The Moho Transition Zone of ophiolites is dominantly composed of dunit
e, with various types of segregations (gabbros, pyroxenites, and chrom
itites). Representing a level of magmatic exchange between asthenosphe
ric mantle and the constructing ocean crust, it records active melt ci
rculation below a spreading ridge axis and offers the opportunity of o
bserving the distribution of melt locally percolating and pending in a
deforming porous matrix. In the Oman ophiolite, the Moho Transition S
one has a thickness varying from ten to hundreds of meters; its thickn
ess and composition are related to the geometry of the asthenospheric
mantle flow: thick Moho Transition Zones are on top of mantle diapirs
characterized by vertical flow, whereas thin Moho Transition Sones are
present in areas of horizontal mantle flow. A large high-temperature
plastic strain is recorded in thin Moho Transition Sones, in contrast
to thick ones where the strain is weaker and heterogeneous. Thick Moho
Transition Zones display an intense magmatic activity expressed by di
ffuse melt impregnations, dikes and sills. In these thick zones, we ha
ve studied the geometry of the melt circulation at various scales. We
present here the analysis of textures and lattice fabrics which record
high-temperature plastic strain and allow us to quantify it. Melt cir
culates within the dunites and can locally destroy the solid framework
, in relation to a viscosity drop and the sharp overturn of mantle flo
w observed in this type of transition zone.