tectonic subsidence中文是什么意思

• 构造沉降作用

• "tectonic"中文翻译    adj. 1.构造的；建筑的。 2.【生物学】构造的。 ...
• "subsidence"中文翻译    n. 1.沉淀；沉下，陷下。 2.平静，平息；减退，衰耗 ...
• "volcano-tectonic subsidence" 中文翻译 :    火山构造沉陷
• "subsidence" 中文翻译 :    n. 1.沉淀；沉下，陷下。 2.平静，平息；减退，衰耗。
• "tectonic" 中文翻译 :    adj. 1.构造的；建筑的。 2.【生物学】构造的。 3.【地质学；地理学】地壳构造上的，起因于地壳运动的。
• "acceleration of subsidence" 中文翻译 :    沉陷加速度
• "angle of subsidence" 中文翻译 :    边界角; 陷落角
• "anticyclone subsidence" 中文翻译 :    反气旋下沉
• "area of subsidence" 中文翻译 :    沉陷区; 下沉面积
• "atmospheric subsidence" 中文翻译 :    大气衰耗; 大气下沉
• "basinal subsidence" 中文翻译 :    盆形沉陷
• "block subsidence" 中文翻译 :    块体沉陷；块状断陷
• "bottom subsidence" 中文翻译 :    底板沉陷; 底部沉陷
• "caldera subsidence" 中文翻译 :    火口陷落
• "caldron subsidence" 中文翻译 :    火口陷落
• "cauldron subsidence" 中文翻译 :    顶盖沉陷; 火口沉陷; 火山沉陷; 火山口沉陷作用
• "center of subsidence" 中文翻译 :    沉降中心
• "centrifugal subsidence" 中文翻译 :    离心沉降
• "compression subsidence" 中文翻译 :    压缩沉陷; 压缩负荷沉陷
• "crustal subsidence" 中文翻译 :    地壳沉降
• "delayed subsidence" 中文翻译 :    延迟沉降
• "differential subsidence" 中文翻译 :    差异性沉降
• "earthquake subsidence" 中文翻译 :    震陷
• "elevation and subsidence" 中文翻译 :    升降作用
• "endogenetic subsidence" 中文翻译 :    内因沉降

• There is a close relation between the tectonic subsidence and the heat how in basins
  摘要盆地的构造沈降和热流演化具有密切的联系。
• The formation and evolution of the sequence stratigraphy of the yanchang formation are governed by slow tectonic subsidence , warm humid climates , sediment supply and lake - level fluctuations
  延长组层序地层的形成与演化主要受控于当时缓慢的构造沉降、温湿气候、陆源碎屑物源供给及湖平面升降等地质因素。
• One of the frontier recearch of basin analysis in recent years is to analyze the tectonic subsidence history of depositional basins which occur in orogens at different geohistory stage , and to discuss the geodynamic processes involved with the basins
  摘要对造山带各地史阶段的沉积盆地进行构造沉降分析，进而探讨其地球动力学过程，是近年来盆地分析的前缘研究之一。
• The tectonic subsidence curves on the southeastern margin of the yangtze plate are drawn out using of backstripping method for the basin formation and evolution . the basins located in the southern margin of the yangtze plate , in the basin dynamic computer simulation , is explored and constituted to be a typical foreland basin which is of not rather high mountain and thermal situation to be lower in this older orogeny belt
  在沉积盆地分析方面，基本查明扬子板块东南边缘早古生代被动大陆边缘沉积特征及沉积构造演化，同时运用反剥法技术对扬子板块东南大陆边缘沉积盆地形成，演化的构造沉降动力学进行探讨，运用计算机模拟方法，定量动力沉积学对扬子东南边缘奥陶纪到志留纪前陆地进行计算机模拟分析，探索并建立这个古老造山带前陆盆定量参数和动态定量模拟。
• Compared to the basins in east guangxi , the basin of north guangxi is characterized by lower depositional and tectonic subsidence rate during rifting , longer thermal subsidence , later inflexion point from rifting to foreland buckling , as well as later inflexion point separating stable stage from active stage during foreland - buckling
  但与桂东大瑶山地区相比，桂北兴安地区在裂陷阶段的沉积速率和构造沉降速率明显偏低；热沉降阶段的持续时间偏长；裂陷阶段与前陆挠曲阶段的分界拐点偏晚；前陆挠曲阶段，由构造宁静期的缓慢沉降向构造活动期的快速沉降转化的分界拐点也偏晚。