陸成層系 的英文怎麼說

中文拼音 [liùchéngcéng]
陸成層系 英文
terrestrial formation
  • : 陸數詞(六的大寫) six (used for the numeral 六 on cheques, etc. to avoid mistakes or alterations)
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  • : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
  • : 系動詞(打結; 扣) tie; fasten; do up; button up
  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,寒武-奧陶紀為其烴源巖形的重要時期;早奧陶世末-晚奧陶世末的構造反轉是塔中隆起的主要形期,同時也為志留及復合圈閉提供了古地理背景;志留?泥盆紀塔里木盆地南北緣均轉為活動大邊緣,形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;二疊紀后構造變動主要以調節為主。
  2. By physiognomy feature, it could be divided into three types of thermal structure : positive dome model, negative collapse model and border dome core collapse model. based on the depth degree or magma - thermal influenced, it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model, superficial volcano eruption hydro - thermalism and hypabyssal intrusive model, thermal anticline ( thermal dome ) model, mid - deep intrusive model, deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure. there are many interaction system could be induced into a systematic thermal interaction, include : ocean - continent system, basin - mountain interaction, superficial and mid - deep crust - mantle interaction, crust - mantle commingle interaction, vertical thermal interaction ( delamination ) etc.

    依據地貌形態分為三類:正向穹窿型、負向塌陷型、邊隆核陷型:依據巖漿-熱力作用影響的深淺程度或深度分為五類: (古)地熱異常群集區、表淺火山噴發-熱液活動與淺侵入型、熱力背斜(熱穹窿) 、中深侵入型、深部地幔(地殼)熱柱型;提出了熱力構造作用空間分佈的理想模式,將洋統、盆山作用、淺表與中深部殼幔作用、殼幔混合、垂向熱力作用(拆沉)等納入一個整體統一的熱力作用統中,為盆地動力學研究打開了一個新窗口;研討了熱力構造研究方法。
  3. This article contains three parts, namely, preface, body and conclusion. the preface mainly introduces the discussing subject and writing purposes of this article. body is divided into four parts : from the beginning of actio in rem and actio in personam in roman law, the first part detailedly inspects and analyses the formation process of the dual rights system in historical research methods ; the second part discusses the theoretical framework of the dual rights structure from the aspect of system ; the third part mainly analyses the middle rights and the integration of real rights and creditor ’ s rights and the reasons for the emergence of these phenomena, pointing out that the emergence of these phenomena is unevitable in civil law system which ajusts social relationship with systematic code, and how

    正文分為四個部分:第一部分採用歷史研究的方法,從羅馬法上的對人之訴和對物之訴出發,對物債二分體的形過程進行了細致的考察和分析;第二部分從體化的角度討論了物債二分體的理論構,對其理論架構進行了總體上的研究;第三部分著重分析了物權與債權的融合和中間狀態及其出現這些現象的原因,指出在運用體化的方法調整社會關的過程中,出現物權和債權中間狀態的權利形態是不可避免的現象,並對如何正確看待這些問題進行了論證;第四部分在前文論述的基礎上,對我國一些學者提出的制定財產法和設立財產法總則的觀點的可行性進行了分析,指出無論是從我國大的傳統還是從技術面來看,制定財產法或設立財產法總則都是不可行的。
  4. Fungi form mycorrhizae in plant roots and the hyphae take in carbon from plants through their epidermal cells and move mineral nutrients and water from soil to their epidermal cells ; this symbiosis is of high importance in studying biodiversity conservation, the origins and evolution of terrestrial plant, the rehabilitation and reconstruction of degenerated ecosystems, agriculture, horticulture and forestry

    真菌在植物根菌根后,菌絲通過根的皮細胞獲取植物提供的碳源,同時將礦物營養和水從土壤轉運到皮細胞,這種共生過程的研究在生物多樣性的保護、生植物的起源與演化、退化生態統的修復與重建以及農業、林業和園藝業的應用具有重要的意義。
  5. According to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field, including lithology, size distribution, sedimenta ry structure, geochemistry and paleontology etc., the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt. it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal. the peat flat is the important paleoenviron ment for coal accumulation. the tidal channel destroys the coal bed. the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation

    根據肥城煤田石炭太原組的巖性、粒度分佈、沉積構造、地球化學及古生物等沉積特徵,將該區晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環境,認為太原組形於潮汐作用為主的表海海岸,泥炭坪是煤的重要古地理環境,潮渠對煤有一定的破壞作用,地殼的脈動性振蕩作用是控制沉積環境演化和聚煤作用的主要因素。
  6. Abstract : according to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field, including lithology, size distribution, sedimenta ry structure, geochemistry and paleontology etc., the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt. it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal. the peat flat is the important paleoenviron ment for coal accumulation. the tidal channel destroys the coal bed. the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation

    文摘:根據肥城煤田石炭太原組的巖性、粒度分佈、沉積構造、地球化學及古生物等沉積特徵,將該區晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環境,認為太原組形於潮汐作用為主的表海海岸,泥炭坪是煤的重要古地理環境,潮渠對煤有一定的破壞作用,地殼的脈動性振蕩作用是控制沉積環境演化和聚煤作用的主要因素。
  7. The yanchang formation is divided, for the first time, into six third - order sequences, each with an average time duration of about 4. 5 ma. the single sequence is composed of deltaic and lacustrine sandstones, siltstones and mudstones. the subaerial and subaqueous distributary channel and channel - mouth bar sandstone reservoirs are well developed mainly in the lowstand and highland systems tracts

    論文在富縣探區首次應用序地學的觀點和方法,把延長組劃分為6個三級序,平均時限4 . 5ma ,各序由三角洲與湖泊相砂、泥巖沉積組,主要在低位體域和高位體域發育水下(上)分流河道和河口砂壩砂巖儲
  8. This article attempts to analyze the processing mechanism of the pure economic loss which comes to being in the system of civil law and anglo - america law system, summarizes characteristics of the processing mechanism and the policy consideration factor behind these processing mechanism, then carries on the discussion of the construction and the consummation of processing mechanism of the pure economic loss of our country, hopes to give my pygmy effort into the theory and the system of the pure economic loss in the our country

    本文擬從純粹經濟損失賠償制度的立法選擇入手,分析大、英美法各國基於各自法律傳統與法律體所形的各具特色的純粹經濟損失賠償制度,考察其立法選擇背後更深次的政策考量,分析對我國純粹經濟損失賠償制度立法選擇的借鑒意義。
  9. Namely, the scholars in continental law system countries hold the two levels of causality : that is, causality at the level of establishment of tort liability and the level of scope of tort liability. regarding the liabilities determine, determine at the tow levels is adopted as well. because of the unique jury system, the liabilities determine in the anglo - american law system countries consists of two, namely, the determine of causality in terms of causation in fact and that of causation in iaw the dichotomy of causality in the law of tort not only specifies the tort liability but also limits the scope of the liability

    因果關是侵權行為責任立的必備要件,國外因果關理論的「二分法」 ,即大國家學者將因果關分為責任立上的因果關和責任范圍上的因果關兩個次結構,在責任認定上也採用了責任立的因果關的認定和責任范圍的因果關的認定;英美法根據其特有的陪審員制度,在因果關的認定上分事實上因果關的認定和法律上因果關的認定。
  10. The shallow thermocline distributes in the areas of guangdong, guangxi, fujian and vietnam continental shelf, with obviously seasonal variabilily, and at the same time, in the south and middle areas of nanhai, even in winter when there is no thermocline in the coastal area, there also exists the shallow thermocline

    後者廣東、廣西、福建沿海架區則與黃、東海相同,表現為季節性溫躍,有長、強盛、消衰、無躍的年周期變化過程。南海深溫度躍基本屬於水團疊置型,躍分佈范圍及躍強度、上界深度、厚度與氣候關不大。
  11. Conclusion are obtained as follows : 1. basin accepted sedimentation since sinian, and strata were well developed. it was marine sedimentary series from sinian to middle - triassic and become continental sedimentary series since late - triassic

    主要果及認識如下: 1 、盆地自震旦紀以來長期接受沉積,地發育良好,震旦紀至中三疊世為海相沉積體,晚三疊世以後為相沉積體
  12. The availability of modis data, which main goals are to monitor global environment change, gives us a new opportunity for acquirement of the terrestrial parameters and will conduct global change research

    地表和海洋生態統的遙感信息獲取是全球環境變化研究的關鍵組部分,其定量化的研究越來越依賴于長期連續觀測資料的積累與處理分析。
  13. The pre - jurassic basement of hefei basin was composed of thrusts. indosinian foreland thrusts in pre - jurassic bedrocks of the basin increase towards the tan - lu fault zone, indicating indosinian activity of the fault zone

    合肥盆地在印支期的前侏羅紀基底主要表現為大別造山帶前逆沖推覆構造,由一列逆沖斷和逆沖巖片所組
  14. Analysis of petroleum geology, reservoir types and distribution in lujiapu depression indicates that : the forming and distribution of reservoirs had been controlled by source area, source - reservoir relationship, petrophysical characteristics, sedimentary facies and secondary structure, and oil is most abundant in reservoirs around hydrocarbon kitchen ; the upper member of jiufutang formation which was entrained or embedded in the main oil source layer has well developed reservoir and good petrophysical property and is the principle oil - bearing interval ; the mid - fan and fan delta front of nearshore submarine fan is the most favorite facies ; the steep slope of the depression mainly consists of structural reservoirs, the slope belt mainly consists of structural - lithologic and updip pinchout reservoirs, the depressed belt mainly consists of lenticular lithologic reservoirs

    摘要對家堡凹陷油藏形的石油地質條件、已知油藏類型及分佈的分析認為:生油區、生儲配置關、儲集物性、沉積相帶和二級構造帶控制了油藏的形和展布,其中圍繞生油窪陷的油藏含油最豐富;夾持或嵌入主要生油中,儲發育、儲集物性又相對較好的九佛堂組上段是主要含油段;近岸水下扇的扇中和扇三角洲前緣是最有利的相帶:凹陷的陡坡帶以構造油藏為主,斜坡帶以構造巖性及儲上傾尖滅油藏為主,深陷帶主要為透鏡狀巖性油藏。
  15. This is of very important significance to understand the material property and geodynamic of corresponding area, the surface wave attenuation mechanism and the inversion algorithm of attenuation and s - wave quality factor are discussed systemically in this paper. some important fruits and understanding are resulted from the the crust and upper mantle tomography of china. ( 1 ) calculating of the rayleigh surface wave attenuation factor y

    本文首先探討了面波衰減的機理,對面波衰減和s波品質因子q _反演的計算方法進行了統的研究,並對中國大地區地殼上地幔q _三維結構進行像,取得了以下重要果: ( 1 ) rayleigh面波衰減數計算。
  16. This article is based on the comprative study of the system on legal education and the forming of legal profession community in major legal system, from the present conditions such as the weak foundation of legal education and the diversity of back ground knowledge > custom of thinku ^ institution of permitting persuing this profession and so on, in order to form the community of legal profession in china, i raise my suggestion as follows : first, we must establish the conception of forming legal profession community, foster the lofty feeling on persuing this profession and the significance feeling on persuing this mission among the community members ; second, we must reform the train model of legal education, just as promoting the stratification of legal education, standerdizing the type of legal education, scientific planning the train scheme ; third, optimizing the content of legal education, attaching importanca to the theory of law, cultivating the conception of legality and the humanities quality and the professional ethics ; forth, recommending the teaching method, on the one hand, we enrich the traditional lecture method, on the other hand, we tolerant the case method ; finally, we must continuously carry out the way of boding the unified judical examination, at the same time, i put forward some suggestions on improving the unified - examination institution

    本文在對大和英美法主要國家的法律教育和法律職業共同體養制度進行比較研究的基礎上,針對我國法律教育基礎薄弱、法律職業員內部在知識背景、思維習慣及準入制度等方面參差不齊的現狀,從在目前中國社會培養法律職業共同體這一根本目標出發,提出在我國養法律職業共同體必需在教育觀念上樹立培養共同體的意識,培養共同體員的職業崇高敢感和歷史使命感;在培養模式上規范法律教育的類型、提升法律教育的次、科學設計人才培養方案;在教學內容上,必須致力於培養學生優化的綜合素質,包括理論素質、法治素質、人文素質、職業道德素質等方面;在教學方法上,提倡在傳統的講授法的基礎上豐富和嫁接案例教學法;在法律職業的準入制度上,應繼續推行統一的司法考試制度,並對這一制度提出了大膽的重構設想,以期對構建法律職業共同體的養制度具有一些借鑒意義。
  17. The paper put forward the particular mode of sequence stratigraphy in the foreland basin, which includes lacustrine margin alluvial systems tract ( ast ), lacustrine expanding systems tract ( ltst ), and lacustrine highstand systems tract ( lhst ). the upper triassic can be divided into three marine and one nonmarine sequences

    2 、提出了川西前盆地的序地模式,認為川西前盆地一個完整的序是由湖盆邊緣沖積體域、湖侵體域和湖泊高水位體域三部分構
  18. Begining with analysis of sequence stratigraphy of stratum ore hosted, this paper analysed structure of basin, variation of sea level and terrigenous sedimentation input rate which impacted on seafloor hydrothermal sedimentary mineralization, then through the study of characteristics of hydrothermal sedimentary rocks, ore deposit geochemisty and geology, metallogenic series are established

    序地分析著手,分析熱水沉積礦時的沉積環境、海平面變化及源沉積輸入對熱水沉積礦的影響,研究熱水沉積巖的地質特徵和地球化學特徵、礦床地質特徵對比、礦床地球化學、礦物理化學條件等,最終建立了該區的列。
  19. The newly constituted department expects to be working even more closely with charities such as the hear talk foundation, a group of dedicated professionals comprising ent specialists, audiologists, speech therapists and educators with a heart for improving the quality of life of underprivileged children and elderly people in hong kong and mainland china who have hearing and speech communication disorders

    而在更廣闊的面上,新學會更緊密地和其他慈善機構合作,例如耳聽心言基金一個包括耳鼻喉專科醫生、聽力學家、言語治療師及教育工作者所組的非牟利組織,旨在提升在香港和中國大貧困地區有聽障及言語溝通障礙人士的生活質素。
  20. These nne and ne faults become a long transform fault system and formed a boundary between the eastern margin of china continental plate and philippine sea plate

    這些北北東向和北東向斷一條巨長的轉換斷列,也是中國大板塊東緣與菲律賓洋塊的一條邊界。
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