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(1) The hanging wall of the pterygopalatine space, fora- men rotundum, inferior orbital fissure, pterygoid canal and its relationship with the sphenoidal sinus were dis- played on coronal section.

(2) The hanging wall block is relatively little disturbed , but the ore zone beneath bears abundant evidence of tangential movements.

(3) The prospective targets are distributed on the hanging wall of the Baiyin fault and the SOuthern Tala fault in the West sag of the sub-basin.

(4) If the relative movement of hanging wall and footwall is parallel to the strike of fault plane, it is a strike slip fault.

(5) On the hanging wall of the nappe (thrust), isoclinal folds are developed with the axial planes inclined to the north in association with imbricated thrusts dipping to the south.

(6) They connect the hanging wall of one fault to the footwall of another fault, and have special deforming feature, beside them on the hanging wall there are transverse anticlines.

(7) According to ore body characteristics and distribution(Sentencedict), NNW hanging wall transtension fracture and Paomagang Fm fade dolomitic gravel subarkose has great prospects.

(8) For dip-slip faults, there are two prominent effects: the rupture directivity effect and hanging wall effect.

(9) The faults within the strike-slip thrust belts occur as structure in sectional view, thus direct correlation of strata between the hanging wall and footwall is impossible.

(10) A series of small shear zones, which are parallel to the main deformation belt, are formed in the foot wall, while in the hanging wall ductile brittle normal faults are popular.

(11) Fault plane divides faulted rock into two blocks. The block above the fault plane is called hanging wall; the block below the fault plane is named footwall.

(12) Field of the hemisphere is clear that only small, giving induced a feeling of hanging wall.

(13) The research demonstrates a normal faulting tenacity shear zone with hanging wall westwardly sliding according to kinematics characteristics of the tenacity shear zone.

(14) So the fault on the cliff is a reverse fault because the red rock layer in the hanging wall has moved up relative to that in the footwall.

(15) If a fault has a vertical fault plane. How do we determine its hanging wall and footwall ?

(16) The northeast sag in the north depression was formed by fault-bend folding of the hanging wall of the north dipping listric Weihai normal fault caused by the northward movement of the hanging wall.

(17) Gudian structure was formed in the late period in the deposition of Nenjiang series in Early Cretaceous, by the dray dueing the uplift of the hanging wall of the Gudian fault.

(18) Therefore, the risk of fault rock burst when working face advances from the footwall to the fault itself is higher than that from the hanging wall to the fault itself.

(19) The experimental phenomena indicate that there are the maximal stress destruction points in the hanging wall and the footwall.

(20) Overthrusting occurs simultaneously with peak hydrocarbon generation, and thermal evolution of the source rocks in the hanging wall defers, while source rocks in the foot wall get mature rapidly.

(21) The results show that the stability of roof becomes poor with reduction of distance away from the fault whether the working face is mined in the footwall or hanging wall of fault.

(22) The hydrocarbon generating potential of source rock is weaker in the hanging wall and the heavier relatively in the lower plat of upper Paleozoic in the west margin belt.