拆离
1.It formed owing to the regional stretchingproces of the end of Mesozoic Era the beginning of cenozoic Era,the direction of the extension de- tachment is the east of Eastnorth.
2.(2)The above mentioned detachment is characterized by wedge with negative velocity gradient (shown with LVL) above R1 interface between Samada and Dagyi.
3.After studying the macroscopic and microcosmic features, the authors discussed the genetic mechanism of the conglomerate.
4.The paper gives a mechanical and history analysis on the characteristic of Laojunshan metamorphic core complex in southeastern Yunnan and its structural environment, and considers that metamorphic core complex is actually a nuclear column of a vortex structure, which was caused by the Wenshan—Malipo strike-slip fault.
5.The large-scale composite ductile shear zone around Laerdun Daban is analyzed into three stages including horizontal dispatch, uplift by compression and magrnatic intrusion, and dextral strike-slip ductile shearing, respectively of late Early Paleozoic to early Late Paleozoic, Late Devonian, and Permian-Triassic ages.
6.The Mofanggou gold deposit, stratoid in form, occurs in Early Cambrian Zhushadong Formation which overlies the principal detachment-slip zone between Cambrianstrata and Archaeozoic gneissose granodiorite or Palaeoproterozoic adamellite.
7.Finally, it concluded 1) in our country, there are existing just sell-offs and equity carve-out, and it is difficult to spilt-offs totally;
