|
|
|
|
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 |
OF1B |
Average DC offset of frequency1 noise |
BADF_CMR |
CMR Bad Hole (Mud Signal) Flag |
PPOR |
Partial porosities |
WF9N |
Waveform 9 Normalization Factor |
LLG |
Laterolog Groningen Resistivity |
HFK |
HNGS Formation Potassium Concentration |
EN2 |
Vector amplitude of inter echo noise of frequency2 |
WF3T |
Filtered Waveform 3, 2-inch Averaged |
TNST10 |
Monopole multiplex waveform start time |
AHORX |
Array Induction One Foot Rxo |
RES_MIC |
Microresistivity |
A1EP |
APS Array-1 Detector Count Rate |
TNGN07 |
Monopole multiplex waveform gain |
NRAT |
DSN (NDSN/FDSN) Ratio |
PO7 |
Partial porosity from MRIL (single element) |
AHFSWI |
Array Induction Four Foot Radial Water Saturation Image |
M4R2 |
4 foot vertical resolution matched res. - DOI 20 inch |
HNRH |
High Resolution Enhanced Bulk Density |
UMA_HILT |
Apparent Volumetric Photoelectric Factor of Matrix from HILT Lithology Computation |
SGMA6 |
Complex sigma array 6 |
SSD |
Short Spaced Density Count Rate |
TT |
Interval Transit Time |
GR1X |
Gamma Ray from Detector 1, Transmitted |
CHTP |
Label Peak Coherence, Transmitter Array, Compressional - Monopole P&S |
HALC |
APS High Resolution Near/Array Corrected Limestone Porosity |
|
|
|
|
|
|