Analogue experiments were used to investigate pluton emplacement during tra
nspression in brittle crust. Models consisted of silicone putty placed with
in slots in a rigid basement and an overburden of dry sand. The models were
transpressed, causing emplacement of silicone intrusions into the overlyin
g sand. Space was made for intrusions by upward displacements of overburden
along oblique reverse shear zones, in some cases accompanied by extensiona
l shearing above the intrusions. Silicone putty was progressively accreted
to the bases of uplifted blocks, and growing intrusions rode up the shear z
ones, leaving space for accretion of more silicone. The resulting intrusion
shapes depended largely on the geometries of shear zone systems, which in
turn depended on overburden thickness. The intrusion profiles and the struc
tural relationships between intrusions and host in the experiments are comp
arable to some natural examples. A magma accretion model may thus account f
or pluton emplacement and batholith assembly within some transpressive orog
ens.