The slip vector can be evaluated qualitatively by studying any layer resistance folding that may be visible on both sides of the fault. [12] Drag bending is a convolutional zone near an error, probably caused by resistance to friction to motion on the defect. [13] The direction and magnitude of uplift and throw can only be measured by finding common intersections on both sides of the fault (called puncture points). In practice, it is usually only possible to find the direction of error slippage and an approximation of the lifting and throwing vector. Reverse slip defects result from horizontal compressive forces caused by shortening or contraction of the Earth`s crust. The hanging wall moves on and above the foot wall. Thrust errors are inverse errors that fall to less than 45°. Thrust disturbances with a very small immersion angle and a very large total displacement are called thrusts or detachments; These are often found in severely deformed mountain belts. High-thrust faults are characteristic of the boundaries of compressive tectonic plates such as those created by the Himalayas and subduction zones along the west coast of South America. Synthetic and antithetical are terms used to describe minor errors associated with a larger error.

Synthetic errors fall in the same direction as the main error, while antithetical errors fall in the opposite direction. These errors may be accompanied by flyby anticlines (e.g. Niger Delta structural style). A fault plane is the plane that represents the fracture surface of an error. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault track is also the line commonly drawn on geological maps to represent a fault. [3] [4] An example of a fault with valuable porphyry copper deposits is the Domeyko fault in northern Chile with deposits at Chuquicamata, Collahuasi, El Abra, El Salvador, La Escondida and Potrerillos. [28] Further south in Chile, the porphyry copper deposits Los Bronces and El Teniente are located at the intersection of two fault systems. [27] Geometrically, it is a cube forced into a diamond by the fault.

And is it just to punish me for what is my misfortune and not for my fault? And if he left me and went to America, it`s your fault. In normal dip-slip faults, rock masses compress vertically on top of each other and moving rock moves downwards. They are caused by the elongation of the earth`s crust. If they are stiff, they are called high-angle defects, and if they are relatively flat, they are defects of low angle or detachment. The flat segments of the shear fault planes are called flat surfaces, and the inclined thrust sections are called ramps. As a rule, thrust disturbances move within formations by forming shallow formations and climbing sections with ramps. Error can mean „guilt“ as a noun or verb. When you say, „It`s my fault,“ you accept guilt.

Well, at least they can`t blame you for telling the truth. A mistake can be a gap — everyone has flaws because no one is perfect — or a crack in the earth`s crust, like the San Andreas fault. In sports like tennis, a mistake is an illegal shot of the ball, usually when it lands off the court. It is not because we do not recognize the guilt of this plan, or rather this lack of plan. Defect slippage can smooth the walls of the fault plane and mark them with strips called smooth surfactants, or crush them into a fine-grained clayey substance known as fault joint; If the gravelly rock is relatively coarse, it is called a fault breach. Sometimes the beds adjacent to the fault plane bend or bend because they resist slippage due to friction. Areas with deep sedimentary rock cover often show no surface evidence of the underlying fault. Errors can be vertical, horizontal, or tilted at any angle. Although the angle of inclination of a particular fault plane tends to be relatively uniform, it can vary greatly from place to place along its length.

When rocks slide over each other during faults, the upper or upper block along the fault plane is called a hanging wall or head wall; The block underneath is called the foot wall. The fault stroke is the direction of the intersection line between the fault plane and the earth`s surface. The immersion of a fault plane is its angle of inclination, measured from the horizontal. The two sides of a non-vertical fault are called a hanging wall and a foot wall. The hanging wall is above the fault plane and the foot wall below. [14] This terminology comes from mining: while working on a tabletop ore body, the miner stood with the foot wall under his feet and with the wall hanging above him. [15] These terms are important for distinguishing between different types of slippage errors: reverse errors and normal errors.