tectonism造句
例句與造句
- The palaeogeographical evolution sensitively responds to the tectonism in the whole triassic
紹興宜春斷裂作為構(gòu)造分區(qū)的界限，控制了其兩側(cè)古地理的發(fā)展。 - The increasing volcanism implies that the regional tectonism became progressively severe from the early stage to late stage of the late carboniferous
自晚石炭世早期到晚期，火山活動(dòng)期逐漸增長(zhǎng)，休眠期逐漸縮短，反映出盆地性質(zhì)自穩(wěn)定向活動(dòng)的轉(zhuǎn)化過程。 - Eastern zhanhua sag is one of the most complicated tectonism areas in jiyang depression , and it is also one of the most hydrocarbon proliferous areas in shengli oilfield
沾化凹陷東部是濟(jì)陽(yáng)坳陷構(gòu)造變動(dòng)最為復(fù)雜的地區(qū)之一，同時(shí)也是勝利油田油氣資源最為豐富的地區(qū)之一。 - The polyphasic and episodic tectonism of these basins usually had a significant influence on the regional deposition - erosion cycles and the depositional patterns
盆地構(gòu)造演化的階段性、旋回性及多期的構(gòu)造變革對(duì)盆內(nèi)多旋回的沉積剝蝕過程的疊加和原型盆地的疊合等可產(chǎn)生深刻的影響。 - After making detailed research on ore - controlling factors , the author points out that gold deposits in fujian resulted from the various geologic processes such as sedimentation , metamorphism , tectonism and magmatism
詳細(xì)研究了福建省金礦的金礦的控礦因素，提出省內(nèi)金礦的形成是沉積作用、變質(zhì)作用、構(gòu)造作用和巖漿作用(包括火山作用)的綜合結(jié)果。 - It's difficult to find tectonism in a sentence. 用tectonism造句挺難的
- The tectonism in this area can be divided into three phases , that is the folded basement formation and stable ancient land in pre - mesozoic , ancient land cracking phase in mesozoic , the faulted activity and subsidence phase in cenozoic
本區(qū)構(gòu)造變動(dòng)劃分為三個(gè)大的階段，即：前中生代褶皺基底的形成和穩(wěn)定古陸發(fā)育階段、中生代古陸裂解階段、新生代塊斷活動(dòng)及整體沉降階段。 - On the basis of former work , the basic structural feature is studied in this paper , the tectonism and basin development model are put forward , the transformed mechanism of stress field is analyzed , and the basin feature is discussed
本文在以往工作的基礎(chǔ)上，研究了本區(qū)的基本構(gòu)造特征，提出了構(gòu)造變動(dòng)及“盆地”發(fā)育的模式，分析了應(yīng)力場(chǎng)轉(zhuǎn)換機(jī)制，并對(duì)“盆地”性質(zhì)進(jìn)行了探討。 - The tuchengzi formation mainly consists of carbonate ( limestone and dolomite ) clast conglomerate characterized by poorly sorted and poorly rounded clasts , which shows that the deposition of the tuchengzi formation is closely associated with late jurassic tectonism
礫巖的成分和結(jié)構(gòu)成熟度都表明它的形成與劇烈的構(gòu)造活動(dòng)緊密相關(guān)，是研究區(qū)內(nèi)晚侏羅世時(shí)期強(qiáng)烈構(gòu)造變動(dòng)的沉積記錄。 - Comprehensive analysis by combination of basin tectonism during basin formation and evolution with the basin filling and reforming is the key to reveal the configuration of depositional systems and the source , reservoir and seal in the inland tectonically active basins
摘要結(jié)合盆地形成演化過程中各種構(gòu)造作用與盆地沉積充填和改造過程的成因分析，是揭示內(nèi)陸構(gòu)造活動(dòng)盆地沉積體系域時(shí)空配置和生儲(chǔ)蓋發(fā)育分布的重要基礎(chǔ)。 - The mechanical genesis of the complicated rock mass is because several times of tectonism in pro - period made the structure of rock mass in the right dam foundation damaged seriously and rock mass alteration made its mechanical character more anisotropy . after that the fractures in the right dam foundation slope were stretched at the beginning of the quaternary period because in the period yakouhoushan mountain quaquaversal dome was blowups quickly . at the same time , the valley trenching of lancang river reach to 800 - 1000 meter in altitude at the right bank in nuozadu dam site
導(dǎo)致右岸巖體復(fù)雜化的成因是，右岸巖體在早期遭受了多期構(gòu)造作用和巖體蝕變的基礎(chǔ)上，第四紀(jì)早期丫口后山穹隆的快速隆起與當(dāng)時(shí)河谷下切至800m 1000m高程這一特殊因素組合引起了右岸巖體沿原有的斷裂(裂隙)張開，使地下水等風(fēng)化營(yíng)力能夠到達(dá)坡體較深部位，經(jīng)過長(zhǎng)期的風(fēng)化卸荷作用，形成了右岸復(fù)雜巖體。 - Recently , we brought the salt crystal products form poland and himalayas for the beauties of the town . from ancient times , tectonism made ocean changed to be mountain , with the formation of the magnificent mountains , salt water had covered in the deep of the mountains has existed mineral salt crystals
巖鹽水晶產(chǎn)自喜瑪拉雅山一帶，約2億8千萬年前為海洋,由于地殼變動(dòng)形成現(xiàn)今的山脈，而海水中的鹽份則深藏在地下約數(shù)千米，經(jīng)過幾億年的蘊(yùn)藏將地底的礦物質(zhì)與海鹽結(jié)合形成晶狀。 - Past investigation found the rock in the right dam foundation composing of granite ( _ 4 ~ 3 _ 5 ~ 1 ) in dyas - trias , which has a very complicated mechanical environment . the complicated phenomenon is as follows : tectonism , alteration , rock mass demobilize , rock mass stress release and other factors . because of this several weakness rock zones and a loosen rock mass zone are develop in the right dam foundation
前期的調(diào)查表明其右岸巖體力學(xué)環(huán)境復(fù)雜，表現(xiàn)為：構(gòu)成右岸壩基(肩)巖體主體的二迭三迭紀(jì)花崗巖( _ 4 ~ 3 _ 5 ~ 1 )受構(gòu)造變動(dòng)、蝕變、風(fēng)化卸荷等因素的影響形成了壩基軟弱巖帶和壩肩上部卸荷松弛巖體。 - ( 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 )羌塘盆地與意大利中部中?晚侏羅世剖面穩(wěn)定同位素響應(yīng)的對(duì)比研究表明，中?晚侏羅世全球海平面表現(xiàn)為在五次升降旋回中呈現(xiàn)上升的總趨勢(shì)，而在研究區(qū)表現(xiàn)為在五次升降旋回中海平面下降的總趨勢(shì)，區(qū)域構(gòu)造作用和全球海平面變化共同對(duì)研究區(qū)相對(duì)海平面變化中起到控制作用。 - During my master " degree investigation , i mainly focused on the coarse - grain stratigraphy within mesozoic basins in chengde and pingquan districts , the eastern yanshan , and did systemic provenance analysis and paleo - current direction measurement and studied the relationship among basin evolution , volcanism and tectonism . then i summarized the mesozoic basin development and the coupling characters of basin and mountain . the evolution of basin and mountain in this area can be divided into several stages : the stage of compression uplift and flexural basin during the triassic through the early jurassic , the stage of structural compression - volcanism and foreland basin during the middle and late jurassic and the stage of rift basin in the cretaceous
在野外典型路線調(diào)查的基礎(chǔ)上，對(duì)燕山地區(qū)東段承德、平泉地區(qū)的中生代盆地中發(fā)育的粗碎屑沉積層，進(jìn)行了系統(tǒng)的物源分析與古流測(cè)定，并在此基礎(chǔ)上重點(diǎn)剖析了盆地的發(fā)育、火山活動(dòng)、構(gòu)造變動(dòng)三者之間的關(guān)系，總結(jié)了本區(qū)中生代盆地發(fā)育規(guī)律及盆山耦合特征，并將盆山演化劃分為：三疊紀(jì)?早侏羅紀(jì)的構(gòu)造擠壓隆升與撓曲盆地發(fā)育階段階段，中晚侏羅紀(jì)的構(gòu)造擠壓?火山活動(dòng)與類前陸盆地發(fā)育階段，早白堊世的拉張斷陷盆地發(fā)育階段。 - 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
盆地規(guī)模的沉積旋回多是盆地幕式裂陷、多幕擠壓撓曲沉降、多期構(gòu)造反轉(zhuǎn)、斷塊差異沉降等構(gòu)造作用的沉積回應(yīng)；高頻層序單元的發(fā)育則主要與湖平面和沉積物供給量的變化有關(guān)。
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