GLKM (Geodesic Clustering of Localized Model) is a method used in seismic imaging to focus on specific localized features within the subsurface by clustering seismic data based on common properties. It helps in isolating and analyzing smaller-scale geological features such as faults, fractures, and fluid pathways for more detailed subsurface characterization.
why are seismic dampers important
Seismic stratigraphy is based on the principles of using seismic reflections to interpret sedimentary layers, identifying key seismic surfaces such as unconformities, and correlating these surfaces across different seismic profiles. It also involves understanding the relationship between seismic reflection patterns and depositional processes, as well as recognizing seismic facies changes to interpret sedimentary environments.
A seismic trace is a graphical representation of seismic data collected during seismic surveying. It shows how the amplitude of seismic waves changes over time and can be used to identify subsurface structures like rock layers or hydrocarbon reservoirs. Seismic traces are essential in geophysics for interpreting subsurface geology.
Geologists study seismic waves to understand the characteristics of subsurface rock formations.
A seismic gap
(not seismic, seismic wave)Seismic waves are waves of energy that travel through the earth.
(not seismic, seismic wave)Seismic waves are waves of energy that travel through the earth.
why are seismic dampers important
Seismic shifting is the shifting of the earth's crustal plates, causing seismic activity.
Seismic plan is to produce and maintain seismic-resisting system components in construction work.
why are seismic dampers important
She hits me like a seismic shake! The seismic measurement systems are very sensitive.
Seismic stratigraphy is based on the principles of using seismic reflections to interpret sedimentary layers, identifying key seismic surfaces such as unconformities, and correlating these surfaces across different seismic profiles. It also involves understanding the relationship between seismic reflection patterns and depositional processes, as well as recognizing seismic facies changes to interpret sedimentary environments.
It is possible to have a seismic wave without having an earthquake. Any wave moving through the ground is a seismic wave, and all earthquakes are seismic waves. But seismic waves can be created by volcanic action, landslides, meteor strikes or the like. Though all earthquakes are seismic waves, not all seismic waves are earthquakes.
Seismic waves are associated with earthquakes.
Seismic Seconds was created in 199#.
A seismograph can locate a seismic wave.