the oblique slip fault is a movement that has a combination of normal and strike-slip fault
i have no clue but goog luck ive looked everywere bing Google this yahoo answers but what i don't get is theres like nothing about oblique faults but theres fat kids dancingg and sneezing pandas? stupid...
Rocks can move along a fault in three main ways: 1) They can slide past each other horizontally in a strike-slip motion, 2) They can move vertically in a dip-slip motion, either upwards (reverse fault) or downwards (normal fault), or 3) A combination of strike-slip and dip-slip motion can occur in oblique faults.
A strike-slip fault has side-to-side movement where the blocks move horizontally past each other. This type of fault is classified as either right-lateral or left-lateral, depending on the direction of movement relative to an observer standing on one of the blocks.
The main difference between a dip-slip fault and a strike-slip fault is the direction of movement. In a dip-slip fault, the movement is primarily vertical along the dip direction of the fault plane, either up or down. In a strike-slip fault, the movement is primarily horizontal along the strike direction of the fault plane, either to the left or right.
In a dip-slip fault, the movement is primarily vertical along the fault plane, either up (reverse fault) or down (normal fault). In a strike-slip fault, the movement is primarily horizontal along the fault plane, with minimal vertical movement. Both types of faults are caused by tectonic stresses in the Earth's crust.
the oblique slip fault is a movement that has a combination of normal and strike-slip fault
A fault that is a combination of dip-slip and strike-slip movements
There are 6 types of fault lines. Strike-slip faults, dip-slip faults, oblique- slip faults, listric faults, ring faults, and synthetic and antithetic faults.
i have no clue but goog luck ive looked everywere bing Google this yahoo answers but what i don't get is theres like nothing about oblique faults but theres fat kids dancingg and sneezing pandas? stupid...
Rocks can move along a fault in three main ways: 1) They can slide past each other horizontally in a strike-slip motion, 2) They can move vertically in a dip-slip motion, either upwards (reverse fault) or downwards (normal fault), or 3) A combination of strike-slip and dip-slip motion can occur in oblique faults.
A strike-slip fault has side-to-side movement where the blocks move horizontally past each other. This type of fault is classified as either right-lateral or left-lateral, depending on the direction of movement relative to an observer standing on one of the blocks.
Dip-Slip fault is a bedding fault and its pattern is En-Echelon, while Strike Slip fault is strike fault and its pattern is Parallel.
No. It is a strike-slip fault.
The Hayward Fault is a Strike-slip Fault.
The main difference between a dip-slip fault and a strike-slip fault is the direction of movement. In a dip-slip fault, the movement is primarily vertical along the dip direction of the fault plane, either up or down. In a strike-slip fault, the movement is primarily horizontal along the strike direction of the fault plane, either to the left or right.
Strike slip fault - Look it up!
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