泥盆紀 的英文怎麼說

中文拼音 [pén]
泥盆紀 英文
devonia eriod
  • : 泥名詞1 (含水的半固體狀的土) mud; mire 2 (像泥的東西) any paste like matter; mashed vegetable...
  • : 1. (盛東西或洗東西用的器具) basin; tub; pot 2. (姓氏) a surname
  • : 紀名詞(姓氏) a surname
  1. 2. tazhong ancient uplift originated from normal fault in paleozoic, hydrocarbon formed in ordovician period, structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period, and it provided geologic background for the deposit of silurian - devonian stratum. tazhong uplift formed at the end devonian, ancient reservoir was destroyed and asphaltum sandstone formed, structure deformation more destroyed ancient reservoir in early permian, after then the major of structure deformation is regulation

    塔中隆起源於早古生代拉張背景下的正斷層,寒武-奧陶為其烴源巖形成的重要時期;早奧陶世末-晚奧陶世末的構造反轉是塔中隆起的主要形成期,同時也為志留系形成地層及復合圈閉提供了古地理背景;志留?泥盆紀塔里木地南北緣均轉為活動大陸邊緣,形成了大量的斷裂和不整合;泥盆紀末塔中鼻狀隆起基本定型,古油藏遭受破壞,形成了瀝青砂巖;早二疊世晚期的構造變形使古油藏遭受進一步的破壞;二疊后構造變動主要以調節為主。
  2. The late ordovician - silurian - devonian - early carboniferous stratigraphic division and correlation, including the chronologic correlation of the donghe sandstone, which are the old great difficult key stratigraphic problems interfering with the development of the oil and gas exploration in the tarim basin, are synthetic studied by systematically applying chemobiostratigraphy. several important relevant stratigraphic boundaries are recognized, and the donghe sandstone is attributed to the frasnian, late devonian. the results of the study in particular proves that chemo - biostratigraphy has great significance and is a practical tool for high resolution stratigraphic division and correlation, especially for the region and or the bed with rare fossils

    首次系統應用化學生物地層學對長期遺留的嚴重阻礙了油氣勘探開發步伐的塔里木地重大疑難地層問題:晚奧陶世志留泥盆紀早石炭世地層劃分對比和東河砂巖時代等進行了綜合研究,釐定了幾條重要的相關地層界線,並將東河砂巖的時代確定為泥盆紀世弗拉斯期。這些研究成果表明,化學生物地層學對高解析度地層劃分對比尤其是對在化石缺乏地區和層段進行地層劃分對比工作有重要的意義和實用價值。
  3. Devonian biostratigraphy of dushan, southern guizhou and its coral extinction events

    貴州獨山泥盆紀生物地層以及珊瑚的四次滅絕事件的研究
  4. During the devonian, 410 million years ago, two major animal groups dominated the land

    泥盆紀期間, 410百萬年前,二個主要動物小組控制了土地。
  5. Mineral, palaeontology, middle devonian, permian to early jurassic, and cretaceous

    收藏礦物、古生物學、中泥盆紀、二疊到早期的侏羅和白惡
  6. The sequence of the strata may be correlated with the devonian period bulakebashi formation in west section of east kunlun

    該套地層可與東昆侖西段泥盆紀布拉克巴什組相對比。
  7. It contains the deeply dissected bungle bungle range composed of devonian - age quartz sandstone eroded over a period of 20

    這些成行成列的塔形或圓錐形的山巒,由泥盆紀時代的石英砂構成。
  8. The reefs widely developed from sinian to neogene in china, with main reef - forming stages in devonian, permian and neogene, respectively

    摘要中國生物礁從震旦至新近均有發育,分佈范圍廣,並有泥盆紀、二疊和新近3個主要造礁期。
  9. These geomorphic units of paleogeography constitute the basic model of paleocontinent, littoral - neritic sea and carbonate plateform at that stage, and this depositional model is similar to the pattern of the east china continent and ocean, which is the result of evolution during the past long geologic age

    這些古地理地貌單元構成了湖北省泥盆紀時期古陸濱淺海和碳酸鹽巖臺地的基本沉積模式,這種沉積模式與現今中國東海大陸、海洋格局基本一致,亦是經過了漫長地質歷史時期演化,而形成現今這種格局的。
  10. ( 4 ) the formation and growth of structural traps and stratigraphic - unconformity traps in the area is controlled by three compressive stages of silurian - devonian, late permian - tertiary and oligocene - quaternary ; non - structural and compound traps mainly grew in the early paleozoic. structural traps mostly grew in the late paleozoic and the cenozoic and mostly grew on the north and south belts ; non - structural traps mostly grew in the northern area of the hetian concave. most traps in the area formed or typed at last in the himalayan episode, dispersed on the north and south belts

    ( 4 )研究區構造與地層不整合圈閉的形成和發育受志留-泥盆紀、晚二疊世-第三、漸新世-第四三個擠壓階段的控制;早古生代主要發育非構造圈閉和復合圈閉,晚古生代和新生代則主要發育構造圈閉:構造圈閉主要發育在南北兩帶上,其次為中帶;非構造圈閉主要發育在和田凹陷以北的地區;研究區內大多數圈閉是喜山期形成或最終定型的,在南北兩帶都有分佈,而海西期圈閉主要分佈於研究區中帶瑪南構造帶處。
  11. The first tetrapods, or land - living vertebrates, appeared during the devonian, as did the first terrestrial arthropods, including wingless insects and the earliest arachnids which had already ventured onto land during the silurian

    第一tetrapods ,或土地生存脊椎動物,出現在泥盆紀期間,象第一地球節肢動物,包括已經冒險土地在西里瑞斯人期間的無翼的昆蟲和最早期的蜘蛛綱的動物。
  12. A sequence of paralic strata which contains biota fossils from early - middle devonian is found in bukadaban district in west - middle section of east kunlun mt. and it is certained there is the strata of devonian period

    摘要在東昆侖中西段布喀達阪峰地區發現了一套含早中世生物化石的海陸交互相地層,從而確定了該地區泥盆紀地層的存在。
  13. This paper emphasize the research of geometry, kinematics, age of formation of oblique - thrustin. it is discussed that geological significance of obligue - trusting. ( 1 ) this paper classified the strata of sertengshan - xitieshan in northern qaidam basin into daken - dabanyan group in lower proterozoic, tanjianshan group in ordovician - silurian period, aimunike group in upper devonian period and guokesan formation of zhongwu - nunsan group in permo - carboniferous

    ( 1 )對柴達木地北緣的賽什騰? ?錫鐵山一帶出露的地層進行了較為系統的劃分,釐定了古元古代達肯大坂巖群、奧陶? ?志留灘間山(巖)群、泥盆紀統埃姆尼克群、石炭? ?二疊中吾農山群果可山組。
  14. The results indicate that these parameters in profile change closely with geotectonic cycles as follows : sulfur, colloid and asphaltene contents keep the lowest values in devonian, triassic, jurassic and tertiary ; they are in accordance with regressive geotectonic phases, of which the maximum values appear to be correspond to the largest - scale marine transgressions occurred in caledonian cycle, hercynian cycle and middle phase of alpine cycle

    指出,這些石油參數在剖面上的變化與大地構造旋迴有密切關系:硫,膠質和瀝青質的含量在泥盆紀、三疊、侏羅和新近為最低值,它們與海退構造階段相一致;石油化學成分最大值與加里東旋迴、海西旋迴和阿爾卑斯旋迴中期的最大海侵相一致。
  15. Devonian fossil plant considered one of the earliest forms of vascular land plants ; similar to genus rhynia but smaller

    被認為是有脈管的陸地植物的最初形式之一的泥盆紀化石植物;與鹿角蕨屬相似,較小。
  16. On the base of fully utilizing the available data about tectonic maps and structural elements, the present paper has made synthesized research that used the ways of stratigraphic sequence edge unconformity analysis and stratigraphic thickness correlation analysis, and combined seismic - data interpretation, review of paleo - structure and ancient landform and research of tectonic evolution and petroleum system, and combined region and location, plane and profile and time and spatial. by the synthesis analysis on tectonic evolution of hetian paleo - uplift in tarim basin, the results indicate that : ( 1 ) hetian paleo - uplift is a sedimental and erosional paleo - uplift. the formation and evolution of the hetian paleo - uplift experienced three stages, that is, the uplifting and eroding stage of the caledonian period, the depositional stage of the hercynian period and the destroying stage of the himalayan period, and evolved from paleo - lift to inclining strap at last

    本文採用地質和地球物理相結合的研究思路,運用多種技術手段和方法;在充分利用已有構造圖資料和構造要素資料的基礎上,運用地層層序邊界不整合分析法、地層厚度對比分析法,結合地震資料的精細解釋、古構造和古地貌的恢復、構造演化史研究、含油氣系統的研究,和區域和局部、平面和剖面、時間和空間的結合研究,對塔里木地和田古隆起構造演化及油氣關系進行了綜合分析,認為: ( 1 )和田古隆起為一沉積?剝蝕性古隆起;形成於志留-泥盆紀;其構造演化可分為三個階段,即加里東期的抬升剝蝕階段、海西期的沉積階段和喜山期的破壞階段,最終由古隆起演變為一斜坡帶。
  17. The oldest exposed rocks are devonian fluvial sediments that were deposited 400 million years ago. the region was subsequently inundated by a shallow sea

    年代最久遠的巖石是四億年前泥盆紀時期由河流沖積形成的沉積巖。
  18. Hong kong lies on the southern edge of an ancient land mass. the oldest exposed rocks are devonian fluvial sediments that were deposited 400million years ago

    香港處于古陸塊的南緣,最老的外露巖石是在4億年前的泥盆紀時期,由河流沖積形成的沉積巖。
  19. From the earliest life some 400 million years ago to hong kong s return to chinese sovereignty in 1997, the hong kong story

    香港歷史博物館的香港故事常設展覽,展現香港四億年前泥盆紀至1997年回歸中國的傳奇。
  20. In this paper, the authors prove the sedimentary environment of every lithostratigraphic unit of devonian, and precisely divide the geomorphic units of petrologic paleogeography of that period, based on the multiple division and detailed study to the petrostratigraphy, biostrtigraphy and sequence stratigraphy of devonian in hubei and its adjacent provinces

    摘要通過對湖北及鄰省泥盆紀巖石地層、生物地層與層序地層進行多重劃分對比和詳細研究,以大量實際資料確定該時期各巖石地層單位的沉積環境,準確劃分出該時期巖相古地理地貌單元。
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