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tectonic style
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  构造样式
    The dextral strike-slip tectonic deformation on both sides of the coastline in Huanghua Basin is discussed from aspects of tectonic style, fault combination, and sedimentary feature. The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.
    从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在,指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。
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  构造样式
    The dextral strike-slip tectonic deformation on both sides of the coastline in Huanghua Basin is discussed from aspects of tectonic style, fault combination, and sedimentary feature. The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.
    从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在,指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。
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  tectonic style
Similarly, the details of plate tectonic modalities (plate size, plate motion rate, plate thickness, tectonic style, irregular crustal growth, etc...) were different of modern plate tectonics.
      
The tectonic style of a terrestrial planet depends strongly on the mechanisms of heat release from the mantle through the lithosphere to the surface.
      
Today one of the main questions standing before geology of Venus is comprehension of tectonic style on surface of this planet.
      
These factorsinfluence the mechanical properties of the lithosphere across thediscontinuity, and ultimately the tectonic style of the NTD that can besupported.
      
Swath bathymetry and sidescan data, together with seismic reflection and geopotential data obtained during the GEODYNZ-SUD cruise, showed major changes in tectonic style along the margin.
      
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By analyzing and interpreting multi-channel seismic profiles, it is foundthat there are four tectonic styles, including buried hill style, extensive fault block,compressed anticline and dominoes faulted structure, associated with structural traps ofanticline type and fault block type which are mainly oil-gas traps in the Wan' anBasin of the South China Sea.

通过对大量多道地震剖面的解释和分析,认为南海万安盆地发育有潜山披覆、基底张性断块、挤压背斜和骨牌式构造等4类典型构造样式,并形成背斜型和断块型两类主要的构造圈闭,构成了盆地内重要的油气圈闭类型。

The dextral strike-slip tectonic deformation on both sides of the coastline in Huanghua Basin is discussed from aspects of tectonic style, fault combination, and sedimentary feature. The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover. The single shear model is used to explain the geological phenomenon: because of the dextral strike-slip movement during Cenozoic,...

The dextral strike-slip tectonic deformation on both sides of the coastline in Huanghua Basin is discussed from aspects of tectonic style, fault combination, and sedimentary feature. The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover. The single shear model is used to explain the geological phenomenon: because of the dextral strike-slip movement during Cenozoic, the NE-striking R shears were developed on both sides of the primary displacement zone (PDZ); and the co-action of NW-SE-striking extension and the SN-striking extension resulted in a discontinuous tectonic line on both sides of the coastline today.

从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在,指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。采用单剪模式解释了由于NNE向基底隐伏走滑带在新生代的右旋走滑活动,在主位移带(PDZ)的两侧产生了NE向的R剪切,R剪切受区域NW—SE向伸展和由走滑导致的SN向局部伸展的共同作用,导致了现今黄骅盆地中区海岸线两侧构造线不连续的现象。

 
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