Interpreting a geological map - with faults

  Рет қаралды 6,704

Rob Butler

Rob Butler

Күн бұрын

Пікірлер: 7
@nadiasourez8560
@nadiasourez8560 2 жыл бұрын
Tank you. For your interpretation very helpful
@vijaymare5116
@vijaymare5116 2 жыл бұрын
It very use ful sir keet upload more videos
@hassanaleem2871
@hassanaleem2871 2 жыл бұрын
really very useful. loved it
@hassanaleem2871
@hassanaleem2871 Жыл бұрын
I see that this is a superb example to understand various key concepts while drawing subsurface profiles, although I am curious regarding the assumptions concerning varying thicknesses in a fault bounded basin (fold-thrust-belt), where more often than not, I would expect more thickness on the hanging wall of the normal fault (and footwall in case of reverse fault)? for example, the conglomerate layer in given example
@robbutler2095
@robbutler2095 Жыл бұрын
I'm not sure I understand your question - the example shows listric normal faults so yes indeed, stratal packages thicken on the hangingwall sides of faults. As you note, this relationship is reversed (thicker on footwall side) for thrust faults...
@hassanaleem2871
@hassanaleem2871 Жыл бұрын
@@robbutler2095 thanks for explicit comment, I was looking at the thicknesses of conglomerate layer in the two fault hanging walls, where in fault Y, it has more thickness compared to the fault X, and both are normal faults, but looking at the order of faulting happened, I got to understand it. Thanks
@salihal-awami8465
@salihal-awami8465 2 жыл бұрын
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