|
|
|
|
Welcome to Petroleum Geology Forums
This is a free online community that aims to bring petroleum professionals and geologists together and share valuable knowledge. Registration is easy so become a member now for instant free access.
- Petroleum Geologists can stay up to date with industry related topics and exchange ideas and concepts.
- Upstream Oil and Gas Consultants get a chance to share their expertise and gain exposure to land future projects.
- Geology students and graduates can join the discussion and get into contact with potential future employees.
|
|
|
Petroleum Geology AcronymsBrowse through the Acronyms using the letters above or search for the acronym or it's description using the form below. If you have a acronym or abbreviation you would liek to see in this list please contact us.
|
|
Acronym |
Full Name |
RNL |
Real-Time CNP (Limestone Matrix) |
NEU |
Neutron Porosity |
RXO_HRLT |
HRLT Invaded Zone Resistivity |
SSN |
Short Spaced Neutron Count Rate |
TEN |
Differential Tension |
PORA |
Acoustic porosity |
BIT_SIZE |
Bit Size |
FCN |
Formation Factor from CNC |
COHC |
Coherence Value at Compressional Peak |
HLGU |
HALS Uncorrected Laterolog Groningen Resistivity |
CHR2 |
Label Peak Coherence, Receiver Array - Upper Dipole |
LSW |
HRDD Calibrated Count Rate (Array) of Gamma Rays from Long Spacing Device |
PO7C |
Partial porosity from MRIL (single element) |
SONL |
Minimum Ultrasonic Standoff, Left |
GRR_CDR |
Raw Gamma Ray Average |
CRMQ |
Enhanced processing medium quad conductivity |
SCR1 |
Small Shock (50G) Count |
DT24.X |
Interval transit time over 24 inch interval (cross correlation) |
EXD |
Phase avg'd amp of channel 1 (real) portion of echo train |
TCRL |
Long-Spaced Total Countrate |
TTSL |
Transit Time (Sliding Gate) |
SPLF |
Smoothed CNP (Limestone Matrix-Fixed Hole Size) |
ATD2 |
Array Induction Two Foot Outer Diameter of Invasion (D2) |
RPCVSL |
Resistivity Phase Diff Compensated Borehole and Inversion Corrected Short 400kHz |
CRDQ |
Enhanced processing deep quad conductivity |
|
|
|
|
|
|