Cement! Refer back to
post 23: The sand grains (referred to by nerds [me] as 'framework grains') are the dark, roundish things that dominate the frame. The brighter areas in between are cement. This particular example is cemented by calcite, and all of the pore space that was in the sediment when it was deposited has been filled by the cement. However, many, many different minerals can be cements. Quartz, carbonate (calcite, dolomite, etc.), salts (halite, gypsum, anhydrite, etc.), and clays are quite common cements, but cement can take almost any form. Referring back to our picture, we can actually see a couple of different cementation 'events'. The first was most likely an 'early marine' cementation event, common in carbonates. This cementation happens almost as soon as the sediment is deposited, and is represented here by a thin layer of very small, prismatic crystals [bless and do not curse][bless and do not curse][bless and do not curse][bless and do not curse][bless and do not curse][bless and do not curse][bless and do not curse] the edges of the grains themselves. Squint! They're there! They look a bit like this:
The second event is represented by larger, somewhat rounded-looking crystals that fill the remainder of the pore. This event must have happened while the rock was buried deep underground, since the cement fills a fracture that runs ENE across the lower right corner of the picture. Fractures of this type are typically from compaction, which is a result of a heavy (thick) sedimentary overburden.
Sedimentary cements are a chemical precipitate, formed as mineral-rich ground water flows through the pores in the rock.
In the case of rocks made of small, clay sized grains (mudstones and shales, as well as wackestones, which are muddy with dispersed sand-sized grains), cementation takes a back seat to compaction. Muddy rocks can be compacted by up to a factor of ten, and typically have too little pore space for the transmission of ion-bearing waters.