archaean

archaean

1. 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株中度嗜盐菌多为革兰氏阳性菌，呈杆状，不产生色素。3株嗜盐古细菌均为革兰氏阴性菌，呈球状，能产生红色素。

2. - Archaean ( a well-known R.I.

fantasy MMORPG )太古代 (一款知名的R.

3. The Nd model ages show that there exist an Archaean basement in the central uprift of the Tarim Basin(3.2-2.5Ga).

Nd模式年龄还表明柯坪－阿克苏地区存在太古宙基底（3.2－2.5Ga）。

4. and late Archaean greenstone belts.

、晚两期太古代绿岩带。

5. The configuration of Ordovician of lower Palaeozoic system highly inherits that of Archaean group and both have a strong consistency.

下古生界奥陶系构造具有很强的继承性，其构造格局与太古界有很强的一致性；

6. He says by examining oxidation rates they have shown the mantle has cooled several hundred degrees since the Archaean.

丹尤柴夫斯基说，通过检测氧化的速度，他们证明了自从太古代以来，地幔冷却了好几百度。

7. Keywords Erdaogou gold deposit;ore-forming fluid;physicochemical conditions;Archaean greenstone belt type gold deposit;Archean high grade metamorphic terrains;

二道沟金矿;成矿流体;物理化学条件;太古代绿岩带金矿;太古代高级变质地体;

8. ON THE ORIGIN AND DEVELOPMENT OF EARTH FROM THE ARCHAEAN GNEISSES

从太古代片麻岩系推测地球的成因和发展

9. 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.

以太古宙花岗岩-绿岩带为容矿岩的金矿床系列又划分为绿岩带同构造期初生型金矿床和绿岩带后构造期与中生代壳源深熔花岗岩有关的再生型金矿床。

10. 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,目前众多研究对前寒武地质与显生宙地质的宏观差异、世界金矿一些总体规律及若干具体大地构造背景等尚认识不足。

11. 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.

储集层由太古界变质岩、下古生界碳酸盐岩和中生界砂岩、火山岩组成,储集空间主要为构造裂缝及溶蚀孔隙;

12. 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.

储集层由太古界变质岩、下古生界碳酸盐岩和中生界砂岩、火山岩组成，储集空间主要为构造裂缝及溶蚀孔隙；

13. Unit one is the oldest rocks in the region, which is at least older than late Archaean(>2800Ma).

其中,组合(1)是区内最古老的物质组成,其形成时代至少应在晚太古代以前(>2800Ma).

14. THE FORMATION AND EVOLUTION OF ARCHAEAN GRANITOID ROCKS FROM EAST HEBEl AND SOUTHWEST LIAONING PROVINCES , CHINA

冀东-辽西南太古代花岗质岩石的形成与演化

15. EARLY ARCHAEAN WHOLE-ROCK ISOCHRON OF GNEISSES IN SANTUNYING, EASTERN HEBEI, CHINA

冀东三屯营地区片麻岩的早太古宙全岩年龄

16. CONTRASTING ARCHAEAN GRANULITE FACIES ROCKS FROM EASTERN HEBEI, NORTH CHINA

冀东太古代高级变质地体中两类麻粒岩相深成片麻岩

17. K/Rb RATIOS IN ARCHAEAN GRANULITES IN THE EASTERN PART OF HEBEI PROVINCE

冀东太古代麻粒岩相变质岩中的K/Rb比值

18. THE TECTONIC EVOLUTION OF ARCHAEAN HIGH-GRADE METAMORPHIC TERRANE,EASTERN HEBEI,CHINA

冀东太古宙高级变质区构造演化

19. GENESIS AND EVOLUTION OF THE DUCTILE DEFORMATIONAL BANDS IN DEEP TECTONIC FACIES IN THE ARCHAEAN HIGH GRADE METAMORPHIC AREA, EAST HEBEI

冀东太古宙高级变质区深部构造相韧性变形条带的成因及演化

20. RESEARCH ON GEOLOGICAL PROBLEMS OF ARCHAEAN HIGH-GRADE TERRANE IN EASTERN HEBEI PROVINCE

冀东太古宙高级变质岩区若干地质问题的研究

21. ARCHAEAN GRANULITE AND SUBDIVISION OF LOWER CRUST IN EASTERN HEBEI, CHINA

冀东太古宙麻粒岩及下地壳分层的讨论

22. Geochemistry of Early Archaean Glagio Amphibolites in Chaozhuang Group from Eastern Hebei Province

冀东曹庄群早太古变基性火山质斜长角闪岩的地球化学特征

23. THE ORIGIN OF THE METAMORPHIC CONGLOMERATE OF THE ARCHAEAN ZHUZHANGZI GROUP, E. HEBEI PROVINCE, CHINA

冀东朱杖子群老爷庙变质砾岩的成因

24. THE GEOLOGICAT OUTLINE AND RETROGRADE REACTIONS OF THE ARCHAEAN QIANXI GROUP IN EASTERN HEBEI PROVINCE, CHINA

冀东迁安南区迁西群的地质特征与退变质反应

25. THE CHARACTERISTICS AND GENESIS OF THE ARCHAEAN MIGMATITE IN QIAN-AN CAUNTY, HOUBEI PROVINCE

冀东迁安太古界混合岩的特征和成因

26. THREE EARLY ARCHAEAN GNEISSES AROUND SANTUNYING OF QIANXI,EASTERN HEBEI,CHINA:GEOCHEMISTRY AND PETROGENESIS

冀东迁西三屯营地区早太古宙三组片麻岩的岩石地球化学及其成因

27. Archaean era granulite facies metamorphite series are extensively outcropped in Sa- heqiao , Hebei province.

冀东迁西洒河桥是太古代麻粒岩相变质岩系广泛出露的地区。

28. 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.

冀东马兰峪地区出露较大面积的太古宙含紫苏辉石的英云闪长质片麻岩,其中角闪石矿物的Si、Fe、Mg、Mg/(Mg+Fe)等呈明显的环带特点。

29. Progressive Metamorphic Genesis of Archaean Granulites in Central Nei Mongol

内蒙古中部太古代麻粒岩递增变质成因

30. 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

内蒙古兴和-卓资太古宙孔兹岩系变质峰期水活度、氧逸度及其化学位变化

31. DEFORMATION OF ARCHAEAN WULASHAN GROUP IN GUYANG REGION OF INNER MONGOLIA

内蒙古固阳地区太古宙乌拉山群构造变形分析

32. 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.

划分中的重要改变是根据新的年龄值数据将五台群归入太古代,将长城系底界改为1700Ma;

33. 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.

利用此套技术对JZS油气田太古界潜山储层中裂缝性储集层发育情况和含油气性进行了预测。

34. 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

北京西山周口店关坻杂岩蒸发法锆石Pb-Pb年龄:太古宙成因和克拉通化事件证据

35. TECTOPETROLOGY OF ARCHAEAN METAMORPHIC ROCKS IN NORTH CHINA PLATFORM AND THEIR P T CONDITIONS

华北地台北缘的构造岩石学与平衡的温压条件

36. GOLD MINERALIZATION IN THE ARCHAEAN HIGH GRADE METAMORPHIC TERRAINS OF NORHT CHINA PLATFORM

华北地台太古代高级变质地体中的金矿化

37. THE CORDIERITE-SILLIMANITE ASSEMBLAGE IN THE ARCHAEAN GRANULITE BELT ON NORTH CHINA PLATFORM AS AN INDICATOR FOR LOWPRESSURE GRANULITE FACIES

华北地台太古代麻粒岩相带的堇青石-夕线石组合:低压麻粒岩相的标志

38. 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

华北太古代上地幔钕同位素组成、演化及对该区岩石圈地幔不均一性的制约

39. TWO TYPES OF ARCHAEAN GREY GNEISS IN NORTH CHINA AND THEIR GEOLOGICAL SIGNIFICANCE

华北太古宙两类灰色片麻岩及其地质意义

40. Contrasting Metamorphic P T Paths of Archaean High Pressure Granulites from the North

华北太古宙高压基性麻粒岩的两类PT轨迹及其构造意义:矿物化学和变质作用研究

41. PTt Path and Crustal Thermodynamic Model of Late Archaean Early Proterozoic High grade Metamorphic Terrain in North China

华北晚太古代－早元古代高级变质区的变质PTt轨迹及其地壳热动力学演化模式

42. The complete historical processes of the crust growth from the Archaean to the Cenozoic eras are recorded and remained in South China continent.

华南大陆记录和保存了自太古代至今大陆生长层完整的历史过程。

43. Archaean cell walls lack murein, a common component of bacterial cell walls, and their lipids have ether links rather than ester links.

古细菌的细胞壁缺乏细菌细胞壁组成的普遍物质-胞壁质，其连接是醚连接而不是酯连接。

44. LARGE-SCALE TRANSPOSITION IN ARCHAEAN ROCKS OF SOUTHERN JILIN PROVINCE AND ITS CONTROLLING EFFECT ON THE BIF ORE BODIES

吉南太古宙岩群中的大型构造置换及其对BIF矿体的控制

45. Disintegration of the Archaean "Anshan Group" and establishment of major geological event succession in Jiapigougou gold metallogenic belt, S. Jilin

吉南夹皮沟金矿带鞍山群的解体及主要地质事件序列的建立

46. A PRELIMINARY STUDY ON STRATABOUND CHARACTERISTICS OF THE GOLD DEPOSITS IN ARCHAEAN GREENSTON IN SOUTHERN JILIN AND NORTHERN LAONING

吉南辽北太古代绿岩金矿层控特征的探讨

47. THE HUADIAN ARCHAEAN COMPLEX:MINERAL CHEMISTRY AND P-T CONDITIONS OF METAMORPHISM

吉林桦甸太古代杂岩的矿物化学和变质作用温压条件

48. A PRELIMINARY STUDY ON THE CHARACTERISTICS OF PETROLOGY AND AGE OF THE METAMORPHIC COMPLEXES FOR THE ARCHAEAN GRANULITE FACIES IN-THE LAOJINCHANG REGION, JILIN

吉林桦甸老金厂地区太古代麻粒岩相变质杂岩的岩石学特征及其时代的讨论

49. 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岗质岩石及其成因探讨

50. 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.

哈达门沟金矿床位于华北地台北缘西段,产于新太古代乌拉山岩群变质岩系中。

51. 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.

在该含水层外围,以奥陶系为主的隐伏型碳酸盐类裂隙岩溶含水岩组,是其强大的补给来源,这对矿井安全威胁较大。

52. In the Dabieshan area, the late Archaean metamorphic rocks,here termed as the Dabie Group, are complexly deformed.

大别山区晚太古代大别群变质岩系,经历了复杂的变形过程。

53. Archaean era

太古代

54. TWO TYPES OF ARCHAEAN META-BASALTS AND THEIR GEOTECTONIC SIGNIFICANCE

太古代变质玄武岩的地球化学特征及大地构造意义

55. 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.

太古代岩石圈地幔以南非为代表，经历了从地壳物质提取的亏损过程到与软流圈反应和与深部热点物质作用的富集过程。

56. 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.

太古代早期只出现小面积古陆核,岩石含铀量低,硅铝壳演化晚。

57. 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.

太古代末形成的韧性剪切带和金矿无直接成因联系，但为后期脆一韧性剪切带的叠加提供条件。

58. pH-EVOLUTlON OF ARCHAEAN SEAWATER AND ITS RELATIONS TO ORE DEPOSITION

太古代海水pH值的演化及其和成矿作用的关系

59. 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.

太古代至古生代山东主要受到了东西向构造体系的控制,形成了基底“地槽”和“地台”盖层。

60. Archaean Group

太古宇

61. Archaean Eon

太古宙

62. 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壳剖面：华北怀安-丰镇-尚义的麻粒岩-角闪岩系

63. 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壳剖面：华北怀安－丰镇－尚义的麻粒岩－角闪岩系

64. Geodynamic Conditions for the Enrichment of Gold in Archaean Rocks

太古宙岩石中金富集的地球动力学条件

65. The Archaean and Katarchaean units are preserved mainly as relic masses

太古界与远太古界主要作为残余体保存下来。

66. Stretching Southwards,it could connect the Late Archaean Yakou Gneiss and its equivalents in Western Sichuan and Central Yunnan.

它与川滇交界区晚太古代垭口片麻岩等一起构成川西滇中地区的片麻岩基底.

67. 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Archaean时代,3.8到2.5十亿年前,生活第一次出现在地球上。

68. 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.

宝国老金矿产于辽西太古宙高变质绿岩带,受近东西向韧性剪切带控制,多金属硫化物石英脉型,银金矿为主要含金矿物,矿石品位高。

69. In fact, all life during the more than one billion years of the Archaean was bacterial.

实际上,所有生活在Archaean的超过一十亿年期间是细菌的。

70. All orebodies are gold quartz vein type and hosted in New Archaean metamorphic quartz diorite and plagiogranite.

容矿岩系为新太古代变质石英闪长岩、斜长花岗岩。

71. ISOBARIC COOLING (IBC) P-T-t PATH FOR THE WESTERN PORTION OF ARCHAEAN MIYUN COMPLEX, BEIJING: CONSTRAINTS AND ITS GEODYNAMIC GENESIS

密云杂岩西段等压冷却P－T－t轨迹确定及地球动力学成因

72. The test of glycerol diether analog suggested that 3 archaean halophiles contained typical glycerol diether analog.

对细胞壁的甘油二醚衍生物测定显示，3株嗜盐古细菌均含有典型的甘油二醚类衍生物。

73. The Xiaotazhiguo formation had been subjected to regional metamorphism in the end of the early Archaean and the metamorphic grade is granulite facies.

小塔子沟组于早太古代末(2800Ma)遭受区域变质作用,变质程度为麻粒岩相。

74. 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.

山东招远金矿集中区金矿床的围岩为新太古代胶东岩群变质岩和中生代花岗岩。

75. THE ARCHAEAN TONALITES IN QIXIA AREA, SHANDONG

山东栖霞地区太古宙英云闪长岩

76. LATE ARCHAEAN GREENSTONE BELT IN ZHIFANG AREA, TAIAN, SHANDONG, AND THE CHARACTERISTICS OF THE GOLD MINERALIZATION THERE

山东泰安纸房地区太古代晚期绿岩带及其金矿化地质特征

77. Late Archaean Mafic ultramafic Rocks from the Wutaishan, Shanxi Province: a Possible Ophiolite Melange

山西省五台山晚太古代镁铁质-超镁铁质岩: 一种可能的古蛇绿混杂岩

78. The reservoir rocks are the Archaean migmatitic granite,biotite plagiogneiss,leucogranulitite and cataclasite and the Middle Proterozoic dolomite and quartzose sandstone.

岩石储集空间以密集发育的微观裂缝系统为主,宏观裂缝系统主要起渗流通道作用。

79. [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.

张贻侠,叶廷松,阎鸿铨,等.1986.冀东太古代地质及变质铁矿.中华人们共和国地质矿床部地质专报-区域地质第6号,北京:地质出版社,179.

80. GEOLOGICAL FEATURES AND ORIGIN OF ARCHAEAN GRANITIC PLUTONS IN EAST FUSHUN, LIAONING

抚顺东部地区太古宙花岗质侵人体的地质特征及成因