|
|
|
|
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 |
SCO3 |
Smoothed Worst Bin Standoff Correction |
HFEC |
APS High Resolution Far Detector Count Rate |
TRDST01 |
Dipole multiplex waveform start time |
B1B |
B1 magnetic field strength (second TR) |
P16H_UNC |
ARC Uncorrected Phase Shift Resistivity for 16 inch Spacing at 2 MHz |
TRMWV04 |
Acoustic multiplex waveform |
VSUC |
Volume of Shale from Uranium |
OF2 |
Average DC offset of frequency2 noise |
HURC |
HNGS Formation Uranium Concentration in pCi/g |
AHTRT |
Array Induction Two Foot Rt |
RUK |
Ratio of curves U/K |
CNEC |
Corrected Near Epithermal Counts |
SNSC |
Smoothed Near Detector ONLY Porosity (Sandstone Matrix-Caliper Corrected) |
PESI |
Photoelectric Factor Image, 0.1 ft, 16-Sector |
AT10 |
Array Induction Two Foot Resistivity A10 |
CBLF |
CBL Amplitude Fluid Compensated |
GKCL |
Gamma KCl |
TCMR_SIG |
Standard Deviation of Total CMR Porosity |
M2C2 |
2 foot vertical resolution matched cond. - DOI 20 inch |
PO8C |
Partial porosity from MRIL (single element) |
CMFF_SL |
CMR Free Fluid - Station Log |
GRTO |
Total Gamma (150 KeV - 3 MeV) |
TRMST01 |
Monopole multiplex waveform start time |
PPT |
User-entered predicted pipe time |
RAC |
Resistivity Attenuation Borehole Corrected |
|
|
|
|
|
|