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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.
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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
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4. Foster, R. J. Physical Geology (3rd ed.). C. E. Merrill Publ. Co., Columbus,
OH, 1971, 550 pp.
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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.