Assuming that the overburden stress (Sv), is one of the three principal stresses, the stress tensor (representing the in-situ stress field)…
Microseismic location error simply explained
What is microseismic location error?
6 Essential Tools for Geosciences and Engineering Training while Working from Home
2020 has been a year like none other with many businesses adjusting to be able to work from…
Extended Leak-off Test 101
Assuming that the overburden stress (Sv), is one of the three principal stresses, the stress tensor (representing the in-situ stress field)…
What’s b-value after all?
Simply put, b-value is the slope of a log-normal distribution of passive seismic event sizes, namely the number…
On Predicting Physical Rock Properties
The physical properties of rocks – their density and elastic moduli – along with their porosity and the…
Peer-Benchmark on metaKinetic
In 2019 Oil & Gas and Mining industry spent more than $2.8 B in training Geosciences and Engineering…
Image Logs Untangled
Assuming that the overburden stress (Sv), is one of the three principal stresses, the stress tensor (representing the in-situ stress field)…
Microseismic Monitoring: DAS vs. Conventional Geophones (Downhole & Surface)
How does microseismic (MS) acquisition using DAS (Distributed Acoustic Sensing) compare with conventional Downhole or Surface using geophones?…
What you need to know about surface location resolution
The metaKinetic platform now has a simulation under passive seismic gallery that helps understanding some of the concepts…