Page 202 - Open-Hole Log Analysis and Formation Evaluation

Shoreline
(Sea
General
Alluvial
Delta
Deposit
Turbidites,
: 188
Po
Moving
Point
(Sea
or
River
Depositional
Bar
Bar, Shoreline
away
Marine
| in River Bed al) Envi nvironment : Il. OPEN-HOLE
from
Moving
Fringe
Channel
Deposit
FIGURE
Land)
9.20
onto Land)

SP Shapes

i
Size
: Grain MEASUREMENTS LOGGING 189

.
SP

The
The
The ¢
in Different Depositional Sequences,
Bell
Curve Shape
Cylind
Funnel
Cylinder

the
Their
is
Williams,
Wyllie, M.
October
Symposium,
R.J.:
used
Eventually,
box
SP.Curve,”
1984)
a
3-9.
Mexico
Measutement

SP
Trans.,
H., and Dunlap, H.
and
will
AIME
notation
F.:
City, June

(1949)
1981.
be
186,
Implications,”
off
17.
The

will
on
Log
baseline
/ mation Water Resistivity from the SP Log,” SPWLA, 22nd Annual Silva, P., and Bassiouni, Z.: “A New Approach to the Determination Annual Meeting, Oct. 1958. Segesman, F., and Tixier, M. P.: “Some Effects of Invasion on the SP Curve,” SPE Segesman, F.: “New SP Correction Charts,” Geophysics (December Schlumberger: “Log Interpretation Principles,” vol. 1 (1972),
the
track
Ifa
Analyst
.
Some service company engineers will
edge
, (September- Logging of For- 1962) 27. 2 and 13. Services (1972). Properties of , Equation,” The SP Curve,” Study on the Logging Fresh Water . 03/81, sec. 4 Interpre- Pet Eng. Logging Programmable heading. If “ride” the rapidly downhole and a
this
“Short Term Variations in Drilling Parameters.
“A Quantitative Analysis of the Electrochemical Component.of