?Archaean

Archaean 發(fā)音

英：[ɑ?r?ki??n]　　美：[ɑ??k??n]

英：　　美：

Archaean 中文意思翻譯

Archaean 網(wǎng)絡(luò )釋義

adj. 太古代的n. [地質(zhì)] 太古代

Archaean 短語(yǔ)詞組

1、archaean quest ─── 太古代探索

2、archaean period ─── 太古代

3、Archaean era ─── 太古代

4、archaean eon ─── 太古代

5、archaean ffxv ─── 太古代ffxv

6、archaean rna ─── 太古代核糖核酸

7、archaean craton ─── 太古代克拉通

Archaean 相似詞語(yǔ)短語(yǔ)

1、Achaean ─── n.希臘人；亞加亞人；adj.希臘的；亞加亞的

2、archaeus ─── n.活力，[醫]元氣

3、archaea ─── n.古生菌

4、Manichaean ─── adj.（與）摩尼教（有關(guān)）的；摩尼教徒的；二元論的（等于Manichean）；n.摩尼教徒；二元論者（等于Manichean）

5、archaeal ─── adj.古菌的

6、archaeans ─── adj.太古代的；n.[地質(zhì)]太古代

7、archdeacon ─── n.領(lǐng)班神父；副監督；n.(Archdeacon)人名；(英)阿奇迪肯

8、archaeo- ─── 檔案文件

9、Archaean ─── adj.太古代的；n.[地質(zhì)]太古代

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

1、K/Rb RATIOS IN ARCHAEAN GRANULITES IN THE EASTERN PART OF HEBEI PROVINCE ─── 冀東太古代麻粒巖相變質(zhì)巖中的K/Rb比值

2、Using this set of techniques to predict the development and oil/gas-bearing character of fractural reservoir of Archaean buried hill reservoir in JZS oil/gas field. ─── 利用此套技術(shù)對JZS油氣田太古界潛山儲層中裂縫性?xún)瘜影l(fā)育情況和含油氣性進(jìn)行了預測。

3、THE TECTONIC EVOLUTION OF ARCHAEAN HIGH-GRADE METAMORPHIC TERRANE,EASTERN HEBEI,CHINA ─── 冀東太古宙高級變質(zhì)區構造演化

4、The activity of H_2O,fugacity of O_2 and variation of their chemical potential during metamorphic peak of the Archaean khondalite series from Xinghe Zhuozi district,Inner Mongolia ─── 內蒙古興和-卓資太古宙孔茲巖系變質(zhì)峰期水活度、氧逸度及其化學(xué)位變化

5、GENESIS AND EVOLUTION OF THE DUCTILE DEFORMATIONAL BANDS IN DEEP TECTONIC FACIES IN THE ARCHAEAN HIGH GRADE METAMORPHIC AREA, EAST HEBEI ─── 冀東太古宙高級變質(zhì)區深部構造相韌性變形條帶的成因及演化

6、Archaean era granulite facies metamorphite series are extensively outcropped in Sa- heqiao , Hebei province. ─── 冀東遷西灑河橋是太古代麻粒巖相變質(zhì)巖系廣泛出露的地區。

7、LARGE-SCALE TRANSPOSITION IN ARCHAEAN ROCKS OF SOUTHERN JILIN PROVINCE AND ITS CONTROLLING EFFECT ON THE BIF ORE BODIES ─── 吉南太古宙巖群中的大型構造置換及其對BIF礦體的控制

8、The Xiaotazhiguo formation had been subjected to regional metamorphism in the end of the early Archaean and the metamorphic grade is granulite facies. ─── 小塔子溝組于早太古代末(2800Ma)遭受區域變質(zhì)作用,變質(zhì)程度為麻粒巖相。

9、Baoguolao gold deposit, occurred in the Archaean highgrade metamorphic granite greenstone terrance, west part of Liaoning Province, is controlled by E W trending ductile shear zones. ─── 寶國老金礦產(chǎn)于遼西太古宙高變質(zhì)綠巖帶,受近東西向韌性剪切帶控制,多金屬硫化物石英脈型,銀金礦為主要含金礦物,礦石品位高。

10、He says by examining oxidation rates they have shown the mantle has cooled several hundred degrees since the Archaean. ─── 丹尤柴夫斯基說(shuō)，通過(guò)檢測氧化的速度，他們證明了自從太古代以來(lái)，地幔冷卻了好幾百度。

11、and late Archaean greenstone belts. ─── 、晚兩期太古代綠巖帶。

12、TECTOPETROLOGY OF ARCHAEAN METAMORPHIC ROCKS IN NORTH CHINA PLATFORM AND THEIR P T CONDITIONS ─── 華北地臺北緣的構造巖石學(xué)與平衡的溫壓條件

13、The reservoir rocks are the Archaean migmatitic granite,biotite plagiogneiss,leucogranulitite and cataclasite and the Middle Proterozoic dolomite and quartzose sandstone. ─── 巖石儲集空間以密集發(fā)育的微觀(guān)裂縫系統為主,宏觀(guān)裂縫系統主要起滲流通道作用。

14、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,儲集空間主要為構造裂縫及溶蝕孔隙;

15、The ductile shear zone (DSZ) which was formed in late period of Archaean era has no direct relation with the genesis of gold deposit, but it offered conditions for the superimposition of late brittle-ductile Shear zones. ─── 太古代末形成的韌性剪切帶和金礦無(wú)直接成因聯(lián)系，但為后期脆一韌性剪切帶的疊加提供條件。

16、TWO TYPES OF ARCHAEAN META-BASALTS AND THEIR GEOTECTONIC SIGNIFICANCE ─── 太古代變質(zhì)玄武巖的地球化學(xué)特征及大地構造意義

17、pH-EVOLUTlON OF ARCHAEAN SEAWATER AND ITS RELATIONS TO ORE DEPOSITION ─── 太古代海水pH值的演化及其和成礦作用的關(guān)系

18、PTt Path and Crustal Thermodynamic Model of Late Archaean Early Proterozoic High grade Metamorphic Terrain in North China 金巍, ─── 太古宙克拉通型下地殼剖面：華北懷安-豐鎮-尚義的麻粒巖-角閃巖系

19、TWO TYPES OF ARCHAEAN GREY GNEISS IN NORTH CHINA AND THEIR GEOLOGICAL SIGNIFICANCE ─── 華北太古宙兩類(lèi)灰色片麻巖及其地質(zhì)意義

20、Nd ISOTOPIC COMPOSITION AND EVOLUTION OF THE UPPER MANTLE IN THE ARCHAEAN OF NORTH CHINA: CONSTRAINTS ON THE MANTLE HETEROGENEITY OF THE UNMETASOMATIC CONTINENTAL LITHOSPHERE ─── 華北太古代上地幔釹同位素組成、演化及對該區巖石圈地幔不均一性的制約

21、THE CORDIERITE-SILLIMANITE ASSEMBLAGE IN THE ARCHAEAN GRANULITE BELT ON NORTH CHINA PLATFORM AS AN INDICATOR FOR LOWPRESSURE GRANULITE FACIES ─── 華北地臺太古代麻粒巖相帶的堇青石-夕線(xiàn)石組合:低壓麻粒巖相的標志

22、The configuration of Ordovician of lower Palaeozoic system highly inherits that of Archaean group and both have a strong consistency. ─── 下古生界奧陶系構造具有很強的繼承性，其構造格局與太古界有很強的一致性；

23、Geochemistry of Early Archaean Glagio Amphibolites in Chaozhuang Group from Eastern Hebei Province ─── 冀東曹莊群早太古變基性火山質(zhì)斜長(cháng)角閃巖的地球化學(xué)特征

24、Hademengou gold deposit in the western portion of the northen margin of the North China Craton, is hosted by the metamorphic rocks of the Wulashan Group with New Archaean age. ─── 哈達門(mén)溝金礦床位于華北地臺北緣西段,產(chǎn)于新太古代烏拉山巖群變質(zhì)巖系中。

25、During Archaean asthenosphere-lithosphere interaction and post-Archaean interactionwith the deep mantle and other hot spots The Archaean lithospheric mantle beneath SouthAfrica experienced processes of crustal extraction. ─── 太古代巖石圈地幔以南非為代表，經(jīng)歷了從地殼物質(zhì)提取的虧損過(guò)程到與軟流圈反應和與深部熱點(diǎn)物質(zhì)作用的富集過(guò)程。

26、Progressive Metamorphic Genesis of Archaean Granulites in Central Nei Mongol ─── 內蒙古中部太古代麻粒巖遞增變質(zhì)成因

27、Archaean Eon ─── 太古宙

28、A PRELIMINARY STUDY ON ARCHAEAN GRANITIC ROCKS AND ITS ORIGIN IN THE SOUTHERN PART OF JILIN PEOVINCE ─── 吉林省南部太古宙花崗質(zhì)巖石及其成因探討

29、ON THE ORIGIN AND DEVELOPMENT OF EARTH FROM THE ARCHAEAN GNEISSES ─── 從太古代片麻巖系推測地球的成因和發(fā)展

30、Recent studies show, however, that rapakivi granites can be formed in age from Archaean to Phanerozoic and can even occur in orogen. ─── 環(huán)斑花崗巖既可以出現于從太古代到顯生宙的各個(gè)地質(zhì)時(shí)期，也可以產(chǎn)生于造山帶中。

31、Archaean cell walls lack murein, a common component of bacterial cell walls, and their lipids have ether links rather than ester links. ─── 古細菌的細胞壁缺乏細菌細胞壁組成的普遍物質(zhì)-胞壁質(zhì)，其連接是醚連接而不是酯連接。

32、CONTRASTING ARCHAEAN GRANULITE FACIES ROCKS FROM EASTERN HEBEI, NORTH CHINA ─── 冀東太古代高級變質(zhì)地體中兩類(lèi)麻粒巖相深成片麻巖

33、DEFORMATION OF ARCHAEAN WULASHAN GROUP IN GUYANG REGION OF INNER MONGOLIA ─── 內蒙古固陽(yáng)地區太古宙烏拉山群構造變形分析

34、Disintegration of the Archaean "Anshan Group" and establishment of major geological event succession in Jiapigougou gold metallogenic belt, S. Jilin ─── 吉南夾皮溝金礦帶鞍山群的解體及主要地質(zhì)事件序列的建立

35、Geodynamic Conditions for the Enrichment of Gold in Archaean Rocks ─── 太古宙巖石中金富集的地球動(dòng)力學(xué)條件

36、Substantial changes consist in the transfer of Wutaian into Archaean and the alteration of lower limit of Changchengian system from 1850 to 1700 Ma, both based on new interpretation of isotopic dating. ─── 劃分中的重要改變是根據新的年齡值數據將五臺群歸入太古代,將長(cháng)城系底界改為1700Ma;

37、However, contrary to previous views, there is no isotopic evidence that Archaean rocks are present in the Mashan Complex. ─── 然而，與以前的認識相反，麻山雜巖不存在具有太古宙基底的同位素證據。

38、The configuration of Ordovician of lower Palaeozoic system highly inherits that of Archaean group and both have a strong consistency. ─── 下古生界奧陶系構造具有很強的繼承性，其構造格局與太古界有很強的一致性；

39、THE CHARACTERISTICS AND GENESIS OF THE ARCHAEAN MIGMATITE IN QIAN-AN CAUNTY, HOUBEI PROVINCE ─── 冀東遷安太古界混合巖的特征和成因

40、Archaean granulite belts are just the product of plate-tectonic movement of rigid Archaean crust. ─── 太古宙麻粒巖帶就是太古畝地殼發(fā)生剛性板塊運動(dòng)的直接產(chǎn)物。

41、The complete historical processes of the crust growth from the Archaean to the Cenozoic eras are recorded and remained in South China continent. ─── 華南大陸記錄和保存了自太古代至今大陸生長(cháng)層完整的歷史過(guò)程。

42、Archaean era granulite facies metamorphite series are extensively outcropped in Sa - heqiao, Hebei province. ─── 冀東遷西灑河橋是太古代麻粒巖相變質(zhì)巖系廣泛出露的地區。

43、Single-Grain Evaporation Zircon Pb-Pb Ages of Guandi Complex, Zhoukoudian Area, Western Hills of Beijing: Archaean Genesis and Cratonization Events of the North China Craton ─── 北京西山周口店關(guān)坻雜巖蒸發(fā)法鋯石Pb-Pb年齡:太古宙成因和克拉通化事件證據

44、Contrasting Metamorphic P T Paths of Archaean High Pressure Granulites from the North ─── 華北太古宙高壓基性麻粒巖的兩類(lèi)PT軌跡及其構造意義:礦物化學(xué)和變質(zhì)作用研究

45、THREE EARLY ARCHAEAN GNEISSES AROUND SANTUNYING OF QIANXI,EASTERN HEBEI,CHINA:GEOCHEMISTRY AND PETROGENESIS ─── 冀東遷西三屯營(yíng)地區早太古宙三組片麻巖的巖石地球化學(xué)及其成因

46、The wall rocks of gold deposits located in Zhaoyuan gold mineralization area were rooted in metamorphic rocks in Jiaodong rock group in Archaean era and granites in Mesozoic era. ─── 山東招遠金礦集中區金礦床的圍巖為新太古代膠東巖群變質(zhì)巖和中生代花崗巖。

47、The Archaean and Katarchaean units are preserved mainly as relic masses ─── 太古界與遠太古界主要作為殘余體保存下來(lái)。

48、Late Archaean Mafic ultramafic Rocks from the Wutaishan, Shanxi Province: a Possible Ophiolite Melange ─── 山西省五臺山晚太古代鎂鐵質(zhì)-超鎂鐵質(zhì)巖: 一種可能的古蛇綠混雜巖

49、During the Early Archaean only appeared some nuclei of palaeocontinent in small size with low uranium contents in rocks and the sial was formed in the late stage of their evolution. ─── 太古代早期只出現小面積古陸核,巖石含鈾量低,硅鋁殼演化晚。

50、The test of glycerol diether analog suggested that 3 archaean halophiles contained typical glycerol diether analog. ─── 對細胞壁的甘油二醚衍生物測定顯示，3株嗜鹽古細菌均含有典型的甘油二醚類(lèi)衍生物。

51、The Nd model ages show that there exist an Archaean basement in the central uprift of the Tarim Basin(3.2-2.5Ga). ─── Nd模式年齡還表明柯坪－阿克蘇地區存在太古宙基底（3.2－2.5Ga）。

52、Archaean era ─── 太古代

53、THE FORMATION AND EVOLUTION OF ARCHAEAN GRANITOID ROCKS FROM EAST HEBEl AND SOUTHWEST LIAONING PROVINCES , CHINA ─── 冀東-遼西南太古代花崗質(zhì)巖石的形成與演化

54、ARCHAEAN GRANULITE AND SUBDIVISION OF LOWER CRUST IN EASTERN HEBEI, CHINA ─── 冀東太古宙麻粒巖及下地殼分層的討論

55、THE ORIGIN OF THE METAMORPHIC CONGLOMERATE OF THE ARCHAEAN ZHUZHANGZI GROUP, E. HEBEI PROVINCE, CHINA ─── 冀東朱杖子群老爺廟變質(zhì)礫巖的成因

56、RESEARCH ON GEOLOGICAL PROBLEMS OF ARCHAEAN HIGH-GRADE TERRANE IN EASTERN HEBEI PROVINCE ─── 冀東太古宙高級變質(zhì)巖區若干地質(zhì)問(wèn)題的研究

57、The gold deposits in Archaean granite-greenstone belt can be devided into syntectonic primary gold deposits and post-tectonic regenerated gold deposits associated with anatexis magmatic rocks. ─── 以太古宙花崗巖-綠巖帶為容礦巖的金礦床系列又劃分為綠巖帶同構造期初生型金礦床和綠巖帶后構造期與中生代殼源深熔花崗巖有關(guān)的再生型金礦床。

58、THE GEOLOGICAT OUTLINE AND RETROGRADE REACTIONS OF THE ARCHAEAN QIANXI GROUP IN EASTERN HEBEI PROVINCE, CHINA ─── 冀東遷安南區遷西群的地質(zhì)特征與退變質(zhì)反應

59、- Archaean ( a well-known R.I. ─── fantasy MMORPG )太古代 (一款知名的R.

60、[Zhang Yixia,Ye Tingsong and Yan Hongquan,et al.1986.The Archaean Geology and Banded Iron Formation of Jidong,Hebei Province.Geological Monograph Series 1.No.6. ─── 張貽俠,葉廷松,閻鴻銓,等.1986.冀東太古代地質(zhì)及變質(zhì)鐵礦.中華人們共和國地質(zhì)礦床部地質(zhì)專(zhuān)報-區域地質(zhì)第6號,北京:地質(zhì)出版社,179.

61、In the Dabieshan area, the late Archaean metamorphic rocks,here termed as the Dabie Group, are complexly deformed. ─── 大別山區晚太古代大別群變質(zhì)巖系,經(jīng)歷了復雜的變形過(guò)程。

62、Archaean Group ─── 太古宇

63、GEOLOGICAL FEATURES AND ORIGIN OF ARCHAEAN GRANITIC PLUTONS IN EAST FUSHUN, LIAONING ─── 撫順東部地區太古宙花崗質(zhì)侵人體的地質(zhì)特征及成因

64、However, many current studies failed to notice certain macroscopic disparities between Archaean and Phanerozoic geological entities rationally and understand global gold occurrences a. ─── 但是,目前眾多研究對前寒武地質(zhì)與顯生宙地質(zhì)的宏觀(guān)差異、世界金礦一些總體規律及若干具體大地構造背景等尚認識不足。

65、EARLY ARCHAEAN WHOLE-ROCK ISOCHRON OF GNEISSES IN SANTUNYING, EASTERN HEBEI, CHINA ─── 冀東三屯營(yíng)地區片麻巖的早太古宙全巖年齡

66、ISOBARIC COOLING (IBC) P-T-t PATH FOR THE WESTERN PORTION OF ARCHAEAN MIYUN COMPLEX, BEIJING: CONSTRAINTS AND ITS GEODYNAMIC GENESIS ─── 密云雜巖西段等壓冷卻P－T－t軌跡確定及地球動(dòng)力學(xué)成因

67、All orebodies are gold quartz vein type and hosted in New Archaean metamorphic quartz diorite and plagiogranite. ─── 容礦巖系為新太古代變質(zhì)石英閃長(cháng)巖、斜長(cháng)花崗巖。

68、There is clear feature of zonations in Si, Fe, Mg and Mg/(Mg + Fe) for amphibole in Archaean tonalitic gneisses in Malanyu area, eastern Hebei Province. ─── 冀東馬蘭峪地區出露較大面積的太古宙含紫蘇輝石的英云閃長(cháng)質(zhì)片麻巖,其中角閃石礦物的Si、Fe、Mg、Mg/(Mg+Fe)等呈明顯的環(huán)帶特點(diǎn)。

69、LATE ARCHAEAN GREENSTONE BELT IN ZHIFANG AREA, TAIAN, SHANDONG, AND THE CHARACTERISTICS OF THE GOLD MINERALIZATION THERE ─── 山東泰安紙房地區太古代晚期綠巖帶及其金礦化地質(zhì)特征

70、The Archaean era limestone aquifer close to No. 10 coalbed is the direct aquifer of it. ─── 距離其較近的太灰含水層，是10煤開(kāi)采的直接充水含水層。

71、An Oblique Cross Section of Archaean Continental Crust in Shanxi Hebei Nei Mongol Jnnctnve Area, North China Craton ─── 太古宙克拉通型下地殼剖面：華北懷安－豐鎮－尚義的麻粒巖－角閃巖系

72、Keywords Erdaogou gold deposit;ore-forming fluid;physicochemical conditions;Archaean greenstone belt type gold deposit;Archean high grade metamorphic terrains; ─── 二道溝金礦;成礦流體;物理化學(xué)條件;太古代綠巖帶金礦;太古代高級變質(zhì)地體;

73、A PRELIMINARY STUDY ON THE CHARACTERISTICS OF PETROLOGY AND AGE OF THE METAMORPHIC COMPLEXES FOR THE ARCHAEAN GRANULITE FACIES IN-THE LAOJINCHANG REGION, JILIN ─── 吉林樺甸老金廠(chǎng)地區太古代麻粒巖相變質(zhì)雜巖的巖石學(xué)特征及其時(shí)代的討論

74、In fact, all life during the more than one billion years of the Archaean was bacterial. ─── 實(shí)際上，所有生活在Archaean的超過(guò)一十億年期間是細菌的。

75、The lie concealed carbonate cranny Karst water-bearing rock group which mainly are Ordovician distributing outer of the the Archaean era limestone aquifer are the powerful supply of that. ─── 在該含水層外圍,以?shī)W陶系為主的隱伏型碳酸鹽類(lèi)裂隙巖溶含水巖組,是其強大的補給來(lái)源,這對礦井安全威脅較大。

76、In fact, all life during the more than one billion years of the Archaean was bacterial. ─── 實(shí)際上,所有生活在A(yíng)rchaean的超過(guò)一十億年期間是細菌的。

77、It was early in the Archaean Era, 3.8 To 2.5 Billion years ago, that life first appeared on Earth. ─── 它在及早在A(yíng)rchaean時(shí)代,3.8到2.5十億年前,生活第一次出現在地球上。

78、From the Archaean to the Palaeozoic, Shandong was controlled predominantly by the E-W extending structural systems, and the basement geosynclines and platform sedimentary covers were formed. ─── 太古代至古生代山東主要受到了東西向構造體系的控制,形成了基底“地槽”和“地臺”蓋層。

79、Evidence for life has bee found in the Archaean about 3. 8 billion years ago, but life did not become abundant until the Phanerozoic. ─── 最早的生命跡象發(fā)現存在于距今38億年的太古代，但是地球上的生命在顯生宙之前并不豐富。

80、THE HUADIAN ARCHAEAN COMPLEX:MINERAL CHEMISTRY AND P-T CONDITIONS OF METAMORPHISM ─── 吉林樺甸太古代雜巖的礦物化學(xué)和變質(zhì)作用溫壓條件

81、A PRELIMINARY STUDY ON STRATABOUND CHARACTERISTICS OF THE GOLD DEPOSITS IN ARCHAEAN GREENSTON IN SOUTHERN JILIN AND NORTHERN LAONING ─── 吉南遼北太古代綠巖金礦層控特征的探討

82、PTt Path and Crustal Thermodynamic Model of Late Archaean Early Proterozoic High grade Metamorphic Terrain in North China ─── 華北晚太古代－早元古代高級變質(zhì)區的變質(zhì)PTt軌跡及其地殼熱動(dòng)力學(xué)演化模式

83、Archaean cell walls lack murein, and their lipids have ether links rather than ester links. ─── 細胞壁缺乏胞壁質(zhì)，其連接是醚連接而不是酯連接。

84、Unit one is the oldest rocks in the region, which is at least older than late Archaean(>2800Ma). ─── 其中,組合(1)是區內最古老的物質(zhì)組成,其形成時(shí)代至少應在晚太古代以前(>2800Ma).

85、Stretching Southwards,it could connect the Late Archaean Yakou Gneiss and its equivalents in Western Sichuan and Central Yunnan. ─── 它與川滇交界區晚太古代埡口片麻巖等一起構成川西滇中地區的片麻巖基底.

86、Most of 9 morderately halophilies were Gram-positive and rod and did’t produce any pigment. 3 archaean halophiles were Gram-negative and coccus, and produced red pigment. ─── 9株中度嗜鹽菌多為革蘭氏陽(yáng)性菌，呈桿狀，不產(chǎn)生色素。3株嗜鹽古細菌均為革蘭氏陰性菌，呈球狀，能產(chǎn)生紅色素。

87、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，儲集空間主要為構造裂縫及溶蝕孔隙；

88、THE ARCHAEAN TONALITES IN QIXIA AREA, SHANDONG ─── 山東棲霞地區太古宙英云閃長(cháng)巖

89、GOLD MINERALIZATION IN THE ARCHAEAN HIGH GRADE METAMORPHIC TERRAINS OF NORHT CHINA PLATFORM ─── 華北地臺太古代高級變質(zhì)地體中的金礦化