exists and is an alternate of . This depends on how detailed you want to go, but the answer you're probably going for is transcription. This is broken up into many smaller steps that make up transcription to unzip the DNA, create the mRNA, etc. DNA goes through transcription to make mRNA (messenger RNA). mRNA is translated via tRNA in ribosomes to make proteins.
So-called Wide-Azimuth acquisition is increasingly. used in an attempt to overcome such problems (Figure 1). Wide Azimuth seismic follows a very simple strategy - for. each receiver layout a large range of short to long offset. source positions are used over a large range of source-receiver. azimuths.
The seismic strain-rate tensor for shallow-focus earthquakes along the Central America volcanic arc since 1700, has a compressive eigenvector with a magnitude of 0.7 Ã 10 â8 year â1, and oriented in a 357Â° azimuth. The extensive eigenvector is oriented in a 86Â° azimuth, with a magnitude of 0.82 Ã 10 â8 year â1.arthquakes along the grabens of northern Central America yield a seismic strain-rate tensor whose extensive eigenvector has a magnitude of 2.4 Ã 10 â8 year â1, oriented in a 109Â° azimuth. Magnitude and direction are similar to those of the extensive eigenvector for earthquakes along the volcanic arc.