Mudlogging is the creation of a detailed record (well log) of a borehole by examining the chips of rock or sediment brought to the surface by the circulating drilling medium (most commonly mud). Mudlogging is usually performed by a third-party surface logging service provider. This provides well owners and producers with information about the lithology, fluid and gas content of the borehole while drilling. Historically it is the earliest type of well log. A mobile laboratory is placed by the surface logging company on the drilling platform, either an on-shore rig pad, or the deck of an offshore drilling rig or ship.
Drill cuttings are small pieces of rock produced by a drill bit moving through subsurface rock formations while drilling wells. These cuttings are brought to the surface by the circulating drilling fluid and are removed from the borehole by screening the drilling mud over shale shakers. As drilling is more economical than coring, cuttings increasingly replace core samples as the only direct evidence of subsurface geology. At the same time, high-performance polycrystalline diamond compact (PDC) drill bits are gradually replacing roller cone bits, producing ever smaller cuttings in some rock formations. As a result, there is an industry requirement for more advanced cuttings analysis and reporting. The analysis of cuttings is referred to as mudlogging and plays an important role by improving on-site interpretation of downhole tool data including logging while drilling (LWD) and wireline logs. In circumstances where downhole data is limited, such as in deep and horizontal drilling, cuttings data may be the only direct data from the borehole.
Cuttings descriptions at the rig site are conventionally based on manual optical inspection under a microscope which identifies mineralogy, rock types (lithologies), grain size, shape and colour. The presence of basic lithologies such as sandstone, siltstone, clay stone and carbonates is reported. This process is necessarily subjective, qualitative, and limited by the lack in ability to accurately describe the mineralogy, including the type of clay minerals, feldspars and carbonates.