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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.
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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.
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Acronym |
Full Name |
ATCO10 |
Array Induction Two Foot Conductivity A10 |
TYXGN01 |
Y-x multiplex waveform gain |
PO2 |
Partial porosity from MRIL (single element) |
WF1T |
Filtered Waveform 1, 2-inch Averaged |
TCMR |
Total CMR Porosity |
WF4I |
Filtered Waveform 4, 1/2-ft Averaged |
QPN3 |
Acoustic pick quality curve |
FGA12 |
Fixed gate amplitude in cbl |
DPHD |
Density Porosity, Dolomite |
CBF3 |
CMR Bound Fluid Volume for T2 Cutoff 3 |
EHGR |
High Resolution Corrected Gamma Ray |
TRMTT03 |
Monopole multiplex first arrival time |
SGRP |
Strain gauge raw pressure |
TXXWV10 |
X-x axis dipole multiplex waveform |
SNSF |
Smoothed Near Detector ONLY Porosity (Sandstone Matrix-Fixed Hole Size) |
SGM4 |
Complex sigma array 4 |
HLLL |
LDS High Resolution Long-Spaced LL Raw Window Count Rate |
SPDC |
Smoothed CNP (Dolomite Matrix-Caliper Corrected) |
PO5 |
Partial porosity from MRIL (single element) |
SNSC |
Smoothed Near Detector ONLY Porosity (Sandstone Matrix-Caliper Corrected) |
SCOR |
Smoothed Standoff Correction |
CHT.T |
Cable Head Tension (Time-based) |
EC11F |
MRIL filtered echo train packet 1 real |
HTNP |
High Resolution Thermal Neutron Porosity (Ratio Method) in Selected Lithology |
RILM |
Medium induction resistivity |
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