ordovician 中文意思是什麼

ordovician 解釋
n. 名詞 【地質學；地理學】奧陶紀；奧陶系；〈the O-〉奧陶時期；奧陶紀層。
adj. 形容詞 【地質學；地理學】奧陶紀[系]的。

  1. It agrees with the fact that the gabbro is intruded by late ordovician granitic pluton. the pre - sinian basement strata exposed in the north kunlun massif are later archean - neoproterozoic milan group, changcheng system kaqiang group, jixian system liushui formation and qingbaikou system sulu formation

    被蛇綠巖所分隔的昆北地塊上出露的前震旦紀基底地層為：晚太古代-新元古代米蘭巖群，長城系卡羌巖群，薊縣系流水巖組和青白口系絲路巖組。
  2. 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-奧陶紀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?泥盆紀塔里木盆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；二疊紀后構造變動主要以調節為主。
  3. The development of an atypical hirnantia - brachiopod fauna and the onset of glaciation in the late ordovician of gondwana / owen e. sutcliffe. . [ et al. ]

    岡瓦納古陸晚奧陶統一個典型的赫南特貝屬-腕足動物群的發育和冰川作用的開始
  4. From the late middle ordovician to the end of ordovician, the cephalopods, gastropods and corals in the erlangping trough, and the conodonts, coral, brachiopods, cephalopods as well as trilobites in the xichuan shelf were from the north china province

    在中奧陶世晚期至奧陶紀末，二郎坪海槽的腹足類、頭足類和珊瑚與浙川陸棚的牙形石、珊瑚、腕足類、頭足類和三葉蟲均屬華北生物省。
  5. From the cambrian to the early middle ordovician, the cambrian radiolaria and the early ordovician conodonts of the erlangping trough in the northern part of eqm, and the cambrian trilobites and early ordovician conodonts as well as cephalopods of the northern xichuan shelf in the southern part of eqm belonged to the south china province, while the cambrian trilobites and the early ordovician conodonts of the southern xichuan shelf belonged to the south china province with some elements of the north china province

    在寒武紀至中奧陶世早期，東秦嶺北部二郎坪海槽的寒武紀放射蟲和早奧陶世牙形石與東秦嶺南部浙川陸棚北部的寒武紀三葉蟲、早奧陶世牙形石和頭足類屬華南生物省，而浙川陸棚南部的寒武紀三葉蟲和早奧陶世牙形石屬于華南生物省，兼有華北生物省分子。
  6. 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盆地重大疑難地層問題：晚奧陶世志留紀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晚泥盆世弗拉斯期。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。
  7. The origin and evolution of land plants was an important event in the history of earth life and has affected all other lives on the earth and global environment. during the past two decade, the new discoveries of fossil plants microfossils and megafossils from the mid - ordovician through all silurian to the lower devonian improved knowledge of the origin of land plants, provided a time framework of the basal groups for the land plants and the early evolution diversity of vascular plants. three new plant based epochs have been recognized. on the other hand, molecular sequence studies have provided insights into the phylogeny and early branches of land plants. a phylogenetic tree has been established by the joint of a study of comparative morphology and gene sequences. this paper summarizes recent advances and new knowledges, comments on the phylogenetic studies based on the cladistic analysis

    陸生植物的起源和演化是地球生命中的重大事件，它影響到地球上所有的其他生命和全球環境。在過去的20年中，從中奧陶世歷經整個志留紀至早泥盆世的巖層中，化石植物微化石和大化石的新發現改變了人們對陸生植物起源的認識，並且為陸生植物和維管植物早期演化分異提供了基部類群分化的時間框架。據此人們識別出地史中的3個陸生植物的時代：始胚植物時代始維管植物時代和真維管植物時代。
  8. Diagenesis and pore evolution of ordovician carbonate reservoirs in qianmiqiao buried hill

    以千米橋潛山凝析氣藏為例
  9. Laiwu hydrothermal metasomatic iron deposit is located at contact zone of ordovician carbon - ate rock ( majiagou formation ) and late yanshanian diorite or nearby

    摘要萊蕪接觸交代熱液鐵礦賦存於奧陶系馬家溝組碳酸鹽巖與燕山晚期閃長巖的接觸帶及其附近。
  10. The filling evolutionary process in the palaeozoic era in this area was extremely complex. during the majiagou stage of early ordovician period, the researched area went through three tertiary eustatic cycles. with negative movement in ma ; stage, deposits of evaporate platform and local platform were developed

    古生代研究區經歷了十分復雜的充填演化過程，早奧陶世馬家溝期本區經歷了三個三級海平面升降旋迴，其中馬5期隨著海平面下降，發育了蒸發臺地和局限臺地沉積。
  11. Three diagenesis types are help to differentiate the middle caledonian and early hercynian karst, which are stylolite, dolomitization and dedolomitization. 2 ) karst identification symbols and karst reservoir of ordovician in bores, logging, well logging and fmi have been established. karst reservoir have been identified and evaluated in the tahe oilfield

    2 ）建立了奧陶系巖溶在巖芯、錄井、常規測井和成像測井上的識別標志，以及巖溶型儲層在以上方面的識別標志，並對研究區內巖溶型儲層進行了識別和評價。
  12. We have concluded that the structural movement of the area can be divided into three stages : the stretching stage from simian to early ordovician, the extrusion and rising stage from middle and late ordovician to jurassic and stable depressed stage of foreland basin slope from cretaceous to neozoic

    經研究認為研究區的構造運動，主要分為震旦紀到早奧陶世的拉張階段、中晚奧陶世到侏羅紀的擠壓隆升剝蝕階段以及白堊紀到新生代的前陸盆地斜坡穩定沉降階段。
  13. Research on comprehensive treatment of mine ordovician water

    深部礦井奧灰水綜合治理技術
  14. Marine volcanics of early ordovician was found in zhifang region

    摘要紙房地區具有早奧陶世海相火山巖存在。
  15. Characteristics of ordovician carbonate rock reservoirs in tahe oilfield

    高陞油田高81塊儲層特徵與含油氣潛能
  16. Log interpretation of ordovician carbonate reservoirs in tahe oilfield

    塔河油田奧陶系碳酸鹽巖儲層的測井解釋
  17. O3h upper ordovician hongjiawu formation of the zhejiang - jiangxi border region

    浙贛交界地區上奧陶統紅家塢組
  18. This was the result from the large - scale regression in the late ordovician

    這是晚奧陶世晚期大規模海退的結果。
  19. During the ordovician, 505 million years ago, the first plants appeared

    在ordovician期間， 505百萬年前，第一植物出現。
  20. Harness technology for karst water in ordovician limestone with underground grouting of hole

    井下鉆孔注漿治理奧灰水技術
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