|
|
|
|
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 |
TICK_NEU |
Neutron Ticks, 0.1 ft |
LSW1 |
Raw Long Spacing Window 1 Count Rate |
MBVIB |
Irreducible fluid indexes |
TNWV07 |
Acoustic multiplex waveform |
AHO90 |
Array Induction One Foot Resistivity A90 |
CALY |
Caliper from y axis of x-y caliper(s) |
SW |
Water Saturation |
CHTS |
Label Peak Coherence, Transmitter Array, Shear - Monopole P&S |
B15 |
B1 magnetic field strength |
ATD1 |
Array Induction Two Foot Inner Diameter of Invasion(D1) |
CFF2_SL |
CMR Free Fluid for T2 Cutoff 2 - Station Log |
SG22 |
Signature from transmitter 2, receiver 2 |
PORD |
Bulk Density Porosity from DEN |
APLC |
APS Near/Array Corrected Limestone Porosity |
DTRP |
Delta-T Compressional, Receiver Array - Monopole P&S |
GAIN |
Average amplitude of gc1 and gc2 (vector sum) |
SG21 |
Signature from transmitter 2, receiver 1 |
DPE |
Pe Correction |
TTS1 |
Transit Time High Resolution Short Spacing 1 |
HEND_RT |
Near Helium Bank Total Counts, Real-Time |
TXXST01 |
4 component dipole x-x multiplex waveform start time |
LLDC |
Corrected Laterolog Deep Resistivity |
PO9B |
Partial porosity from MRIL (single element) |
SFXN |
Smoothed Neutron Formation Exposure Time |
SG12 |
Signature from transmitter 1, receiver 2 |
|
|
|
|
|
|