Hanging Wall Anticline Structure

This structure was formed in the indosinian yanshanian period characterized by being early formed well inherited and highly uplifted xu et al 2009.

Hanging wall anticline structure.

The anticline is cut by two distinct sets of normal faults. The two sides of a non vertical fault are known as the hanging wall and footwall. When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him. Hanging wall synonyms hanging wall pronunciation hanging wall translation english dictionary definition of hanging wall.

Amplitude height of structure 7. The highest point on a doubly plunging anticline or any geologic structure for that matter is called the culmination an elongate dome which developed as the sediments were being deposited is referred to as a pericline. Which of the following result from tensional stress on rocks. Such faults are typically regional in nature and develop as a response to extensional collapse of a passive continental margin i e.

A dip slop fault in which the hanging wall has moved down relative to the footwall is referred to as a fault. The mass of rock overlying a mineral deposit in a mine. Drill intersected significant mineralization in the hanging wall zone hinge zone drilling encounters high grade gold mineralization encountered high grade gold values in the upper limb portion of the fold structure the axial plane of a large scale anticline fold axis which plunges at a shallow angle to the north. Niger delta mississippi delta.

An anticlinorium is a series of anticlinal folds on a regional scale anticline. The hanging wall has slid down while the footwall has slid up along the fault. In an anticline the oldest beds the ones that were originally underneath the other beds. Joints are the most commonly observed structure at the earth s surface.

Wavelength width of structure from anticline to anticline 6. Sfr is the sea floor reflector. A rollover anticline is a syn depositional structure developed within the downthrown block hanging wall of large listric normal faults. The block above the fault is the hanging wall nothing to do with movement.

This terminology comes from mining. The beds dip toward a central point and the youngest rocks are exposed in the center of the structure. The center of an anticline or syncline is marked. The hanging wall occurs above the fault plane and the footwall occurs below it.

Growth faults which were active during the deposition of the mapped hanging wall sequence black and younger conjugate faults grey that post date the deposition of the imaged sequence.