?Cambrian

Cambrian發(fā)音

英：[?k?mbr??n]　　美：[?k?mbr??n]

英：　　美：

Cambrian中文意思翻譯

n. [地]寒武紀(jì)；威爾士人

adj. [地]寒武紀(jì)的；威爾士的

Cambrian常見例句

1 、Microplants, including 12 genera and 28 species, have been discovered in the Cambrian of Yunxi county, Hubei.───在湖北鄖西縣發(fā)現(xiàn)寒武紀(jì)微古植物共12屬28種。

2 、Feng Zengzhao,Bao Zhidong,Wu Maobing,et al.Lithofacies Paleogeography of the Cambrian and Ordovician in Tarim Area[M].Beijing:Geological Publishing House,2005:1-184(in Chinese with English abstract).───[5]馮增昭,鮑志東,吳茂炳,等.塔里木地區(qū)寒武紀(jì)和奧陶紀(jì)巖相古地理[M].北京:地質(zhì)出版社,2005:1-184.

3 、Whatever the cause, there was one big difference between the Avalon and Cambrian explosions: The Cambrian produced groups that endure to this day, Xiao says, whereas the Ediacaran forms soon vanished.───不過，無論原因?yàn)楹危⑼呗〖o(jì)大爆發(fā)和寒武紀(jì)大爆發(fā)之間存在著一個最大不同，即寒武紀(jì)出現(xiàn)的生物種類持續(xù)至今，而埃迪卡拉紀(jì)物種形式很快就消失了。

4 、Maturity distribution and e volution of Cambrian source rocks are delinea ted using software BasinMod-1D on 250wells and 340pseudowells from the 26seismic profiles.───利用BasinMod-1D軟件計(jì)算了250口探井,26條地震測線中約340個人工井點(diǎn)有機(jī)成熟度隨時間的變化,據(jù)此編制不同地質(zhì)時期塔里木盆地臺盆區(qū)寒武系有機(jī)成熟度平面變化圖。

5 、Micritic dolostone occurs widely in the Middle and Upper Cambrian and is yellowish brown and brickcolored red, in which parallel laminae, bird's-eyes and mud-cracks are developed.───準(zhǔn)同生白云巖廣泛出現(xiàn)于中上寒武統(tǒng)，巖石呈土**、磚紅色，具紋層、烏眼、乾裂構(gòu)造。

6 、A lagerst?tte older than the Burgess Shale, in the Chengjiang area of China's Yunnan Province, has yielded many important recent finds of soft-bodied organisms also characteristic of the Cambrian explosion.───在中國云南的澄江一帶，有著比伯吉斯頁巖更古老的特異埋藏點(diǎn)，已發(fā)掘出許多同樣具有寒武紀(jì)大爆發(fā)特色的重要軟體生物。

7 、The Cambrian phosphoric ore is mainly composed of calcic phosphate, carbonate, silica and silicate minerals.───寒武系**礦主要由鈣**酸鹽、碳酸鹽、硅質(zhì)及硅酸鹽類等礦物組成。

8 、Major hydrocarbon source rocks are in the Cambrian and Ordovician.───寒武-奧陶系烴源巖是該區(qū)主力烴源巖;

9 、Cambrian limestone rock for the geological, tectonic movement as a result of strong crustal mutate, large-area exposure of the bedrock valley cutting deeper.───山巖地質(zhì)為寒武紀(jì)石灰?guī)r，由于構(gòu)造運(yùn)動強(qiáng)烈，地殼發(fā)生變異，大面積基巖裸露，溝谷切割較深。

10 、Cambrian The earliest period of the Paleozoic era, about 590-510 million years ago.───寒武紀(jì):地質(zhì)年代古生代的第一個紀(jì)，在五億九千萬到五億一千萬前。

11 、Potential source rocks in Cambrian and Ordovician that can have primary hydrocarbon generation possibility or secondary hydrocarbon generation potential are regarded as effective source rocks.───寒武系和奧陶系具有一次生烴可能或二次生烴潛力的潛在視為的效有烴源巖。

12 、When I view all beings not as special creations, but as the lineal descendants of some few beings which lived long before the first bed of the Cambrian system was deposited, they seem to me to become ennobled.───當(dāng)我看到所有的生物不是特殊的創(chuàng)造品而是幾種遠(yuǎn)在志留紀(jì)層還未形成之前就已存在的生物的直系后代，他們就似乎變得更加高貴了。

13 、The discovery of two new species improve our knowledge of diversity for protoconulariids.Meanwhile, it provides new clue for the hypothesis about diverse cnidaria in early Cambrian.───兩新種的發(fā)現(xiàn)無疑增加了我們對早期錐石類多樣性的認(rèn)識，為證實(shí)多樣性的刺細(xì)胞動物在早寒武世早期已經(jīng)存在的假說提供了新線索。

14 、In the Early Cambrian, the Tarim area was mainly a carbornate platform, in which there were penebanks, dolomitic flat, and gypsum-halite lake.───在早寒武世，塔里木地區(qū)是一個碳酸鹽巖臺地，其中散布著準(zhǔn)灘、云坪和膏鹽湖。

15 、Fossil evidence has suggested that there was a major jump in eukaryotic complexity some 600 million years ago, during a period dubbed the Cambrian ex-plosion.───化石證據(jù)已經(jīng)顯示出在大約在6億年前，原核細(xì)胞復(fù)雜體在被稱為“寒武紀(jì)大爆發(fā)”的時期發(fā)生了一次大的飛躍。

16 、DISCUSSION OF GENUS PROCONODONTUS FROM TOP CAMBRIAN───對寒武系頂部發(fā)育的原牙形石屬的討論

17 、The distribution of the middle upper Zhangxia Formation, Cambrian in Yishui area, Shandong, is controlled by Yishui rift (including F 4 and F 3 faults).───山東沂水地區(qū)寒武系張夏組中上部地層的分布，受控于沂沭斷裂（F4和F3斷裂），分為西區(qū)、中區(qū)和東區(qū)。

18 、There are 7 principal palaeogeographic units in the Cambrian in South China, i.e.Dianxi Platform, Kangdian Land, Yangtze Platform, Slope, Jiangnan Basin, Southeast Platform and Cathaysian Land.───中國南方寒武紀(jì)有7個主要的古地理單元，即滇西臺地、康滇陸、揚(yáng)子臺地、斜坡、江南盆地、東南臺地和華夏陸。

19 、Not only most metazoan phyla made their debut at the earliest Cambrian, but also the fossil record like calcareous metaphyte flora and acritarch change dramatically nearly at the same time.───地球外部圈層的演替變化，諸如大陸重組、地磁極移、古氣候、大洋地球化學(xué)性質(zhì)的變化以及大氣氧含量的變化等在時間上與這一生命爆發(fā)事件有耦合關(guān)系。

20 、The bimodel volcanic rocks of Middle Cambrian are major host rocks containing many polymetallic VMS deposits with larger scale.───中寒武統(tǒng)雙峰火山巖所賦存的多金屬VMS礦床多、規(guī)模大，是主要含礦巖系。

21 、The Central Paleouplift described by Ordovician top surface was merely present during late Cambrian to last stage of Shihezi.───以奧陶系頂面所刻畫的中央古隆起顯示:中央古隆起僅在晚寒武世-石盒子期末有所顯示。

22 、The lithology of karst is pure carbonatite at geological age of intermediate Cambrian and intermediate Ordovician.───北方巖溶和巖溶水的開發(fā)利用,見于碑刻者亦可追溯至1000年前。

23 、As one of the oldest petroliferous layers in platform-basin transitional area of Tarim basin, More and more attention has been paid to Cambrian by petroleum geologists.───作為塔里木盆地臺盆區(qū)最古老的含油氣層位之一，寒武系越來越為勘探所重視，分析寒武系油氣成藏的主控因素及分布規(guī)律對指導(dǎo)油氣具有重要的意義。

24 、The Middle Cambrian Burgess Shale, discovered at the early of the last century, has long been considered as one of the best windows on the Cambrian explosion.───中寒武世布爾吉斯頁巖發(fā)現(xiàn)早、研究歷史長，是早期人們認(rèn)識寒武紀(jì)爆發(fā)規(guī)模的較理想的窗口。

25 、A CAMBRIAN TRILOBITE FAUNA FROM MUFUSHAN,NANKING───南京幕府山寒武紀(jì)三葉蟲

26 、The area we debated is in infraneritic environment at the Meishucunian Age,early Cambrian Period,when deposited a suit of carbonate and phosphate.───川西南滇東地區(qū)在早寒武世梅樹村期處于上揚(yáng)子淺海環(huán)境,沉積一套淺海碳酸鹽和**酸鹽。

27 、Crumillospongia biporosa are found in Lower Cambrian Chengjiang Biota and Middle Cambrian Burgess Shale Biota, too.───biporosa的牛蹄塘生物群下部層位低于澄江生物群,貴州遵義松林可能是C.

28 、Cambrian explosion designates the sudden appearance of a majority of animal phyla nearly at the base of Cambrian.───寒武紀(jì)生命大爆發(fā)是指多門類的后生動物化石首次于寒武系底部“爆發(fā)”式出現(xiàn)的生物演化輻射事件。

29 、The main ore-bearing country rocks are aregillaceous limestone and marmarization limestone of upper-middle Cambrian.───其中寒武系上、中統(tǒng)大理巖化灰?guī)r、泥質(zhì)灰?guī)r為主要含礦圍巖。

30 、VOICE: How many times have you gone back to Chengjiang, the Chinese Cambrian site?───你已經(jīng)去過澄江,中國寒武紀(jì)的地區(qū)有多少次呢?

31 、The Cambrian oolitic limestones in the Dabeiwang section in Xuzhou, Jiangsu are characterized by numerous layers,complicated textures and types and diverse morphologies.───徐洲大北望地區(qū)寒武系鮞?；?guī)r層數(shù)眾多，結(jié)構(gòu)、類型復(fù)雜，形狀多樣，其中以放射鮞、同心鮞及放射-同心鮞為主。

32 、It occurs in the siliceous rock of Cambrian Hetang group, the ore-body displays occurrence in the form of beds, pralleling wi...───在油漆中替代沉淀硫酸鋇和滑石粉。用硅土作填料，具有提高產(chǎn)品的性能和質(zhì)量，可降低生產(chǎn)成本，增強(qiáng)企業(yè)活力。

33 、EVOLUTION OF CAMBRIAN QINLING PALEO-OCEAN───寒武紀(jì)秦嶺古海洋演化

34 、There is abundant karst fissure water in the limestone and dolomite of Cambrian and Ordovician.───寒武系、奧陶系地層主要為灰?guī)r和白云巖,其間賦存有較豐富的巖溶裂隙水。

35 、Hydrocarbon source rocks in North Tarim Basin can be divided into three petroleum systems such as Cambrian Ordovician system,Tertiary Jurassic system and Carboniferous Permian system.───依據(jù)塔北地區(qū)烴源巖及勘探狀況 ,可劃分出寒武 +奧陶系、三疊 +侏羅系及石炭 +二疊系 3套源巖含油氣系統(tǒng) ,其中 ,前兩套為已知含油氣系統(tǒng) ,后者為推測含油氣系統(tǒng)。

36 、RESEARCHES ON CAMBRIAN BRADORIIDS───寒武紀(jì)高肌蟲的研究

37 、The gold deposits , occurring in the south subzone of western Qinling, existed in the Cambrian silicalite formation .───位于西秦嶺南亞帶寒武系硅巖建造中的金礦床,是我國迄今僅見的與海底噴流作用有關(guān)的層控金礦床。

38 、ZHANG Jun-ming,YUAN Ke-xing.The Early Cambrian reef and its petrogenesis of the Tianheban Formation at Yichang County,Hubei Province[J].Chinese Journal of Geology,1994,29(3):236-243.───[3]張俊明,袁克興.湖北宜昌王家坪下寒武統(tǒng)天河板組古杯礁丘及其成巖作用[J].地質(zhì)科學(xué),1994,29(3):236-243.

39 、Cambrian source rocks,including mud shales and carbonates,are among the main source rocks in Tarim basin.───寒武系烴源巖是塔里木盆地主要烴源巖之一,包括泥頁巖和碳酸鹽巖。

40 、Bryozoa was quite diversified in the Ordovician, but lacked fossil records in the Cambrian.───古生物學(xué)資料表明 ,雖然苔蘚動物的大多數(shù)類群在奧陶紀(jì)已經(jīng)分化出來 ,但它在寒武紀(jì)卻缺乏任何化石記錄。

41 、Therefore the deficiency of pre-Cambrian fossil and the sudden emergence of Cambrian trilobite are like a double edged sword posing threat for the very foundation of Darwin evolutionism.───因而前寒武紀(jì)化石的缺失和寒武紀(jì)三葉蟲等突發(fā)式出現(xiàn)，好象一把雙刃劍，對達(dá)爾文演化學(xué)說的塔基構(gòu)成了威脅。

42 、The beginning of the Cambrian era saw a widespread arrival of multi-cellular organisms, particularly in the form of sponges.───寒武紀(jì)時代的初期看了多細(xì)胞性的有機(jī)體普遍到來,特別以海綿的形式。

43 、Of, belonging to, or being the oldest and largest division of geologic time, preceding the Cambrian Period, often subdivided into the Archeozoic and Proterozoic eras, and characterized by the appearance of primitive forms of life.───前寒武紀(jì)的地質(zhì)年代中最古老和最大的階段的、屬于這一階段的或處于這一階段的，其前為寒武紀(jì)期，寒武紀(jì)期又可細(xì)分為始生代和原生代，特征為原始生命形式的出現(xiàn)

44 、ZENG Yun-fu,SHEN Li-juan,HE Yan-gui,et al.Preliminary analysis of the outcrop sequence stratigraphy for phosphatic series of Early Cambrian in eastern Yunnan[J].Mineral Petrol,1994,14 (3):43-53.───[14]曾允孚,沈麗娟,何延貴,等.滇東早寒武世含**巖系層序地層分析[J].礦物巖石,1994,14(3):43-53.

45 、Follow-up studies using the molecular clock produced estimates for this split that varied significantly, ranging from as old as one billion years ago to as young as just before the Cambrian period.───后來使用分子時鐘來估算分支時間的研究結(jié)果，差異都很大，可能早至10億年前，晚至寒武紀(jì)即將開始時。

46 、The Lower Palaeozoic group mainly includes Cambrian, medial and lower Ordovician, which are marine carbonate in the district.───下古生界包括寒武系和下、中奧陶統(tǒng)，主要由海相碳酸鹽巖構(gòu)成。

47 、A series of discoveries and studies on ancient life forms in the 20th century demonstrated that Cambrian was a geological period full of the wildest imagination.───20世紀(jì)古生物的一系列發(fā)現(xiàn)和研究，證明了寒武紀(jì)是一個最能激發(fā)人們想象力的地質(zhì)時代。

48 、To the question why we do not find rich fossiliferous deposits belonging to these assumed earliest periods prior to the Cambrian system, I can give no satisfactory answer.───對于為什么我們沒有發(fā)現(xiàn)大量的屬于這個比寒武紀(jì)還要早的時期的化石，我無法給出滿意的答案。

49 、Dolostone is the main rock type of the Cambrian in this area.───從下寒武統(tǒng)石龍洞組開始都是白云巖沈積。

50 、Volcanic eruptive activities occurred from Cambrian to Permian,most intensely in Devonian and Carboniferous.───從寒武紀(jì)到二疊紀(jì)都有火山噴發(fā)，以泥盆、石炭紀(jì)火山噴發(fā)活動最強(qiáng)。

51 、And among the total reserves of seimentary deposits,of Sinian are 51%,of Cambrian are 44%,of Devonian are 4.9%,of other periods totaled only about 0.1%.───在沉積**塊巖的總儲量中，震旦紀(jì)的約占51%，寒武紀(jì)的約占44%，泥盆紀(jì)的占4.9%，其余時代占0.1%。

52 、And the main reservoirs include Cambrian sandstones, Ordovician sandstones and Triassic sandstones.Thick marls, dolomite, anhydrite and rock salt are excellent regional seals.───主要儲層包括寒武系、奧陶系和三疊系砂巖，區(qū)域良好蓋層是巨厚的泥灰?guī)r、白云巖、硬石膏和巖鹽。

53 、And Ordovician and Cambrian, Quaternary of the people who hailed from a fight.───和奧陶紀(jì)、寒武紀(jì)、第四紀(jì)的生靈們打個招呼。

54 、EARLY CAMBRIAN REEFS AND BANKS DEVELOPMENT IN SOUTHERN MARGIN OF DABA Mt. AND Micang Mt.───大巴山、米倉山南緣早寒武世礁灘發(fā)育特征。

55 、Two periods of high-pressure metamorphic belts, which have been dated 335.5 Ma and 440-460 Ma seperately by isotopic methods, have been discovered in the mid Cambrian and low-middle Ordovician strata.───同位素年齡分別為335.5 Ma和440-460 Ma的兩期高壓變質(zhì)帶賦存于中寒武統(tǒng)和下中奧陶統(tǒng)中。

56 、The closure of Kabei structure decreased to some extent, but the conditions still existed for the formation of relic Lower-Middle Cambrian gas reservoirs.───卡拉構(gòu)造的圈閉幅度有所減小，但仍具備形成中下寒武統(tǒng)殘存氣藏的條件。

57 、The gold 、 silver 、 polymetallic deposits is mostly formed in two historic era, namely former Cambrian and Mesozoic Yanshan epoch .───華北板塊北緣的金銀、多金屬礦床主要形成于兩大地質(zhì)歷史時期,即前寒武紀(jì)和中生代燕山期。

58 、G book, Cambrian company realize that can't do a simple collers business card printing and membership card-making factory.───圖書公司一樣，寒武紀(jì)公司也意識到了自己不能做一個單純的書刊制卡和會員卡制作廠。

59 、A study of Shijiazhuang depression revealed a low uplift, which is favorable for geothermal prospecting in Cambrian and Ordovician limestone.───工作結(jié)果在石家莊凹陷內(nèi)發(fā)現(xiàn)槐底低凸起存在，是尋找寒武系、奧陶系灰?guī)r類型的地?zé)徇h(yuǎn)景有利地區(qū)；

60 、The salts are continental source and come from the Cambrian and Ordovician systems of the surrounding uplifts.───其鹽源主要是陸源，由周圍凸起的寒武、奧陶系提供。

61 、The study of reservoir bitumen showed that the source is not only the carbonate in middle and late ordovician, but also the carbonate in Cambrian.───儲層瀝青研究表明烴源巖不僅僅只有中上奧陶系烴源巖,還有寒武系烴源巖。

62 、They occur in Early Sinian Beiyixi Formation, Late Sinian Zhamoketi Formation and Shuiquan Formation as well as Early Cambrian Xishanbulake Formation respectively.───它們分別產(chǎn)出于早震旦世的貝義西組、晚震旦世的扎摩克提組和水泉組以及早寒武世的西山布拉克組。

63 、Middle cambrian AWaTaGe formation denude close to YingMai 36.Analysis of sedimentary facies indicate the formation located in the restricted platform tidal-flat facies.───中寒武統(tǒng)阿瓦塔格組剝蝕出露于英買36井區(qū)附近，沉積相分析表明主要處于局限臺地潮坪相區(qū)內(nèi)。

64 、STRANGELOVE OCEAN BEFORE THE CAMBRIAN EXPLOSION───寒武紀(jì)生物爆發(fā)前的死劫難海洋

65 、The extreme climate arisen from "snowball Earth" may promote evolution of life and trigger the "Cambrian Explosion".───"雪球地球"的極端氣候環(huán)境變化,促進(jìn)了生命的演化,造成了寒武紀(jì)生物大爆發(fā)。

66 、Problems of Cambrian trilobite biogeography───寒武紀(jì)三葉蟲生物地理區(qū)的一些問題

67 、Cambrian: the beginning of the Paleozoic Era Animals with hard-shells appeared in great numbers for the first time during the Cambrian.───寒武紀(jì)：古生代的開始（距今5億1,400萬年前），具有硬殼的生物在寒武紀(jì)第一次大量出現(xiàn)。

68 、Hydrocarbon in the Ordovician petroleum accumulation system originated from the Cambrian and Lower Ordovician source rocks.───塔中低凸起奧陶紀(jì)油氣成藏體系的源巖為寒武系及下奧陶統(tǒng)烴源巖 ;

69 、Cambrian and the Cambrian Explosion───三寒武紀(jì)及寒武紀(jì)大爆發(fā)

70 、Even there are different views about the Tan-Lu Fault’s characters, the author think that the Tan-Lu Fault is a huge transcurrent fault which was formed after the Cambrian.───盡管目前關(guān)于郯廬斷裂的性質(zhì)的問題還沒有完全統(tǒng)一，作者認(rèn)為郯廬斷裂的性質(zhì)為晚寒武世之后形成的走滑斷裂。

71 、The Palaeozoic has been broken down into six smaller units of geological time called periods. Cambrian is the oldest period of the Palaeozoic followed successively by Ordovician, Silurian, Devonian, Carboniferous and Permian Periods.───古生代可劃分成6個小的叫做紀(jì)的時間單位，寒武紀(jì)是古生代中最老的一個紀(jì)，然后依次為奧陶紀(jì)、志留紀(jì)、泥盆紀(jì)、石炭紀(jì)和二疊紀(jì)。

72 、Obvious intrusive contact is observed between the Cambrian epimetamorphic rock system intruding into the eastern flank of the NE Heping anticlinorium and surrounding rocks.───侵位于北東向和平復(fù)式背斜東翼的寒武紀(jì)淺變質(zhì)巖系,與圍巖呈明顯的侵入接觸。

73 、County geological formation exposed by geological era, there are 7 lines (JI), the Sinian, Cambrian, Ordovician, Silurian, Cretaceous, Tertiary, Quaternary.───地質(zhì)縣境地層出露按地質(zhì)年代，有7個系（紀(jì)），即震旦系、寒武系、奧陶系、志留系、白堊系、第三系、第四系。

74 、On Sexual Dimorphism of Bradornda from Cambrian───寒武紀(jì)高肌蟲的性雙形研究

75 、Cambrian in the southeastern sedimentary copper Jilin is considered to be the products of sedimentation and later reworking.───吉林東南部寒武紀(jì)沉積銅主要為沉積和后期熱液改造綜合作用的產(chǎn)物。

76 、In Britain, Cambrian rocks are found in Wales and North-West Scotland.───在英國的威爾士和蘇格蘭的西北部，發(fā)現(xiàn)了寒武紀(jì)的巖石。

77 、The gold deposits,located in the Cambrian silicalite formation of western Qinling, are the new type stratabound gold deposit, closely associated with submarine exhalative sedimentation.───產(chǎn)于西秦嶺南亞帶寒武系硅巖建造中的金礦床，是我國境內(nèi)發(fā)現(xiàn)的一種與海底噴流作用有關(guān)的、具有獨(dú)特地質(zhì)特征的層控金礦床。

78 、If I can engineer a world to the threshold of the Cambrian explosion and let it boil over the edge on its own, that will be truly impressive.───如果我可以操控一個世界達(dá)到寒武紀(jì)大爆發(fā)的臨界點(diǎn)，然后讓它自己沸騰溢出邊界，那才是真正的永生難忘。

79 、The Xiajiadian gold deposit is a newly-discovered ore deposit occurring in the contact between Sinian and Cambrian strata .───夏家店金礦是在東秦嶺震旦系與寒武系界面新發(fā)現(xiàn)和勘查的金礦床,主要為含金角礫巖型。

80 、King, W. B. R. - The Cambrian Fauna of the Salt Range of India.───印度鹽嶺寒武紀(jì)動物群 金氏著

寒武紀(jì)的符號怎么念

寒武紀(jì)

屬于顯生宙PH的古生代Pz

符號是Є（有點(diǎn)像C中間一橫），西里爾文大寫字母（烏克蘭語）Ie，發(fā)復(fù)合音[je],類似英語yes里的ye

寒武紀(jì)的符號怎么念

發(fā)音“卡姆”，“Cambrian”，第一個字母C，為了區(qū)別于石炭系，中間加一橫，與烏克蘭語無關(guān)