|
|
|
|
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 |
QP28 |
Acoustic pick quality curve |
GRAX |
Gamma Ray Apparent, Transmitted |
TYXST11 |
Y-x axis dipole multiplexed waveform start time |
NPBM |
Neutron Porosity Base, Memory |
DTCO |
Delta-T Compressional |
HTT3 |
High Resolution Transit Time 3 |
CHT1 |
Label Peak Coherence, Transmitter Array - Lower Dipole |
FPE |
Far Detector Only Photoelectric Absorption Factor |
ASOA |
Average Ultrasonic Standoffs, Quadrant(B-L-U-R) Array |
VCL_HILT |
Volume of Clay type Material relative to Total Volume from HILT Lithology Computation |
WF8 |
Waveform 8 |
VSSG |
Volume of Shale from SGR |
P16H |
ARC Phase Shift Resistivity 16 inch Spacing at 2 MHz, Environmentally Corrected |
SFL7 |
Synthetic focused laterolog 7 resistivity |
QP22 |
Acoustic pick quality curve |
WFSH |
Warning Flag for Shear |
B15 |
B1 magnetic field strength |
TNRB_RT |
Thermal Neutron Ratio, Bottom, Real-Time |
TRMTT07 |
Monopole multiplex first arrival time |
FGA12 |
Fixed gate amplitude in cbl |
TNWV05 |
Acoustic multiplex waveform |
DPHI |
Density Porosity |
MRM |
Mud resistivity from rmudtmp2_0 pfn |
P16H_UNC |
ARC Uncorrected Phase Shift Resistivity for 16 inch Spacing at 2 MHz |
SG22 |
Signature from transmitter 2, receiver 2 |
|
|
|
|
|
|