palaeozoic 中文意思是什麼

palaeozoic 解釋
adj. 形容詞 【地質學；地理學】古生代的。
n. 名詞 〈the Palaeozoic〉古生代。

  1. Many carbonate masses older than middle palaeozoic are of dolomite rather than calcite.

    中古生代以前的許多碳酸鹽類礦物是白雲石而不是方解石。
  2. The area was wholly uplifted with caledonian orogeny in the early palaeozoic, and underwent thereafter denudation

    早古生代以來，加里東運動使本區全面上升，同時遭受剝蝕。
  3. Zhang hong, wang yongdong, shen guanglong, he zonglian, wang jun. 1999, palaeophytogeography and palaeoclimatic implications of permian gigantopterids on the north china plate. proc. int. conf. pangea & palaeozoic transition. 167 - 168

    沈光隆，張泓，王軍，張雙全， 2000 ，陜西渭北煤田石炭-二疊紀植物地層初步研究，第三屆全國地層會議論文集。 117 - 124 。
  4. 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。
  5. Mrecator might be used by a geologist mapping current directions in palaeozoic sediments.

    地質學家可用麥卡托投影來繪制古生界沉積的水流方向。
  6. Mercator might be used by a geologist mapping current directions in palaeozoic sediment.

    地質學家可用麥卡托投影來繪制古生界沉積中的水流方向。
  7. The karst formation of phong nha - ke bang national park has evolved since the palaeozoic ( some 400 million years ago ) and so is the oldest major karst area in asia

    豐芽格邦國家公園的喀斯特地貌的形成是從古生代（大約40億年前）開始的，是亞洲最古老的喀斯特地貌。
  8. My professor studies flora of the palaeozoic era

    我的教授研究古生代的植物群。
  9. Deep basin gas reservoirs of late palaeozoic in northern ordos basin

    鄂爾多斯盆地北部晚古生代的深盆氣氣藏
  10. Sedimentary - tectonic event and hyhrothermal depositional mineralization in palaeozoic sedimentary basin, south qinling

    構造事件與熱水沉積成礦
  11. Prospects of exploring palaeozoic primary oil and gas pools in southern area of north china cratonic basin

    華北古生代克拉通盆地南部原生油氣藏勘探前景
  12. The target strata in yulin gas field lie in the bottom of shanxi formation of permian, upper palaeozoic

    摘要榆林氣田目的層系位於上古生界二疊系山西組底部。
  13. The study on elements and model of pool - forming in mesozoic and palaeozoic stratum in tongwang area, donying depression

    東營凹陷通王地區中古生界油氣成藏要素及成藏模式研究
  14. There are a series of lead - zinc polymetallic deposits, such as fozichong, dongtao, xiashui, wenlongjing and jilongding distributed along the fault zone. these deposits have some similiar features : ? ll of them are bounded in the strata of lower palaeozoic group ; ? ain orebodies occur as stratiform or stratoid form with occurrence consistent with that of host strata ; ? tratiform skam or baritic rock are the direct country rock of orebodies ; ? ypical syngenetic sedimentary fabric preserved in the ore. these deposits may be included in the same metallogenic series

    佛子沖、東桃、下水、文龍徑、雞籠頂等一系列鉛鋅多金屬礦床沿該斷裂帶分佈，這些礦床雖然在成礦規模、賦礦層位和礦石礦物組成等方面存在一些差異，但均產于下古生界地層中；主要礦體呈層狀、似層狀產出，與地層產狀大體一致；直接賦礦圍巖為層狀綠色巖或重晶石巖；礦石中保留有典型的同生沉積組構。
  15. One of the most important discoveries in this study is the regional exhalative sedimentary mineralization along the bobai - chenxi faulted zone in early palaeozoic, based on which, the metallogenic model of diplogenesis is developed for the fozichong orefield

    博白-岑溪斷裂帶在早古生代為一同生斷裂系統，在拉張環境下沿斷裂帶形成了一地塹型斷陷盆地。
  16. In the last few years, we had obtained plenteous harvests on the exploration of lower palaeozoic burial hills in the regions of zhuangxi and chengdao, jiyang depression. with the enhancing of the exploration degree, it needs more deep research on its reservoirs to adapt to it

    隨著勘探程度的不斷加大，也需要對其潛山儲集層的研究不斷深入與之相適應，本文著重從地球化學的角度對樁西、埕島地區下古生界古潛山儲層的發育機制進行了研究和探討。
  17. This thesis emphasizes to proceed the study on the mechanism of formation of the reservoirs of lower palaeozoic burial hills in the regions of zhuangxi and chengdao from the angle of geochemistry. the research of petrology reveal rock types of the regions mainly include carbonate rock, claystone, siltstone, breccia and a few of evaporite rock

    巖石學研究表明，樁西、埕島地區下古生界古潛山儲層的巖石類型有碳酸鹽巖、粘土巖、碎屑巖、以及少量蒸發巖，其中碳酸鹽巖是該區下古生界古潛山儲層最主要的巖石類型，為一種穩定地臺型海相沉積環境的產物。
  18. Among of them, carbonate rock is the primary type of them, it is the product of stable platform facies of marine. we study the geochemical characteristic of carbonate rock of lower palaeozoic burial hills in the regions of zhuangxi and chengdao and find that the calcite fillings in cave or vein have high value of 87sr / 86sr, low value of 13c and 18o and high mn content among of different structural components. so it has been exposed to be dissolved by meteoric water on supcrgene diagenetic stage

    通過對樁西、埕島地區下古生界碳酸鹽巖的地球化學特徵研究，表明在巖石的各種結構組分中，洞或脈中的方解石充填物具有顯著較高的~ （ 87 ） sr ~ （ 86 ） sr比值，較低的~ （ 13 ） c 、 ~ （ 18 ） o和較高的mn含量，其所經歷的重要巖溶作用是大氣淡水成巖作用，發生的時間為表生成巖階段。
  19. The reservoir is located at yishan slope area between jinxi fold belt and tianhuan depression, it has the characters of less structural deformation, overlying hydrocarbon genetic center in upper and lower palaeozoic era, growth of high efficient reservoirs and as well as fast lateral changes of reservoir physical properties, it has the condition of forming non structural traps, which is the major area for gas reservoir exploration in the basin

    位於晉西撓褶帶和天環坳陷間的伊陜斜坡區，因具有構造變形微弱，上、下古生界生烴中心疊置，高效儲層發育，儲集層物性側向變化快等特點，具備形成非構造圈閉優越條件，為盆地氣藏勘探約重點區帶。
  20. Camp belong to the south qinling orogenic belt middle segment palaeozoic strench basin fold indo - chinese epoch drape north part, and belong to the miliangchuan schiefer

    礦區所在部位屬南秦嶺造山帶中帶古生代伸展盆地疊加印支期沖褶帶的北部，隸屬于米糧川逆沖巖片。
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