Hi Denis, Robert,
Just checked, it is called nappes in English

. These are sheets of sediments and other rocks, which are pushed on top and over each other during orogenesis (mountain forming) caused by continental drift, in this case the proto-Italian plates and African shield moving into the European shield. Shields are essentially the oldest part of continents, formed when the Earth first cooled off.
The gneiss, which essentially is formed by warmed up sediments (because they were lying rather deep originally), to a degree that these old sediments lost all old structures, and aren't recognizable as sediments anymore, are nappes themselves, as are the calcareous rocks and sandstones etc., in the Alps and adjoining mountains. The granite is old shield, i.e., old continental crust, but even some pieces of those became nappes because the shear force broke off large shards of the stuff. By large I mean many kilometres in size.
Generally, however, the granites in the Alps are so-called massifs, which were there orginally, and which were covered by younger rocks, not necessarily in the right order, of tectonically shifted layers of rocks.
So, the choice of granite for this pen is correct: the granites form the old, original core of the Alps, and of the Mont Blanc.
And Robert, you were right after all: the gneiss is younger than the granite; I did look it up.
Warm regards, Wim