tectonic uplift中文是什么意思

• 构造上升

• tectonic    adj. 1.构造的；建筑的。 2.【生物学】构造的。 ...
• uplift    vt. 1.举起，提起。 2.打起(精神)，发扬(优良品 ...
• uplift    vt. 1.举起，提起。 2.打起(精神)，发扬(优良品德)，鼓起(干劲)。 3.提高(社会地位)。 4.【地质学；地理学】使(地面)上升。 n. 1.举起，抬起。 2.【地质学；地理学】隆起。 3.〔美国〕(优良品德的)发扬，(精神的)高涨，(感情的)激发；进步。 4.〔口语〕(使胸部鼓起的)乳罩 (＝ uplift brassiere)。 an uplift worker 热心社会工作的人。 n. -er
• tectonic    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。
• anticlinal uplift    背斜隆起
• basement uplift    基底隆起
• block uplift    断块上升作用
• buoyant uplift    漂浮上升作用
• central uplift    中央隆起
• differential uplift    差异隆起; 差异上升
• domal uplift    穹状隆起
• epeirogenetic uplift    造陆隆起
• epeirogenic uplift    造陆上升
• fennoscandia uplift    芬诺斯堪的亚地块隆起
• hydraulic uplift    静水浮托力
• hydrostatic uplift    静水浮托力; 静水上托力
• land uplift    地面隆起
• linear uplift    线状隆起
• marginal uplift    边缘隆起
• net uplift    净上升
• orographic uplift    地形抬升
• regional uplift    区域抬升; 区域性隆起
• residual uplift    残留隆起
• salt uplift    岩盐隆起
• seepage uplift    渗透扬压力

• Tectonic uplift of the cenozoic era in the qinling range
  秦岭新生代构造隆升研究
• The effects of cenozoic tectonic uplift on earth surface chemical weathering and global climate change
  新生代构造抬升对地表化学风化和全球气候变化的影响
• The formation and evolution of sequence stratigraphy of middle - upper jurassic series is affected by change of global sea level , tectonic uplift and subsidence , sedimentary supply and climate conditions
  中?上侏罗统层序地层的形成演化受全球海平面变化、构造隆升与沉降、沉积物供给以及气候条件的综合影响。
• To reconstruct the evolution and variability of the east asian monsoon during the late cenozoic on millennial , orbital and tectonic time scales . 3 . to identify and better understand the links between tectonic uplift , erosion and weathering hemipelagic deposition , and climate change , including the evolution of the asian monsoon and the neogene global cooling
  Odp184航次1999年2月至4月间在中国南海进行钻探取样，通过钻取半远洋沉积，以期说明南海的新生代历史，包括它的生物地层学、岩石地层学、年代学、古气候学和古海洋学；重建千年级的晚新生代东亚季风的发展和演化、轨道和构造时间尺度；识别和更好地理解构造抬升、侵蚀和风化、半远洋沉积和气候变化，包括亚洲季风和晚第三纪的全球变冷。
• A general survey of the formation , evolutionary histories of continental orogenic belts both in china and abroad reveals that orogenic belts have often undergone numerous and varied tectono - evolutionary stages , such as palaeocontinental break - up , ocean - land transition , continental matching - collision , intracontinental extension - basin - range coupling , and new tectonic uplift ( intracontinental orogeny ) , which are respectively accompanied by characteristic volcano - magmatisms
  纵观我国以至全球的大陆造山带形成、演化历史，一个造山带往往经历了古大陆裂解、洋陆转换、陆块拼合碰撞、陆内伸展盆山耦合和新构造隆升（陆内造山）等众多不同的构造演化阶段，这些不同的构造演化阶段和不同的构造环境均有特定火山岩浆作用与之相伴。
• Scanning the formation - evolutionary histories of continental orogenic belts in both our country and whole workd , an orogenic belt has often undergone numerous and various tectono - evolutionary stages , such as palaeo - continental break - up , ocean - land transition , continental matching - collision , intracontinental extension - basin - range coupling , new tectonic uplift ( intracontinental orogeny ) , etc . , which are respectively companied with characteristic volcano - magmatism
  纵观我国以至全球的大陆造山带形成-演化历史，一个造山带往往经历了古大陆裂解、洋陆转换、陆块拼合-碰撞、陆内伸展-盆山耦合和新构造隆升（陆内造山）等?多不同的构造演化阶段，这些不同的构造演化阶段和不同的构造环境均有特定火山岩浆作用与之相伴。
• With the tectonic uplift of the source area and the climate turning dry , the coal forming period was over , the fluvial system and fluvial - delta system became to play a major role . based on the study of former researchers and the theory of deep basin gas reservoir forming , the deep basin gas trap in the ordos basin is analyzed and is supposed to form in the ramp of the basin . it is supposed that the hydrocarbon of the deep basin gas trap is mainly composed of coal , carbonate and carbonaceous shale and with the " upper water seal " in the north of the study area the g
  根据深盆气成藏理论和前人的研究成果，分析了深盆气藏的分布类型，认为鄂尔多斯盆地深盆气藏属于盆地斜坡成藏类型；认为深盆气的源岩以煤、炭质泥岩、暗色泥岩和碳酸盐岩为主；北部气水倒置、东部露头区有天然气逸出；气藏具有多重压力系统；成藏机理主要是气体动态的运移与聚集，稳定的构造背景有利于气藏的大面积保存。
• O curve of dsdp607 v30 - 97 show that loess began to deposit on the terrace of the yellow river about 1 . 20 ma b p , and passed thirteen climatic changes from drier and cooler to warmer and wetter later . the turn of sedimentation from alluvium to loess , an event of transformation from accumulation to down - cut of the yellow river , indicates a sharp tectonic uplift occurred around 1 . 2 ma b p . key words : loess - paleosol ; susceptibility ; climatic changes ; tectonic movement ; yellow river ; yangfan section
  通过对杨范剖面黄土地层岩性特征沉积结构质量磁化率和频率磁化率的分析及与深海氧同位素曲线的对比，划分了剖面地层，初步确定了黄土沉积始于1 . 20 ma b p ,黄土沉积以来该区发生了13次大的干冷暖湿气候变化沉积转型指示河流强烈加积转变为河流侵蚀，代表约在1 . 20 ma b p发生过一次强烈的构造抬升事件。
• This preliminary research focus on the tectonic uplift in late mesozoic - early cenozoic after the main collision oregeny to understand more and detail on the total process of tectonics evolvement in east dabie mountain and beihuaiyuan area . the research works that have been done are : apatite fission track dating , apatite thermal - evolvement patterns ; the fluid characteristics including fluid inclusions " microthermometer , the compositions , 5 d - 8 18o , and their geochemistry , thermodynamics parameters
  为更全面了解东大别山及北淮阳地区大地构造完整的演化，并为之提供研究实例积累，本研究主要从热年代学及造山后流体特点角度对东大别山及北淮阳构造区碰撞造山后中生代未-新生代初构造隆升活动进行了初步探讨。