Page 200 - Geology of Carbonate Reservoirs
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FRACTURES AND FRACTURED RESERVOIRS  181

























               Figure 7.5   Photo of a microbial bioherm in the Wilberns Formation (Cambrian) of Central
               Texas showing differential compaction that has caused fracturing in bedded rocks immedi-
               ately above and below the bioherm. This type of fracturing is commonly associated with large


               reef and mound buildups. (Photo by Richard Rezak in Ahr (1971) .)
                    Surface - related fractures are created by unloading stresses. Quarrying and weath-
               ering, for example, may remove stabilizing masses and create instability that leads
               to collapse of quarry walls. Surface - related fractures are not considered to be impor-
               tant in hydrocarbon reservoirs.
                    Fractures can also be produced by differential compaction at the local scale, such
               as compaction of strata above buried topography. Antecedent features such as reefs
               and mounds, shelf edges, erosional outliers, or horst blocks could cause overlying
               beds to drape, extend, and fracture in patterns related to the size and shape of the
               antecedent topographic feature. For example, brittle fractures have been docu-
               mented by this author in the basal 5 – 20 meters of Mississippian  “ mud mounds ”  in
               the Williston Basin of North Dakota, where thin (1 – 15  cm thick) mudstone and

               cementstone beds appear to have been fractured by the overburden load of the
               mature mound (up to 150 meters thick). Differential compaction of carbonate strata
               above and below resistant mounds and reefs is common. An excellent example is
               illustrated by a Cambrian microbialite mound in Central Texas (Figure  7.5 ), where
               the beds above have draped (extension) over the mound and the beds below have
               been compressed (compaction) by the concentrated overburden. Larger - scale dif-
               ferential compaction fractures can occur along buried shelf edges, large reefs, ero-
               sional remnants, and fault blocks.

               7.1.4  Fracture Morphology

                 In fractured reservoirs, total porosity and permeability values consist of both matrix
               and fracture components. In order to assess the importance of fracture porosity and
               permeability to total reservoir performance, it is necessary to determine the relative
               contributions of matrix porosity and permeability as compared to fracture porosity
               and permeability. Nelson  (2001)  ranks the four most useful petrophysical determina-

               tions to make on fractured reservoirs (in order of increasing difficulty of calculation)
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