Linking Gondwana inheritance to Alpine paleogeography in the Northern Dora-Maira Massif (Western Alps)
Gianni Balestro , Matthieu Roà , Carlo Bertok , Marco Gattiglio , Stefano Ghignone , Chiara Groppo , Valby van Schijndel , Andrea Festa
Geoscience Frontiers ›› 2026, Vol. 17 ›› Issue (2) : 102245
Inherited structures in rifted continental margins strongly influence the architecture and evolution of collisional orogens. The northern Dora-Maira Massif in the Western Alps (NW Italy) preserves records of such inheritances, capturing the transition from Gondwana inheritance to Alpine convergence. New lithostratigraphic and structural data, together with U-Pb zircon dating, reveal a long-lasting tectonostratigraphic and/or magmatic evolution during (i) pre-Permian, (ii) Permian, (iii) Triassic and (iv) Jurassic time intervals. The heterogeneous Paleozoic basement consists of pre-Variscan micaschist and metabasite, and was intruded by Permian igneous bodies now corresponding to the Borgone metagranite and Luserna augen gneiss. The basement was later overlain by a Mesozoic cover made up of Lower Triassic siliciclastic sediments, a Middle to Upper Triassic carbonate platform and Lower to Middle Jurassic syn-rift deposits linked to the opening of the Ligurian-Piedmont Ocean Basin. Our results highlight that the Dora-Maira Massif was located within a transitional paleogeographic domain, emphasizing the role of pre-rift architecture in governing margin segmentation. Successive cycles of sedimentation, magmatism, and rifting created structural and rheological heterogeneities that may have localized strain during the Cenozoic Alpine-related overprinting. The Dora-Maira case illustrates that deep-time inherited structures and tectonostratigraphic settings continue to influence rifting, subduction, and collision, offering a broader framework for understanding the dynamics of orogens worldwide.
Pre-orogenic tectonostratigraphy / Structural inheritance / Ocean-continent transition zone / Western Alps / Dora-Maira Massif
| [1] |
|
| [2] |
|
| [3] |
|
| [4] |
|
| [5] |
|
| [6] |
|
| [7] |
|
| [8] |
|
| [9] |
|
| [10] |
|
| [11] |
|
| [12] |
|
| [13] |
|
| [14] |
|
| [15] |
|
| [16] |
|
| [17] |
|
| [18] |
|
| [19] |
|
| [20] |
|
| [21] |
|
| [22] |
|
| [23] |
|
| [24] |
|
| [25] |
|
| [26] |
|
| [27] |
|
| [28] |
|
| [29] |
|
| [30] |
|
| [31] |
|
| [32] |
|
| [33] |
|
| [34] |
|
| [35] |
|
| [36] |
|
| [37] |
|
| [38] |
|
| [39] |
|
| [40] |
|
| [41] |
|
| [42] |
|
| [43] |
|
| [44] |
|
| [45] |
|
| [46] |
|
| [47] |
|
| [48] |
|
| [49] |
|
| [50] |
|
| [51] |
|
| [52] |
|
| [53] |
d’Atri, A., Piana, F., Barale, L., Bertok, C., Martire, L., 2016. Geological setting of the southern termination of Western Alps. Int. J. Earth Sci. 105 (6), 1831-1858. |
| [54] |
|
| [55] |
|
| [56] |
|
| [57] |
|
| [58] |
|
| [59] |
|
| [60] |
|
| [61] |
|
| [62] |
|
| [63] |
|
| [64] |
|
| [65] |
|
| [66] |
|
| [67] |
|
| [68] |
|
| [69] |
|
| [70] |
|
| [71] |
|
| [72] |
|
| [73] |
|
| [74] |
|
| [75] |
|
| [76] |
|
| [77] |
|
| [78] |
|
| [79] |
|
| [80] |
|
| [81] |
|
| [82] |
|
| [83] |
|
| [84] |
|
| [85] |
|
| [86] |
|
| [87] |
|
| [88] |
|
| [89] |
|
| [90] |
|
| [91] |
|
| [92] |
|
| [93] |
|
| [94] |
|
| [95] |
|
| [96] |
|
| [97] |
|
| [98] |
|
| [99] |
|
| [100] |
|
| [101] |
|
| [102] |
|
| [103] |
|
| [104] |
|
| [105] |
|
| [106] |
|
| [107] |
|
| [108] |
|
| [109] |
|
| [110] |
|
| [111] |
|
| [112] |
|
| [113] |
|
| [114] |
|
| [115] |
|
| [116] |
|
| [117] |
|
| [118] |
|
| [119] |
|
| [120] |
|
| [121] |
|
| [122] |
|
| [123] |
|
| [124] |
|
| [125] |
|
| [126] |
|
| [127] |
|
| [128] |
|
| [129] |
|
| [130] |
|
| [131] |
|
| [132] |
|
| [133] |
|
| [134] |
|
| [135] |
|
| [136] |
|
| [137] |
|
| [138] |
|
| [139] |
|
| [140] |
|
| [141] |
|
| [142] |
|
| [143] |
|
| [144] |
|
| [145] |
|
| [146] |
|
| [147] |
|
| [148] |
|
| [149] |
|
| [150] |
|
| [151] |
|
| [152] |
|
| [153] |
|
| [154] |
|
| [155] |
|
| [156] |
|
| [157] |
|
| [158] |
|
| [159] |
|
| [160] |
|
| [161] |
|
/
| 〈 |
|
〉 |