构造作用 meaning in Chinese
tectinization
tectogenesis
tectonic action
tectonic process
tectonism
tectonization
Examples
- In summary , this paper indicates that yanshanian tectonic process of xiaoqinling aera give priority to deformation of thrusting and napping and coexist with deformation of extending and pullapart . taihua group was rapid uplifted in yanshanian that resulted in both compressive thrusting and napping and extending process
结合燕山期秦岭造山带构造特征和深部岩石圈演化特征，认为小秦岭燕山期构造作用主要表现为以挤压逆冲推覆构造作用为主和以伸展拉张作用为辅的特征。 - The essential elements and process of gas reservoir formation of ordovician in ordos basin have been annalysed systematicly and scientificly by means of the theory and method of organic geochemistry and tectonic geology in this dissertation . the several advanced techniques , such as gas generation thermal simulation , on - line individual gas compounds carbon isotope determination ( py - gc - c - ir - ms ) , the analysis technique of light hydrocarbons and biomarkers in natural gas , gas migration simulation and gas carbon isotope determination in fluid inclusions , have been applied to focuse on the study of the gas generation mechanism of souce rock , correlation between gas and source rock , reservoir formation history , migration direction , charging road in detail
应用有机地球化学和构造地质学理论和方法对鄂尔多斯盆地奥陶系天然气地质研究中薄弱环节成藏要素和作用进行了系统科学分析。利用烃源岩生气定量热模拟技术、热模拟在线碳同位素实验技术、气体轻烃和生物标志物分析技术、运聚成藏物理模拟技术和包裹体中碳同位素分析技术等多种先进的实验技术对烃源岩的生气机理、气源和混合比、成藏史、充注路径、运移方向和构造作用与成藏关系等问题进行了深入的研究，在前人研究的基础上，经过本次大量的实验分析和综合研究，提出了一些新的认识。 - ( 6 ) the comparative study of stable isotope respond between qiangtang basin and middle - upper jurassic epoch section in the central italy indicated that the global sea level presented a general rising trend in five rise and fall cycles in middle - late jurassic epoch , whereas it presented a general falling trend of sea level in five rise and fall cycles in the studied area . regional tectonism and global sea level change play a controlling role in the relative sea level change of the studied area
( 6 )羌塘盆地与意大利中部中?晚侏罗世剖面稳定同位素响应的对比研究表明，中?晚侏罗世全球海平面表现为在五次升降旋回中呈现上升的总趋势，而在研究区表现为在五次升降旋回中海平面下降的总趋势，区域构造作用和全球海平面变化共同对研究区相对海平面变化中起到控制作用。 - Depositional cycles on basin scale have been interpreted as the result of depositional response to tectonism such as episodic rifting , polyphasic compressive flexural subsidence and reversion , and differential subsidence of fault blocks ; while the formation of high frequency sequences was attributed to variation in lake level and sediment supply
盆地规模的沉积旋回多是盆地幕式裂陷、多幕挤压挠曲沉降、多期构造反转、断块差异沉降等构造作用的沉积回应；高频层序单元的发育则主要与湖平面和沉积物供给量的变化有关。 - By physiognomy feature , it could be divided into three types of thermal structure : positive dome model , negative collapse model and border dome core collapse model . based on the depth degree or magma - thermal influenced , it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model , superficial volcano eruption hydro - thermalism and hypabyssal intrusive model , thermal anticline ( thermal dome ) model , mid - deep intrusive model , deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure . there are many interaction system could be induced into a systematic thermal interaction , include : ocean - continent system , basin - mountain interaction , superficial and mid - deep crust - mantle interaction , crust - mantle commingle interaction , vertical thermal interaction ( delamination ) etc .
依据地貌形态分为三类：正向穹窿型、负向塌陷型、边隆核陷型：依据岩浆-热力作用影响的深浅程度或深度分为五类： (古)地热异常群集区、表浅层火山喷发-热液活动与浅成侵入型、热力背斜(热穹窿) 、中深层侵入型、深部地幔(地壳)热柱型；提出了热力构造作用空间分布的理想模式，将洋陆系统、盆山作用、浅表与中深部壳幔作用、壳幔混合、垂向热力作用(拆沉)等纳入一个整体统一的热力作用系统中，为盆地动力学研究打开了一个新窗口；研讨了热力构造研究方法。