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26     PETROPHYSICS: RESERVOIR ROCK PROPERTIES


                      Porphyroblasts: crystals created during metamorphism that are larger
                    than the mineral grains in the rock.
                      Pyroclasts: viscous magma containing gas erupting at the surface; the
                    gas expands rapidly, blowing the plastic magma into fragments high in
                    the air. Pyroclasts less than 2 mm in size are called ash, between 2 mm
                    and 64 mm it is lapilli, and when the size is greater than 64 mm pyroclasts
                    are known as blocks or bombs.
                      Pumice: formed from a froth of  small bubbles in magma which has
                    erupted suddenly. It is light, glassy, and floats on water.
                      Sedimentary rocks: composed of  the weathered fragments of  older
                    rocks that are deposited in layers near the earth’s surface by water, wind,
                    and ice.
                      Shale: composed of clay particles less than 1/256 mm. Not gritty when
                    tested by biting. Exhibits fissility.
                       Siltstone  (mudstone):  composed  of  particles  between  1/256  and
                    1/16 mm in size. Noticeably gritty to the teeth.
                      Tuff  a  deposit of  volcanic ash that  may  contain  as  much  as  50%
                    sedimentary material.
                       Vitreous (glassy): variously described as greasy, waxy, pearly, or silky.

            REFERENCES


                      1. Allen, T. 0. and Roberts, A.  P. Production Operations, Vol. I. Oil & Gas
                        Consultants International, Inc., Tulsa, OK, 1982, 290 pp.
                      2. Crocker,  M.  E.,  Donaldson,  E.  C.  and  Marchin,  L.  M.  “Comparison
                        and Analysis  of  Reservoir Rocks and Related Clays.” DEO/BETC/RI-S3/7,
                        Oct.  1983. National  Technical Information Service,  US  Department of
                        Commerce, Springfield, VA, 25 pp.
                      3. Donaldson, E. C. and Crocker, M. E. “Characterization of the Crude Oil Polar
                        Compound Extract.” DOE/BETC/RI-80/5,  Oct.  1980. National Technical
                        Information Service,  US Department of Commerce, Springfield, VA, 27 pp.
                      4. Foster, R. J. Physical Geology (3rd ed.). C. E. Merrill Publ. Co., Columbus,
                        OH, 1971, 550 pp.
                      5. Ehlers,  E.  G.  and  Blat,  H.  Petrology:  Igneous,  Sedimentary  and
                        Metamorphic.  W. H. Freeman, San Francisco, 1982, 731 pp.
                      6. Bowen, N. L. The Evolution of Igneous Rocks. Princeton University Press,
                        Princeton, NJ, 1956, 333 pp.
                      7. George, R.  D. Minerals and Rocks. D. Appleton-Century Co., New York,
                         1943,595 pp.
                      8. Correns, C. W. Introduction to Mineralogy. Springer-Verlag, New York,
                         1969,484 pp.
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