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tectonic pattern中文是什么意思

  • 構(gòu)造模式
  • 構(gòu)造型式
  • 構(gòu)造形式

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  • 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
    盆地內(nèi)部的構(gòu)造樣式以自盆地邊緣至中心以此形成背斜構(gòu)造為顯著特徵,背斜兩翼多發(fā)育逆斷層,構(gòu)成“兩斷夾一隆”的構(gòu)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
    為該巖系的時(shí)代歸屬、地層劃分及與鄰區(qū)對(duì)比提供了古生物證據(jù),也為研究該區(qū)巖相古地理、大地構(gòu)造格局提供了可靠資料。
  • 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:本文介紹了盈江盆地的構(gòu)造格架及構(gòu)造分區(qū)、晚第三紀(jì)盆地沉積特征,對(duì)盆地蓋層發(fā)育的氧化帶進(jìn)行分類,論述了氧化帶的發(fā)育特征及其與鈾礦化的關(guān)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
    根據(jù)中生界上侏羅統(tǒng)和下白堊統(tǒng)地層和控盆斷裂分布分析,中生代晚期晚侏羅早白堊世郯廬斷裂帶的左旋走滑平移導(dǎo)致郯廬斷裂帶以西自北向南發(fā)育了3個(gè)北西向斷塹系,即北部的渤海斷塹系中部的濟(jì)陽(yáng)斷塹系和南部的魯西南斷塹系。從區(qū)域資料綜合分析,渤海灣盆地的基本格局是早第三紀(jì)以來(lái)的新生代盆地格局。渤海灣盆地的形態(tài)構(gòu)造和沉積特征及熱流值分布表明該盆地在新生代為拉分盆地。
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