Fig. 12.
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Response of proto-halo regions towards a large-scale tidal field. The different panels show the cases with λz = −0.5, 0 and 0.5 – corresponding to a stretching tidal field, no tidal field and a compressing tidal field in the vertical direction respectively. A negative (stretching) tidal field delays infall and shrinks the proto-halo patches in the corresponding direction, whereas a positive (compressing) tidal field facilitates infall and extends the proto-halo patches.
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