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Chapter 1 – DRILLING GEOLOGY                                       7






                                            Lithology

                    Lithology refers to the physical character of the rock. Lithology is a
                 description of the rock and is based on such characteristics as mineral
                 composition, color, grain size, and other textures. Thus a shale could contain
                 some sand (sandy shale) or a rock could be mainly sand with some shale
                 minerals within it (shaley sand). The lithology will affect many drilling
                 decisions when planning and drilling the well. If the wrong decisions are
                 made due to a lack of detailed lithology knowledge, serious problems can
                 result that will increase the cost of the well and could even prevent the well
                 from reaching its objectives.


                    Shales

                    Shales consist of layers of clay minerals. Clay minerals are crystal
                 structures of various metal oxides associated with alumina silicates in
                 connection with varying numbers of water molecules. The metal oxides
                 are most commonly those of iron and magnesium but may also be
                 those of sodium, potassium, or other metals. Their presence together in
                 varying ratios results in a wide range of clay mineral types. Clay minerals
                 originate in sedimentary rocks by the physical and chemical breakdown
                 of other minerals originally present. The weathered clays are carried by
                 wind or water, or both, to an area of eventual deposition. They may then
                 undergo further physical or chemical breakdown. More water may become
                 associated with the clay minerals.

                    Eventually the clay minerals become buried under other sediments.
                 They will be compacted, and water will be driven off. Diagenesis will alter
                 their structure or composition to change the accumulation of clay minerals
                 into a sedimentary rock type. The water that comes out of the shale is less
                 saline (contains less salt) than the water left behind, so the shale gets more
                 salty as it dehydrates.
                    Some shales react very quickly with water. Hydration of these shales
                 leads  to  the  crystalline  layers  expanding.  During  drilling,  fluids  are

                 pumped down the hollow drillstring and back up the hole to clean and
                 cool the drill bit and perform various other functions. If such a shale is

                 drilled using water as the circulating fluid, the shales can absorb water and
                 rehydrate. Millions of years of diagenesis can be reversed in under an hour.







        _Devereux_Book.indb   7                                                   1/16/12   2:06 PM
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