SERPENTINES IN THE OPHIOLITE COMPLEXES OF THE VOURINOS AND KAMVOUNIA MTS. (NORTHERN GREECE)

Year, pages: 1997, 19 - 26

The Vourinos as well as the Kamvounia ophiolite complexes yielded in origin of the serpentine-group minerals of different appearance. In this stage of laboratory studies we have concentrated on: a — filling of shear zones occurring within "basal serpentinites" of the Vourinos Complex (lizardite + chrysotile + splintery antigorite), b — the rock-forming mass of the Kamvounia massif (antigorite), c — slip-fiber "asbestos" within the Kamvounia massif (chrysotile + fibrous antigorite). While the Vourinos Complex during its geological history never reached greenschist facies conditions, the Kamvounia massif underwent metamorphic recrystallization under such conditions.

Hovorka, D., Savvidis, S., Stankovic, J., Samajova, E., Turanova, L. 1997. SERPENTINES IN THE OPHIOLITE COMPLEXES OF THE VOURINOS AND KAMVOUNIA MTS. (NORTHERN GREECE). In Geologica Carpathica, vol. 48, no.1, pp. 19-26. 1335-0552.

Hovorka, D., Savvidis, S., Stankovic, J., Samajova, E., Turanova, L. (1997). SERPENTINES IN THE OPHIOLITE COMPLEXES OF THE VOURINOS AND KAMVOUNIA MTS. (NORTHERN GREECE). Geologica Carpathica, 48(1), 19-26. 1335-0552.