Mount Emei to step onto the Mount Emei Yangtze platform fold belt broken arch and figuratively, in western Sichuan, Sichuan Taiwan Taiwan depression, is a fault-block mountain. Its structure more complex. The main structure now be summarized as follows:
Fold
Mount Emei anticline is located in Zhang ditch - Hong Chunping area, north-south axis, about 7 km. View of the northern end was heart Um faults and oblique faults Temple thousands of years can not be extended north; the southern end of Mount Emei fault oblique and can not be extended south. Of its nuclear department relief, the oldest exposed granite rock of Mount Emei. Wings asymmetrical, West wingspan of cloth about 18 kilometers, the exposed strata of the Sinian - Lower Triassic Jialingjiang inclination of 10 to 12 degrees; East wingspan of cloth about 5 kilometers, the exposed strata are Sinian - Next Tertiary inclination of 16 ~ 50 degrees, the newly opened temple to the east of multi-strata have been reversed. For a Western tilt of the Xiewai axial anticline.
Osmanthus field syncline (also known as Temple syncline years) is located in Chun-yang Palace - Osmanthus field area. Axial North West, about 30 kilometers north west as a whole was Kei-like pitching. By ring tunnel fault, gray Jinchanggou dislocation of two: South-eastern section of the market from the Chun-yang palace to the sweet-scented osmanthus, nuclear Ministry of narrow, its formation date for the next Triassic Jialing Group. Wings for the Lower Triassic strata Feixianguan Formation - Upper Permian Emeishan basalt. North, East Wing, 5 ~ 20 degree angle from the rapid change from steep, southwest wing affected by faults reversal often occurs in the vicinity of Chun-yang Palace syncline looked up and convergence disappeared; the north western section from the foot to Hongyan Huang Wan, nuclear department relief, 6 ~ 45 degrees angle wings. Syncline quickly aside the gradual transition to monoclinic.
Yak Mountain anticline (also known as Waduan Mountain anticline) is located in Long openings?? Ray rocks along the axial North West, about 12 km. Nuclear Department of the oldest exposed strata are Lower Permian Maokou. Wings were exposed Emeishan Basalt Group - Jurassic. The northern section of the Blackwater Kong to mine rock, more symmetrical wings, dip 15 to 50 degrees; the middle and southern section by Cattle Fu Husi Shan faults and fault effects of asymmetric wings, Nancy wing angle 35 ~ 60 degrees, North East Wing angle of 60 ~ 75 degrees. Nuclear Division near the anticline dip steepened and gradually to turn.
Fault
Mount Emei Mount Emei fault is found in south east. In this regional context, from the southwest Yangcun shop near the north east longitude Zhang Shan, to the Emeishan City Central District. The district about 40 kilometers towards the north east, north-west orientation, cross section, wavy. 45 ~ 70 degrees inclination. North West plate thrust plate at the top of the South East. North-West dish is often derived growth drag folds and faults, south east partial inverted plate stratigraphy, and associated a series of small folds and small faults. Breaking away from the biggest part of the fault in its nuclear department, breaking away from the more than 3,500 meters, that is, North West, Mount Emei granite thrust plate on the South East intraday Triassic Mine Group slope above the mouth. The North East, which is located in Emei rift basin north-west edge, most of the Quaternary cover, showing intermittent outcrops. Such as: liangshuijing, 40 hospitals and other places. Its performance for the North West, the Upper Cretaceous guankou disk group on the South East of thrust plate on the third line and make it reverse.
View Heart Hermitage fault south east on the newly opened Temple, by Chun-yang palace and watch mind slope, north west until YU Tian son, towards the north west, about 15 kilometers. Nancy section sloping angle of 65 ~ 75 degrees. Nancy plate relative increase in the performance of the thrust fault. That the fault is north-east and east-west-trending faults cut the number of paragraphs. The southern section of newly opened Temple Tai E Mountain Temple, Mount Emei anticline developed in the East Wing. By Nancy thrust plate, resulting in north-east disk formation to turn. Temple to the middle of beef heart Tangshan, developed in the southwest wing of syncline sweet-scented osmanthus field, and oblique Emei anticline. Nancy set up the formation of heart rate by drag anticline, north-east disk formation inverted, breaking away from the 1,500 meters. Northern section of the dam to the YU Tian Asako son, the main fault in the Triassic, the southwest plate up to develop into a small drag folds.
Temple thousands of years in the small fault south east ditch, the North West until God hexagrams Hill. Towards the north west, about 13 kilometers, is the concept of mind derived Om fault thrust fault in the same direction. Nancy dumping section inclination of 50 degrees. Southern Section-off in the Lower Permian - Lower Triassic Feixianguan group, the two strata are reversed. Mid-off on the Upper Permian Emeishan basalt - Lower Triassic Feixianguan group, the two strata reversed. North off the main fault in the Triassic.
Elders from the beginning of Dian Ping fault near the north by Xianfeng Temple, south 3 Bay post. Nearly north-south direction, about 10 km. Section east tilt, inclination of 85 degrees. In addition to peak near the middle of Tianchi expressed as normal faults, south, the northern section are reverse faults. In the early hall area, three sections of the East disc Dengying dolomite and West set Qiongzhu Temple Group Lower Cambrian siltstone offset, broken away from about 80 meters, Xian Huang Taiwan side visible fault breccia. Ping in the vicinity at the Four Seasons, the East and West plate granite plate Emeishan Dengying bis offset, Dengying dolomite visible drag phenomenon. Temple thousands of years in the small fault south east ditch, the North West until God hexagrams Hill. Towards the north west, about 13 kilometers, is the concept of mind derived Om fault thrust fault in the same direction. Nancy dumping section inclination of 50 degrees. Southern Section-off in the Lower Permian - Lower Triassic Feixianguan group, the two strata are reversed. Mid-off on the Upper Permian Emeishan basalt - Lower Triassic Feixianguan group, the two strata reversed. North off the main fault in the Triassic.
Elders from the beginning of Dian Ping fault near the north by Xianfeng Temple, south 3 Bay post. Nearly north-south direction, about 10 km. Section east tilt, inclination of 85 degrees. In addition to peak near the middle of Tianchi expressed as normal faults, south, the northern section are reverse faults. In the early hall area, three sections of the East disc Dengying dolomite and West set Qiongzhu Temple Group Lower Cambrian siltstone offset, broken away from about 80 meters, Xian Huang Taiwan side visible fault breccia. Ping in the vicinity at the Four Seasons, the East and West plate granite plate Emeishan Dengying bis offset, Dengying dolomite visible drag phenomenon.
Yak Mountain fault developed in the Ministry of Cattle Mountain anticline core. Towards the north west and south east on the maliu Bay, through the two estuaries, Zhang Shan, north west Liang Ping, about 9 km. Nancy dumping its cross-section, inclination 60 degrees. 2 contacts close, the two can be seen near the mouth of Lower Permian limestone Maokou fragmentation phenomena occur. Is a thrust fault and shear.
Big E Mountain Temple fault west ditch stalagmite east Huayan Monastery towards things, about 5 km. Cross Mount Emei anticline and syncline osmanthus field and off the wrong concept of mind Um, and thousands of years Temple 2 fault. The north drive to the west, south east disc dislocation for slip-thrust fault. East North disk Feixianguan Group, Jialing Group and other local reversal formation. Watertight nature of the fault good diving along the surface exposed cross-section up to form Mount Emei Quan Yu Ye
