QUOTE (serpens @ Apr 5 2015, 07:10 PM)
A consensus seems to be forming that the veins seen here and at Sheepbed represent hydraulic fracture fill. This indicates that the mudstone must have been covered to depth certainly no less than a kilometre and probably much more. But it also implies that there would be a significant thickness of sediment below the mudstone which compacted to provide the high pressure solution necessary to fracture the mudstone cap and form the fracture fill.
Yes, the source of the overpressure that resulted in the brittle tensile failure of the mudstone is where my curiosity(!) lies. An authigenic or mineralogic volume increase, as you've stated, could certainly be a good candidate, especially when dealing with anhydrous and hydrated sulphate minerals. Hydrated clays also can exhibit significant volume changes as water is added and lost from their crystal lattice. Deep burial, on its own, should not cause this type of feature. Deep burial followed by quick exhumation, on the other hand, can do this, in the presence of isolated pressure cells (here the sandstone and mudstone strata). Other terrestrial causes include biogenic and thermogenic hydrocarbon generation, although when this happens at deepest burial, horizontal, rather than vertical tensile fractures can form (the famous "beef" veins of the Yorkshire, Dorset, and Somerset Jurassic exposures). It is interesting that you are seeing sigmoidal fractures and C-S features, suggesting some horizontal stress and shear in addition to the burial/vertical/lithostatic stress. In terrestrial fracture fills associated with overpressure, calcite crystallizes in veins as a distinctive cone-in-cone fabric when there is a component of horizontal stress, rather than the prismatatic, fracture-spanning "beef" fabric associated with overcoming lithostatic stress (nice review article, behind a paywall,
here).
The go-to analyses to really determine the source of the overpressure involve determining the phase/PT behavior and composition of fluid inclusions in the fracture fill minerals. Certainly would be candidates for caching for a possible sample return, or reason for including such instrumentation on a future landed mission.