Stretched pebble conglomerate L-tectonite illustrating a stretch lineation within a shear zone, Glengarry Basin, Australia.
2.
These tectonite layers are of whitish color and tend to survive granular or mass exfoliation much longer than the surrounding protolith.
3.
The tectonite layer is always thickest in the central part of the cupule, i . e . where the greatest amount of energy was applied.
4.
The foliation planes are close to vertical and contain horizontal lineations also striking NW-SE . The rock is therefore a " S-L tectonite ".
5.
The conversion to tectonite does not appear to be reversible, and the high resistance of that product to weathering processes protects the parent rock it conceals from both granular and mass exfoliation.
6.
This definition has been challenged recently because new studies of oceanic crust by the Integrated Ocean Drilling Program and other research cruises have shown that in situ ocean crust can be quite variable, and that in places volcanic rocks sit directly on peridotite tectonite, with no intervening gabbros.
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