tectonic pattern meaning in Chinese
构造模式
构造型式
构造形式
Examples
- The tectonic style inside the basin is characterized by occurrence of anticlines from the margins to center of the basin , with two limbs mostly starting from reverse faults , developing a tectonic pattern of two faults sandwiching an uplift
盆地内部的构造样式以自盆地边缘至中心以此形成背斜构造为显著特徵，背斜两翼多发育逆断层，构成“两断夹一隆”的构造格局。 - It is the first time to discover the early paleozoic strata based on reliable fossils , which not only provides evidence to its age ascription , classification of the strata and its correlation to adjacent areas but also offers data to lithofacies , palaeogeography and tectonic pattern of studied area
为该岩系的时代归属、地层划分及与邻区对比提供了古生物证据，也为研究该区岩相古地理、大地构造格局提供了可靠资料。 - Abstract : this paper introduces the tectonic pattern and tectonic division , sedimentary features of late tertiary , and the classification of the oxidation zone in sedimentary cover , and discusses development features of the oxidation zone and its relationship with uranium mineralization in yingjiang basin
文摘:本文介绍了盈江盆地的构造格架及构造分区、晚第三纪盆地沉积特征，对盆地盖层发育的氧化带进行分类，论述了氧化带的发育特征及其与铀矿化的关系。 - Based on the analysis of distribution of upper jurassic and lower cretaceous strata and basin - controlled faults , tanlu fault zone strike slip to develop the three nw - trending grabens from north to south western to tanlu fault zone in late jurassic and early cretaceous , which are bohai graben , jiyang graben and luxinan graben . based on the analysis of regional geology , the basic tectonic pattern of bohai basin is the cenozoic basin pattern since early paleogene . the outline , structure , deposit characteristics and heat flow distributions show that the basin is pull - apart basin in cenozoic time . the tectonic evolution pattern can be reconstructed based on the analysis of cenozoic strata , deposit thickness , location and activity of basin - controlled faults in the different depresses in bohai basin . the characteristics of structure and depositment in this mesozoic and cenozoic time show that bohai basin is a mesozoic and cenozoic composite basin
根据中生界上侏罗统和下白垩统地层和控盆断裂分布分析，中生代晚期晚侏罗早白垩世郯庐断裂带的左旋走滑平移导致郯庐断裂带以西自北向南发育了3个北西向断堑系，即北部的渤海断堑系中部的济阳断堑系和南部的鲁西南断堑系。从区域资料综合分析，渤海湾盆地的基本格局是早第三纪以来的新生代盆地格局。渤海湾盆地的形态构造和沉积特征及热流值分布表明该盆地在新生代为拉分盆地。