.8 | −17.6 | 22.2 | N | 30 | Aubourg et Chabert-Pelline, 1999 |
III. Primary directions without paleohorizontal | ||||||||||||||
Formation | Lat | Long | Age (Ma) | N | D | I | alpha 95 | K | Rotation | dR | Significant | Age − R | Reference | |
39 | Bergell massif | 46 | 8 | 30-25 | 405 | 338.7 | 57.4 | 1.2 | – | −26.3 | 3.7 | Y | 30 | Heller, 1980 |
40 | Sesia andesites dikes | 45.5 | 8 | 33-30 | 68 | 337.2 | 37.3 | 9.7 | – | −28.8 | 9.8 | Y | 30 | Lanza, 1977 |
41 | Sesia andesites flows | 45.5 | 8 | ∼30 | 152 | 135.9 | −2.9 | 8.8 | 27.8 | −50.1 | 7.1 | Y | 30 | Lanza, 1979 |
42 | Traversella massif | 45.5 | 7.8 | ∼30 | 8/150 | 142.7 | −6.3 | 6 | – | −43.3 | 5.0 | Y | 30 | Lanza, 1984 |
43 | Dikes Biellese | 45.6 | 8.1 | Tertiary | 11 | 331 | 31 | 19 | – | −35.0 | 17.7 | Y | 30 | Bigioggero et al., 1981 |
44 | Esterelite intrusions | 43.5 | 6.8 | 33 | 37 | 349.5 | 51 | 7.1 | 118 | −17.6 | 9.6 | Y | 30 | Zijderveld, 1975 |
IV. Secondary directions without paleohorizontal | ||||||||||||||
Formation | Lat | Long | Age (Ma) | N | D | I | alpha 95 | K | Rotation | dR | Significant | Age − R | Reference | |
45 | Aar massif | 46.5 | 8.7 | 25-12. | 2/27 | 186.7 | −70.1 | 8.1 | – | 2.7 | 19.6 | N | 20 | Heller, 1980 |
46 | Eastern Dauphinois zone (North − Joly) | 45.8 | 6.7 | 20-30 | 14 | 18.3 | 63.4 | 9.7 | 17.7 | 13.3 | 17.8 | N | 25 | Crouzet Unpublished |
47 | Eastern Dauphinois zone (Center − Maurienne) | 45.3 | 6.3 | 20-30 | 43 | 358.9 | 63 | 4.7 | 22.6 | −6.1 | 8.8 | N | 25 | Ménard and Rochette, 1992 |
48 | Eastern Dauphinois zone (Bourd d’Oisans + Romanche) | 45 | 6.1 | 25-23 | 58 | 3.5 | 61.5 | 3.9 | 24.2 | −1.5 | 7.3 | N | 25 | (a) |
49 | Briançonnais Am. Rosso | 44.7 | 6.6 | 30-25 | 76 | 142 | −57 | 8 | 44 | −44.0 | 11.8 | Y | 25 | Thomas et al., 1999 |
50 | Ubaye Am. Rosso | 44.5 | 6.8 | Lower Oligocene | 85 | 121 | −52 | 11 | 17 | −64.0 | 14.6 | Y | 30 | Collombet, 2001 |
51 | Liguria | 44.1 | 7.6 | Lower Oligocene | 58 | 72 | −48 | 15 | 20 | −113.0 | 18.3 | Y | 30 | Collombet, 2001 |
52 | Lepontine dome (without Bergell) | 46.3 | 8.8 | 25-12. | 8/102 | 331.7 | 59.5 | 7.8 | 51.9 | −32.3 | 12.7 | Y | 20 | Heller, 1980 |
53 | Traversella massif | 45.5 | 7.8 | post 30 | 2/34 | 338.7 | 55.7 | 25.4 | 98.6 | −27.3 | 39.2 | N | post 25 | Lanza, 1984 |
54 | Besano Mt San Giorgio | 45.8 | 8.9 | Eocene | 2/32 | 338.5 | 34.1 | 5.3 | 24.3 | −27.5 | 5.3 | Y | post 30 | Dallanave and Muttoni, 2007 |
55 | Permian volcanic rocks Guil valley | 44.67 | 6.67 | Eocene ? | 8 | 147 | −32 | 14 | 16.7 | −39.0 | 13.2 | Y | 30 | Roche and Westphal, 1969 |
The rotation is calculated after Demarest (1983) taking into account the age of magnetization and the corresponding Torsvik et al. (2012) synthetic APWP reference.
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