tectonic uplift中文是什么意思

發(fā)音:

中文翻譯
造句

構(gòu)造上升

tectonic adj. 1.構(gòu)造的；建筑的。 2.【生物學(xué)】構(gòu)造的。 ...
uplift vt. 1.舉起，提起。 2.打起(精神)，發(fā)揚(yáng)(優(yōu)良品 ...
uplift vt. 1.舉起，提起。 2.打起(精神)，發(fā)揚(yáng)(優(yōu)良品德)，鼓起(干勁)。 3.提高(社會地位)。 4.【地質(zhì)學(xué)；地理學(xué)】使(地面)上升。 n. 1.舉起，抬起。 2.【地質(zhì)學(xué)；地理學(xué)】隆起。 3.〔美國〕(優(yōu)良品德的)發(fā)揚(yáng)，(精神的)高漲，(感情的)激發(fā)；進(jìn)步。 4.〔口語〕(使胸部鼓起的)乳罩 (＝ uplift brassiere)。 an uplift worker 熱心社會工作的人。 n. -er
tectonic adj. 1.構(gòu)造的；建筑的。 2.【生物學(xué)】構(gòu)造的。 3.【地質(zhì)學(xué)；地理學(xué)】地殼構(gòu)造上的，起因于地殼運(yùn)動的。
anticlinal uplift 背斜隆起
basement uplift 基底隆起
block uplift 斷塊上升作用
buoyant uplift 漂浮上升作用
central uplift 中央隆起
differential uplift 差異隆起; 差異上升
domal uplift 穹狀隆起
epeirogenetic uplift 造陸隆起
epeirogenic uplift 造陸上升
fennoscandia uplift 芬諾斯堪的亞地塊隆起
hydraulic uplift 靜水浮托力
hydrostatic uplift 靜水浮托力; 靜水上托力
land uplift 地面隆起
linear uplift 線狀隆起
marginal uplift 邊緣隆起
net uplift 凈上升
orographic uplift 地形抬升
regional uplift 區(qū)域抬升; 區(qū)域性隆起
residual uplift 殘留隆起
salt uplift 巖鹽隆起
seepage uplift 滲透揚(yáng)壓力

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例句與用法

Tectonic uplift of the cenozoic era in the qinling range
秦嶺新生代構(gòu)造隆升研究
The effects of cenozoic tectonic uplift on earth surface chemical weathering and global climate change
新生代構(gòu)造抬升對地表化學(xué)風(fēng)化和全球氣候變化的影響
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?上侏羅統(tǒng)層序地層的形成演化受全球海平面變化、構(gòu)造隆升與沉降、沉積物供給以及氣候條件的綜合影響。
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月間在中國南海進(jìn)行鉆探取樣，通過鉆取半遠(yuǎn)洋沉積，以期說明南海的新生代歷史，包括它的生物地層學(xué)、巖石地層學(xué)、年代學(xué)、古氣候?qū)W和古海洋學(xué)；重建千年級的晚新生代東亞季風(fēng)的發(fā)展和演化、軌道和構(gòu)造時間尺度；識別和更好地理解構(gòu)造抬升、侵蝕和風(fēng)化、半遠(yuǎn)洋沉積和氣候變化，包括亞洲季風(fēng)和晚第三紀(jì)的全球變冷。
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
縱觀我國以至全球的大陸造山帶形成、演化歷史，一個造山帶往往經(jīng)歷了古大陸裂解、洋陸轉(zhuǎn)換、陸塊拼合碰撞、陸內(nèi)伸展盆山耦合和新構(gòu)造隆升（陸內(nèi)造山）等眾多不同的構(gòu)造演化階段，這些不同的構(gòu)造演化階段和不同的構(gòu)造環(huán)境均有特定火山巖漿作用與之相伴。
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
縱觀我國以至全球的大陸造山帶形成-演化歷史，一個造山帶往往經(jīng)歷了古大陸裂解、洋陸轉(zhuǎn)換、陸塊拼合-碰撞、陸內(nèi)伸展-盆山耦合和新構(gòu)造隆升（陸內(nèi)造山）等?多不同的構(gòu)造演化階段，這些不同的構(gòu)造演化階段和不同的構(gòu)造環(huán)境均有特定火山巖漿作用與之相伴。
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
根據(jù)深盆氣成藏理論和前人的研究成果，分析了深盆氣藏的分布類型，認(rèn)為鄂爾多斯盆地深盆氣藏屬于盆地斜坡成藏類型；認(rèn)為深盆氣的源巖以煤、炭質(zhì)泥巖、暗色泥巖和碳酸鹽巖為主；北部氣水倒置、東部露頭區(qū)有天然氣逸出；氣藏具有多重壓力系統(tǒng)；成藏機(jī)理主要是氣體動態(tài)的運(yùn)移與聚集，穩(wěn)定的構(gòu)造背景有利于氣藏的大面積保存。
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
通過對楊范剖面黃土地層巖性特征沉積結(jié)構(gòu)質(zhì)量磁化率和頻率磁化率的分析及與深海氧同位素曲線的對比，劃分了剖面地層，初步確定了黃土沉積始于1 . 20 ma b p ,黃土沉積以來該區(qū)發(fā)生了13次大的干冷暖濕氣候變化沉積轉(zhuǎn)型指示河流強(qiáng)烈加積轉(zhuǎn)變?yōu)楹恿髑治g，代表約在1 . 20 ma b p發(fā)生過一次強(qiáng)烈的構(gòu)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
為更全面了解東大別山及北淮陽地區(qū)大地構(gòu)造完整的演化，并為之提供研究實例積累，本研究主要從熱年代學(xué)及造山后流體特點角度對東大別山及北淮陽構(gòu)造區(qū)碰撞造山后中生代未-新生代初構(gòu)造隆升活動進(jìn)行了初步探討。

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