She takes the broadest of views, including any discrete carbonate structure with topographic relief formed by in situ or bound organic components.
There is also a general lack of seismic reflection horizons as a result of the uniformity of the carbonate succession.
They are attached to the vein walls and embedded in carbonates just like the carbonaceous filaments.
These fluids emanate from gigantic carbonate edifices that can reach 60m in height.
Syn-kinematic, en-echelon tension gaps were filled by carbonate material.
Possibly existing carbonates will form sulphates at their surfaces.
We present a record of carbonate-associated trace sulfate concentrations over the same time period.
The sabkhas are covered by a salt crust, 3-5 cm thick, under which there lies 25-150 cm of carbonate sand, gypsum and halite.
