imbricate造句
1) The author finds out the imbricate thrust structure within low Jurassic series in Qidam basin Lenghu 5 fold core and considers the structure formed in late Yanshan movement.
2) The roof tiles imbricate.
3) On the section, the imbricate thrust zone is situated below the front margin of the triangular-zone structure, and they are overlapping distributed on plane.
4) The structural types mainly are fault-related folds, imbricate structure and fault delta zone.
5) The imbricate fan of thrusts and soft layer are main structure features distinguishing thrust-nappe structure in magma-tic body area.
6) Results Normal imbricate epitheliums and LSIL and HSIL and cancer cells were recognized and classified, the recognition rate of training set was 98.29%,[http:///imbricate.html] the recognition rate of test set was 96.57%.
7) Under compression, two kinds of main fault combination were formed in the Kalpin fault uplift:imbricate thrust sheets and tectonic windows.
8) The results indicate that the occurrence of Baguamiao gold deposit is dually controlled by its brittle-ductile shear zone, imbricate up thrust fault and its induced structure.
9) The rhizome is short, thick shape, cylinder, by most imbricate arrangement scaled leaf.
10) The Yanqi Basin formed in Mesozoic and Cenozoic, is a hydrocarbon bearing basin, which has not only an imbricate , back, ramp thrust structural styles, but also a wrench structural style and so on.
11) In Baiyangping ore concentrated area, the master mineralization epoch is in Lanping basin became imbricate down-warped, strike-slip and pull-apart basin.
12) The structural system of nappe consists of several overthrust fracture belts, thrust sheets and thrust slices, and master fault and secondary fault form an imbricate structure.
13) The middle(early Himalayan)is the main deformation, characterized by the imbricate thrust structure system, whose west zone shows thrusting from SW toward NE.
14) In fact, this fault dip with depth smaller surface phenomenon, they are also important features for Longmen Mountain imbricate thrust faults.
15) They separated the forearc basin into several sub-basins, which imbricate in the background of a forearc basin with sedimentary characteristics of the piggyback basin.
16) From north to south, several tectonic belts can be distinguished:front compressive detachment belt, overturned thrusting belt, sheeted thrusting belt and imbricate thrusting belt.
17) The formation of the basin might be probably related to crustal extension controlled by a series of imbricate, low-angle, rooted shear faults.