Transition zones (TZ) are tricky areas for seismic exploration, since data can’t be acquired by the same techniques used for land or deep water surveys. These areas are characterized by rapid changes in water depths, tides, variation in sea bottom topography and sediments which impose constraints survey design and equipment. These dynamic, complex environments require tools and equipment that bridge the gap to ensure continuity of seismic information from land to shallow water to deep marine.View Products
What does it all mean? Vibroseis terms can be confusing, and there are many terms used in seismic acquisition today. This is exacerbated by the fact that, in some instances, the same term is used with a different meaning depending on the context it is being applied. Our team here at INOVA discuss vibroseis terminology and explains terms like fundamental ground force and peak ground force as well as other common terms used today.
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