4,5 Km/s
In seismic investigations, the velocity of hard basalt is expected to be high due to its dense and strong nature. Basalt typically has high seismic velocities because of its mineral composition and compactness, which allows seismic waves to travel quickly through it. Understanding the velocity of hard basalt helps geoscientists interpret subsurface structures and properties, such as identifying boundaries between different rock layers or the presence of faults.
Average velocity is defined as the change in position of an object divided by the time taken to undergo that change. It gives a measure of how fast an object is moving in a particular direction over a given time interval. Mathematically, it is represented as: average velocity = (final position - initial position) / time.
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
The seismic discontinuity at the base of the crust is known as the Mohorovičić discontinuity, or Moho for short. It marks the boundary between the Earth's crust and the underlying mantle, where seismic waves experience a sudden change in velocity.
The crust-mantle seismic discontinuity was discovered by Yugoslav seismologist, Andrija Mohorovičić, in 1909 through his observation of seismic waves. This discontinuity marks the boundary between Earth's crust and mantle, characterized by a sudden increase in seismic wave velocity.
non optimal regional velocity applied to your seismic data
For the instantaneous value of average velocity, average speed and average velocity are equal.
In seismic investigations, the velocity of hard basalt is expected to be high due to its dense and strong nature. Basalt typically has high seismic velocities because of its mineral composition and compactness, which allows seismic waves to travel quickly through it. Understanding the velocity of hard basalt helps geoscientists interpret subsurface structures and properties, such as identifying boundaries between different rock layers or the presence of faults.
Velocity is speed and its direction. Average velocity is average speed and its direction.
The velocity model in seismic imaging is important because it helps determine how seismic waves travel through the subsurface. This impacts the accuracy of subsurface imaging because variations in velocity can distort the images produced, leading to potential errors in interpreting the subsurface geology. A precise velocity model is crucial for accurately mapping underground structures and identifying potential resources.
Always.
velocity is a vector and speed is scalar. Velocity has magnitude and directions, with magnitude being speed. The magnitude of average velocity and average speed is the same.
The speed of something in a given direction.
Average velocity can be calculated by dividing the displacement (change in position) by the time interval. The formula for average velocity is average velocity = (final position - initial position) / time interval.
The average velocity over an time interval is the average of the instantaneous velocities for all instants over that period. Conversely, as the time interval is reduced, the average velocity comes closer and closer to the instantaneous velocity.
The instantaneous velocity is the limit of the average velocity, as the time interval tends to zero. If you are not familiar with limits, basically you make the time interval very small and calculate the average velocity.
The cost of a ton of shale can vary depending on factors such as location, quality, and market demand. On average, the price of shale can range from $30 to $100 per ton.