?paleozoic

paleozoic 發(fā)音

[,p?li:?u'z?uik; -,pei-]

英：　　美：

paleozoic 中文意思翻譯

paleozoic 短語(yǔ)詞組

1、paleozoic canadia ─── 古生代加拿大

2、Paleozoic era un. ─── 古生代 [網(wǎng)絡(luò)] ─── 古生代初期； ─── 古生代 ─── 古生代

3、paleozoic period ─── 古生代

4、paleozoic era plants ─── 古生代植物

5、paleozoic dinomischus ─── 古生代恐龍化石

6、paleozoic cambroraster ─── 古生代寒武紀(jì)

7、paleozoic invertebrates ─── 古生代無(wú)脊椎動(dòng)物

8、Paleozoic Alps ─── 古生代阿爾卑斯山脈

9、paleozoic yugioh ─── 古生代尤吉奧

paleozoic 相似詞語(yǔ)短語(yǔ)

1、Cainozoic ─── adj.新生代的（等于Cenozoic）；n.新生代（等于Cenozoic）

2、heliozoic ─── 古生代

3、Palaeozoic ─── adj.（與）古生代（有關(guān)）的；古生代巖石；n.古生代時(shí)期

4、Paleozoic ─── adj.古生代的

5、Caenozoic ─── adj.新生代的；新生界的（等于Caenozoic）

6、holozoic ─── [動(dòng)]全動(dòng)物營(yíng)養(yǎng)的

7、hylozoic ─── 古生代

8、Neozoic ─── adj.新生代的

9、paleozoologic ─── 古動(dòng)物學(xué)

paleozoic 常見(jiàn)例句（雙語(yǔ)使用場(chǎng)景）

1、Fankou Pb-Zn deposit is a submarinehydrothermal spring effusion type ore deposit, which occurred in upper Paleozoic carbonaterock formation. ─── 凡口鉛鋅礦床是發(fā)育于上古生界碳酸鹽巖建造中的海底熱泉噴溢礦床。

2、Buried hills of Archaeozoic,Paleozoic and Mesozoic Eras developed well in the west part of Dongying Depression. ─── 東營(yíng)凹陷西部發(fā)育太古界、古生界及中生界潛山。

3、The deformation of the shear zones possibly occurred in the late Early Paleozoic, which was related to the in teraction between the Cathaysian plate and the Yangtze plate during that period. ─── 剪切帶的主要變形時(shí)代可能是早古生代后期,與這一時(shí)期華夏板塊與揚(yáng)子板塊之間的相互作用有關(guān)。

4、This was one of the first fossil algae to be described as such from Late Paleozoic rocks. ─── 這是最早化石藻類之一，描述了這種從晚古生代巖石作為。

5、The Lower Paleozoic source rocks in the eastern exploration region of Sinopec are mainly marine carbonates with a low organic content. ─── 中國(guó)石化東部探區(qū)下古生界烴源巖以海相碳酸鹽巖為主,有機(jī)質(zhì)豐度較低。

6、During the discussing hydrocarbon property in Changdi Paleozoic erathem buried hill and its east flank of drape structure in 2000, the oil source in Changdi area was initially discussed. ─── 20 0 0年,在討論長(zhǎng)堤古生界潛山以及其披覆構(gòu)造東翼的含油氣性時(shí),曾對(duì)長(zhǎng)堤地區(qū)的油源問(wèn)題進(jìn)行過(guò)初步分析。

7、The Qiuling sediments-hosted disseminated gold deposit in Zhenan, Shanxi is hosted in Nanyangshan Formation and Yuanjiagou Formation of Upper Paleozoic. ─── 丘嶺微細(xì)浸染型金礦床產(chǎn)于上古生界南羊山組及袁家溝組地層中。

8、Tall Paleozoic trees superficially resembling modern screw pines,structurally intermediate in some ways between cycads and conifers. ─── 一種高大的古生代樹(shù)木，外表與現(xiàn)代的露兜樹(shù)相似，結(jié)構(gòu)上介于蘇鐵和針葉樹(shù)之間。

9、South Boyang Sag is a typical superimposed basin,its Mesozoic and Paleozoic marine facies formation has relatively favorable conditions for generating oil &gas reservoirs. ─── 南鄱陽(yáng)坳陷是一個(gè)典型的疊合型盆地,中、古生界海相具有較好的油氣成藏條件;

10、Previous research considered that local intervals of Pingliang Formation were rich in mud and could act as Lower Paleozoic hydrocarbon source rocks, but they were not exploration targets. ─── 以往研究認(rèn)為平?jīng)鼋M局部層段富含泥質(zhì)，可作為下古生界烴源巖，但非勘探目的層。

11、There are great bifurcations as yet on the structural environment and on the evolution of the Xingmeng Paleozoic orogenic belt in Southeast Inner Mongolia during the Carboniferous Period. ─── 內(nèi)蒙古東南部古生代造山帶在石炭紀(jì)時(shí)期的構(gòu)造環(huán)境和構(gòu)造演化,至今在認(rèn)識(shí)上存在較大的分歧。

12、This was the end of the Permian period, and of the era of life called the Paleozoic. ─── 這就是二疊紀(jì)以及整個(gè)古生代的終結(jié)。

13、Feng Zengzhao, Chen Jixing et al.1991. Lithofacies paleogeography of early Paleozoic of ordos.Beijing:Geological Publishing House(in Chinese). ─── 馮增昭,陳繼興等.1991.鄂爾多斯地區(qū)早古生代巖相古地理.北京:地質(zhì)出版社.

14、Paleozoic simple dichotomously branched plants of Europe and eastern Canada including the oldest known vascular land plants. ─── 分布于歐洲和加拿大東部的古生代簡(jiǎn)單的二岐式植物，包含最古老的脈管陸地植物。

15、Within the belt ,the mid-late Proterozoic (epimetamorphic) green-schists were ovethrust from south to north onto the late Paleozoic granitic batholith at a low angle. ─── 中晚元古代淺變質(zhì)的綠片巖系自南向北以低角度輾掩于晚古生代花崗巖基之上。

16、County formation hypoplasia, missing the entire Paleozoic sector in the health sector and the Triassic. ─── 縣內(nèi)地層發(fā)育不全，缺失整個(gè)古生界和中生界的三疊系。

17、The reservoir rocks are Archaean granite, Lower Paleozoic carbonate rocks,Mesozoic sand rock and volcanic rock and fracture,solution cavities and pores are the major preserving spaces. ─── 儲(chǔ)集層由太古界變質(zhì)巖、下古生界碳酸鹽巖和中生界砂巖、火山巖組成,儲(chǔ)集空間主要為構(gòu)造裂縫及溶蝕孔隙;

18、The reservoir rocks are Archaean granite, Lower Paleozoic carbonate rocks, Mesozoic sand rock and volcanic rock and fracture, solution cavities and pores are the major preserving spaces. ─── 儲(chǔ)集層由太古界變質(zhì)巖、下古生界碳酸鹽巖和中生界砂巖、火山巖組成，儲(chǔ)集空間主要為構(gòu)造裂縫及溶蝕孔隙；

19、Tarim Basin is a superimposed and composite basin of numerous proto type basins combosed of the Paleozoic cratonic basins and Meso Cenozoic foreland basins. ─── 全面系統(tǒng)地總結(jié)并提出塔里木盆地10大石油地質(zhì)基本特征：（1）塔里木盆地為一古生界克拉通盆地與中新生界前陸盆地組成的大型疊合復(fù)合型盆地；

20、The sea-level fluctuation was an important controlling factor for karst carbonate reservoir development in the Early Paleozoic Tarim Basin. ─── 海平面變化是控制塔里木盆地下古生界巖溶儲(chǔ)層發(fā)育的一個(gè)重要的因素。

21、The paleozoic source rock in North China went into the main oil generating period at the end of Triassic. ─── 華北地區(qū)古生界生油巖在三疊紀(jì)末已進(jìn)入主要生油期。

22、According to the amplitude of vibration,wave group continuity and forms of seismic waves reflected on the 6 sections,the Meso Cenozoic,Upper Paleozoic,Predevonian,Precambrian,intrusive mass and the basic magma basement could be identified. ─── 利用深部地震剖面上反射波的振幅強(qiáng)弱、波組連續(xù)性和波組外形等識(shí)別標(biāo)志 ,可識(shí)別出中、新生界、上古生界、前泥盆系、前寒武系、侵入巖體和基性巖漿底墊等地質(zhì)體 ;

23、in Permian, it had developed and formed a typical Cathaysian flora and was an important part of late Paleozoic Cathaysian flora. ─── 二疊紀(jì)時(shí)已發(fā)展為典型的華夏植物區(qū)系的性質(zhì)，是晚古生代華夏植物區(qū)系的重要組成部分。

24、The Lower Paleozoic reservoir mainly by corrosion pore, intercrystalline pore and the crack are composed. ─── 下古生界儲(chǔ)層主要由晶間孔、溶孔和裂縫組成。

25、The Lower Paleozoic source rock in the region has undergone two oil generation processes,the first one has taken place in basin subsidence before Caledonian movement. ─── 區(qū)內(nèi)下古生界烴源巖經(jīng)歷了兩次成油過(guò)程,第一次在加里東運(yùn)動(dòng)前的盆地沉降階段,第二次在加里東運(yùn)動(dòng)后晚古生代陸表海沉積階段。

26、Accordingly, the South China was an Early Paleozoic orogenic belt instead of the Cathaysian Block (Paleocontinent). ─── 因此,華南是早古生代形成的造山帶,而不是華夏地塊(古陸)。

27、Hence, the Paleozoic, Mesozoic and Cenozoic zones over continental nucleus and its circumferences were of both individual feature and sizable superposition. ─── 其中波斯清盆地最為典型，古生界、中生界和新生界次第重合。

28、Compared with the Paleozoic, bivalves and are also many new types of development, ammonite is more complex decoration and chrysanthemum stone-suture. ─── 與古生代相比，雙殼類和菊石類也多屬新發(fā)展的種類，菊石多具有復(fù)雜的紋飾和菊石式縫合線。

29、Under the tectonic backgrounds of island arc belt, fore-arc trench belt, back-arc basin, and epicontinental active belt of Late Paleozoic, it has different volcanic rock characteristics. ─── 在晚古生代島弧帶、弧前海溝帶、弧后盆地或陸緣活動(dòng)帶等構(gòu)造環(huán)境下發(fā)育有不同的火山巖組合。

30、Discussion on Time- Depth Conversion for Paleozoic ─── 古生界時(shí)深轉(zhuǎn)換關(guān)系探討

31、Paleozoic carbonate buried hill reservoir in Nanpu oilfield is a pore-fracture dual media reservoir. ─── 南堡油田古生界碳酸鹽巖古潛山油藏為孔隙-裂縫型雙重介質(zhì)油藏。

32、South Tianshan: a Late Paleozoic or a Triassic orogen? ─── 南天山:晚古生代還是三疊紀(jì)碰撞造山帶?

33、Research on brachiopod fauna and stratigraphy of the late paleozoic in north China platform II. ─── 華北地臺(tái)晚古生代腕足動(dòng)物群及其地層研究2。

34、Any of numerous extinct marine arthropods of the class Trilobita, of the Paleozoic Era, having a segmented body divided by grooves into three vertical lobes and found as fossils throughout the world. ─── 三葉蟲多種構(gòu)成三葉蟲綱任一種的已滅絕的海洋節(jié)肢動(dòng)物，身體分節(jié)，有帶溝將身體一分為三個(gè)垂直的葉，在世界各地都發(fā)現(xiàn)過(guò)其化石

35、Early Paleozoic high-overmature strata are important source rock in Chinese petroliferous basins. ─── 下古生界高過(guò)成熟地層是我國(guó)重要的烴源巖。

36、Based on the late Paleozoic fold basement, Simao Triassic sedimentary basin formed in the early continental island arc colliusion stage after the close of Paleo Tethys ocean. ─── 三疊紀(jì)沉積盆地建立在晚古生代褶皺基底之上，形成了古特提斯洋閉合后，造山早期的弧陸碰撞階段。

37、Ancient plant in the early Paleozoic marine mainly to the late Silurian Period, the original plants begin boarding land. ─── 古植物在古生代早期以海生藻類為主，至志留紀(jì)末期，原始植物開(kāi)始登上陸地。

38、The concentrations of Br are lower in Cenozoic and Mesozoic sections than those in Paleozoic section that suggests that the sedimentary environment and evapo-concentration have an important effect to the content of Br. ─── 中新生界溴濃度較低、古生界較高，溴濃度受海陸相沉積環(huán)境和蒸發(fā)濃縮作用的控制。

39、This study provides solid deep geochemical constraints on the existence of Precambrian blocks among the Paleozoic Xingmeng orogen. ─── 上述研究首次為興蒙造山帶內(nèi)存在前寒武古老地體以及該造山帶組成特征提供了明確和系統(tǒng)的深部地球化學(xué)制約。

40、In the Southern North China region,a series of the Late Paleozoic formation with platform facies,transitional facies and inland lake facies had been deposited. ─── 南華北地區(qū)晚古生代沉積了一套臺(tái)地相-海陸過(guò)渡相-內(nèi)陸湖相地層,上古生界烴源巖主要為一套連續(xù)沉積的含煤巖系。

41、After 1999, the basite zone was found in the group of Kuerliang in middle-upper Carboniferous, in the Late Paleozoic strata of the North Kunlun area. ─── 1999年以來(lái)，在北昆侖地區(qū)晚古生界中上石炭統(tǒng)庫(kù)爾良群中發(fā)現(xiàn)了基性巖漿巖帶。

42、The Kalaxianger porphyry copper deposit(belt)is located in a Late Paleozoic island arc on the southern margin of the Altay Mountains. ─── 卡拉先格爾斑巖銅礦(帶)位于阿爾泰東南緣晚古生代島弧區(qū),含礦斑巖主要為一套中-晚海西期的中酸性斑巖,圍巖為中泥盆統(tǒng)北塔山組。

43、At the same time, coal bearing series strata in upper Paleozoic distributes within all basins, so coal-genetic gas is also abound.In order to reali... ─── 因此,為實(shí)現(xiàn)大港油田天然氣生產(chǎn)的良性循環(huán),應(yīng)堅(jiān)持科技創(chuàng)新和油氣并舉的原則,加快對(duì)黃驊坳陷天然氣新領(lǐng)域的勘探步伐,加快氣田(藏)的高效開(kāi)發(fā)和老區(qū)的滾動(dòng)挖潛。

44、However, we should also research the Paleozoic in the sedimentary basins, and focus on the places where preserved good and overlying sediments are thin, as these places have good petroleum resources. ─── 另外，對(duì)盆地中的古生界應(yīng)加強(qiáng)研究，在保存較好并且中新生代沉積較薄的地方做探查工作，應(yīng)該有一定的油氣前景。

45、of Paleozoic plants congregated at the water's edge and began to colonize the Earth's surface. ─── 的古生代植物聚集在水域邊緣，并逐漸蔓延到地球的各個(gè)角落。

46、On the basis of a detailed study of the Late Paleozoic section in the Bogexi area,Batang county,western Sichuan,six lithostratigraphic formations may be recognized in the study area. ─── 在對(duì)四川西部巴塘縣波格西地區(qū)晚古生代地層剖面研究的基礎(chǔ)上，從巖性、巖相分析入手，將該區(qū)地層劃分為6個(gè)組級(jí)巖石地層單位。

47、There is still much disagreement over the depositional characteristics of the Carboniferous Taiyuan Formation of Upper Paleozoic in the northern Ordos Basin. ─── 關(guān)于鄂爾多斯盆地北部上古生界石炭系太原組的沉積特點(diǎn),目前存在著多種不同的觀點(diǎn)。

48、From late Paleozoic to early Mesozoic , there was a complex trench-arc-basin system between Yangtze and Cathaysia blocks. ─── 從晚古生代-早中生代，揚(yáng)子陸塊和華夏陸塊之間可能存在一個(gè)復(fù)雜的溝弧盆體系。

49、Bivalves and there have been noticeable changes in the types of Late Paleozoic only a very small number continue to exist, many new types of produce, and a considerable number of many. ─── 雙殼類也有明顯變化，晚古生代的種類只有很少數(shù)繼續(xù)存在，產(chǎn)生了許多新種類，并且數(shù)量相當(dāng)繁多。

50、The reservoir type is Ordovician weathering crust in the Lower Paleozoic,and the main gas layer is in the fifth member of Majiagou Formation. ─── 儲(chǔ)集層類型為下古生界奧陶系古風(fēng)化殼型,其主力含氣層為馬家溝組第五段。

51、Based on the late Paleozoic fold basement, Simao Triassic sedimentary basin formed in the early continental-island arc collusion stage after the close of Paleo-Tethys ocean. ─── 三疊紀(jì)沉積盆地建立在晚古生代褶皺基底之上,形成于古特提斯洋閉合后,造山早期的弧陸碰撞階段。

52、The geotectonic background for copper-polymetallic mineralization in marine volcanic rocks of Paleozoic era,Beishan area,is expounde respectively according to synvolcanic and postvolcanic stages. ─── 分同火山作用期和后火山作用期間述了北山地區(qū)古生代海相火山巖中銅-多金屬成礦作用的構(gòu)造背景。

53、The following examples of oil and gas fields in distributary and delta-fringe sand bodies range in age from Late Paleozoic to Middle Cenozoic. ─── 下面所列舉的是分布于分流和三角洲前綠砂體的油氣田的例子，在地質(zhì)時(shí)代上從晚古生代至中新生代。

54、The tectonic pattern of midding-deep hiberarchy which includes upper Paleozoic's carbonatite is possibly thrust and broad-tempered fold. ─── 以上古生界碳酸巖為主的中深層次,其構(gòu)造樣式推測(cè)以沖斷和寬緩褶皺為主。

55、The sandstones in the upper Shihezi Formation of the Permian is the important objective reservoirs for the natural gas exploration in upper Paleozoic in the Bohai Bay Basin. ─── 二疊系上石盒子組砂巖是渤海灣盆地上古生界天然氣勘探的重要目的儲(chǔ)層。

56、The current Paleozoic is dominated by relic gas reservoirs survived reconstruction, while the Mesozoic is dominated by oil and gas r... ─── 下一步油氣勘探應(yīng)圍繞古生界烴源巖在綜合分析油氣成藏條件的基礎(chǔ)上,采用現(xiàn)代勘探技術(shù)落實(shí)有效圈閉,進(jìn)行立體勘探。

57、The enormous amount of natural gas generated from gas source rock of Paleozoic erathem and continuous gas supply ability is the base of the concertrated gas reservoirs. ─── 上古生界氣源巖巨大的排氣量和持續(xù)的供氣能力是古生界氣藏富集的基礎(chǔ),天然氣早期以垂向和側(cè)向運(yùn)移為主,晚期就近運(yùn)移聚集,為古生界特別是上古生界大面積含氣提供了有利條件。

58、The communities of Paleozoic plants congregated at the water ’s edge and began to colonize the Earth's surface. ─── 古生代的植物群落積聚在河邊，逐漸向地面進(jìn)軍。

59、Uranium mineralization of ductile fault rock type and other types were with metallogenetic ages being of Middle-Late Proterozoic and Late Paleozoic. ─── 發(fā)育有韌性斷層巖型等鈾礦化類型，成礦時(shí)代為中晚元古代和古生代晚期。

60、Late Paleozoic spore fossils found in the Shishuyuan Formation in Nanzhao County, Henan Province, confirm the existence of a Late Paleozoic trough in the North Qinling. ─── 南召柿樹(shù)園組發(fā)現(xiàn)晚古生代孢子化石，證實(shí)存在北秦嶺晚古生代海槽。

61、On this basis the paleogeographical changing process during the Paleozoic in the eastern Qinling is discussed. ─── 在此基礎(chǔ)上探討了東秦嶺古生代古地理變遷過(guò)程。

62、And the Bayan Har gold deposit, which is related to the granite-porphyry intruded in Sonid Zuoqi ophiolitic melange belt in the middle-late stage of the Late Paleozoic, is of an epithermal type. ─── 另一種是以巴彥哈爾為代表的、與侵入于蛇綠混雜巖帶中的晚古生代中晚期花崗斑巖有關(guān)的淺成低溫?zé)嵋盒徒鸬V。

63、Cathaysia Flora, one of the four famous floras of Late Paleozoic, is always the focus of study to palaeobotanists at home and abroad. ─── 作為晚古生代全球四大著名植物群之一的華夏植物群 (CathaysiaFlora),一直是國(guó)內(nèi)外古植物學(xué)家研究的焦點(diǎn)。

64、The crustal components in the region include: late Archean crystallization basement, middle-late Proterozoic fold series and Paleozoic cover of upper Sinian to Permian stratigraphic system. ─── 區(qū)域地殼結(jié)構(gòu)有基底結(jié)晶巖系(新太古界)和褶皺巖系(中新元古界),蓋層為古生界,自上震旦統(tǒng)至二疊系基本連續(xù)出露。

65、In Mesozoic, Guangdong flora had a big change, the gymnosperm was prosperous, but it was evolved from the late Paleozoic Cathaysian flora as a whole. ─── 中生代，廣東植物區(qū)系成分發(fā)生了很大的變化，裸子植物大量繁盛，但總體上是在本區(qū)晚古生代華夏植物區(qū)系的基礎(chǔ)上演化而來(lái)的。

66、Santanghu Basin is located between Altai Mountain and Tianshan Belt,it is a composite and reconstructed basin which superposes on the Paleozoic erogenic belt of Paleozoic age. ─── 三塘湖盆地位于阿爾泰山系與天山山系之間，為一疊置在古生代造山帶之上的復(fù)合改造型盆地。

67、The gold deposit at Hongtugou-Chuancigou in the northern Qilian area occurs in an Early Paleozoic collision orogenic belt, is a typical ductile shear zone gold deposit. ─── 北祁連地區(qū)的紅土溝-川刺溝金礦床產(chǎn)于早古生代碰撞造山帶中，是該造山帶形成和演化的階段性產(chǎn)物。

68、Lin Huixi.2004.Karstification of Lower Paleozoic reservoir in Zhuangxi-Chengdao area,Jiyang Sag,China.Journal of Chengdu University of Technology (Natural Sci.Ed.),31 (5):490-497. ─── [2]林會(huì)喜.2004.濟(jì)陽(yáng)坳陷樁西-埕島地區(qū)下古生界潛山儲(chǔ)層巖溶作用.成都理工大學(xué)學(xué)報(bào)(自然科學(xué)版),31(5):490-497.

69、The content of this text is studying evolutive degree of the source rock of the upper Sinian and the Paleozoic group mainly by vitrinite,pyrogenation,conodont and sporopollen. ─── 以鏡質(zhì)體反射率、熱解、牙形刺、孢粉作為劃分的主要依據(jù),研究了金衢盆地上震旦統(tǒng)和古生界烴源巖的演化程度。

70、Dynamic analysis of gas formation revealed that the resisting force for the capillary tubes in the Upper Paleozoic reservoir was so high that it prevented the remigration of gas. ─── 含氣范圍內(nèi)的同一氣層連通性較差，氣水分布受區(qū)域構(gòu)造控制，局部明顯存在邊底水，也沒(méi)有整體活塞式氣驅(qū)水作用形成的區(qū)域性氣水界面。

71、From late Paleozoic to early Mesozoic, there was a complex trench-arc-basin system between Yangtze and Cathaysia blocks. ─── 從晚古生代-早中生代，揚(yáng)子陸塊和華夏陸塊之間可能存在一個(gè)復(fù)雜的溝弧盆體系。

72、Of, belonging to, or designating the geologic time, system of rocks, and sedimentary deposits of the seventh and last period of the Paleozoic Era. ─── 二疊紀(jì)的，二疊巖的是、屬于或標(biāo)明為古生代第七個(gè)和最后一個(gè)階段的地質(zhì)時(shí)期、巖層及沉積礦藏

73、The Meso-Cenozoic Yingjisu depression is a piggyback foreland ba si n developed in the setting of the Paleozoic thrust nappe structure. ─── 疊瓦式逆沖斷層、花狀構(gòu)造、構(gòu)造三角帶、斷展褶皺和披覆構(gòu)造是英吉蘇凹陷的主要變形樣式。

74、Of,belonging to,or designating the geologic time,system of rocks,and sedimentary deposits of the seventh and last period of the Paleozoic Era. ─── 二疊紀(jì)的，二疊巖的是、屬于或標(biāo)明為古生代第七個(gè)和最后一個(gè)階段的地質(zhì)時(shí)期、巖層及沉積礦藏。

75、Thus the Nalati-Bindaban-Weiya zone was interpreted as an accretion-collision suture of continental blocks during Paleozoic time. ─── 因此，該帶被解釋為古生代大洋俯沖、陸塊碰撞拼貼的縫合帶。

76、The Meso-Cenozoic tectonic movements have great influence on present petroleum accumulations in Paleozoic basins in the south of China. ─── 南華北中南部中新生代盆地的形成演化主要受郯廬斷裂帶、大別造山帶構(gòu)造運(yùn)動(dòng)的制約。

77、NAN Run-shan, GUO Sheng-zhe, Paleozoic biostratigraphy and geography in the geosyncline of Inner Mongolia -Northeast [M].Beijing: Geological Publishing House,1992: 1-142. ─── [4]南潤(rùn)善,郭勝哲.內(nèi)蒙古-東北地槽區(qū)古生代生物地層及古地理[M].北京:地質(zhì)出版社,1992:1-142.

78、The Paleozoic prototype is related with the orogeny of the surrounding Altay Mts., East and West Junggar Mts., Northwest Tianshan Mts. ─── 其古生代盆地的形成與相鄰的阿爾泰山和東、西準(zhǔn)噶爾山、天山及博格達(dá)山的造山作用相關(guān)。

79、The three-dimensional positions of Paleozoic strata in the South Tianshan orogenoic belt were changed architecturally during the collision between the Tarim and Yining paleo-continents. ─── 南天山古生代地層的三度空間位置因造山作用改造而發(fā)生結(jié)構(gòu)性重組。

80、The paleozoic source rock in North China went into the main oil generating period at the end of Triassic. ─── 華北地區(qū)古生界生油巖在三疊紀(jì)末已進(jìn)入主要生油期。

81、Longshan complex, the junction of Qinling-Qilian orogen, Archean TTG, southern margin of North China Craton, early Paleozoic, island arc volcanics, Xinjie Complex. ─── 01隴山雜巖:秦嶺-祁連構(gòu)造結(jié)合部位;太古代TTG;華北地塊南緣;早古生代;島弧火山巖;新街片麻巖套

82、The homoclinal reverse fold occurred in the Meso-Proterozoic.The superimposed fold in the late stage occurred in the Early Paleozoic. ─── 主期褶皺形成于中元古代，晚期褶皺形成于早古生代；

83、There are few survivors of the animals that lived in the Paleozoic period. ─── 古生代的動(dòng)物現(xiàn)今已鮮有孑遺。

84、The communities of Paleozoic plants congregated at the water 's edge and began to colonize the Earth's surface. ─── 古生代的植物群落積聚在河邊，逐漸向地面進(jìn)軍。

85、Geological stratums from all eras, including the Pre-Cambrian period to the Paleozoic era, the Mesozoic era, and the Cenozoic era, are evenly distributed. ─── 從年代角度看，從前寒武紀(jì)到古生代、中生代、新生代的所有地層均勻分布，巖石由各種火成巖、沉積巖及變質(zhì)巖構(gòu)成。

86、Li Hongsheng and Bian Q antao.1993.Upper Paleozoic radiolaria of the Xijin Ulan-Gangqiqu ophiolite complex,Kekexili.Geoscience,7(4) :410-420. ─── [2]李紅生,邊千韜1993可可西里西金烏蘭-岡齊曲蛇綠混雜巖中晚古生代放射蟲現(xiàn)代地質(zhì),7(4):410-420.

87、Meteoric water leaked and dissolved the lower Paleozoic carbonate rock along faults in Paleogene because of differential upwarding of fault-block. ─── 古近紀(jì)斷塊發(fā)生差異升降，大氣淡水可以沿?cái)嗔褲B流到下古生界碳酸鹽巖中產(chǎn)生溶蝕作用；

88、They are, from the oldest to the youngest, the Paleozoic, Mesozoic, and Cenozoic eras. ─── 他們是,從最老對(duì)最年輕,古生代,中生,和Cenozoic時(shí)代。