古巖溶 的英文怎麼說

中文拼音 [gǔyánróng]
古巖溶 英文
palaeokarst
  • 古 : Ⅰ名詞1 （古代） antiquity; ancientry 2 （先哲的遺典、道統） books or orthodoxies of ancient sages...
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 溶 : 動詞（溶化; 溶解） dissolve
  1. However, the authors discovered recently that the top and bottom surfaces of the loushanguan formation are palaeokarst unconformity interfaces, and there are a lot of interbeds of granular ( oolite, pisolite and oncolite ) dolomite and algae - mat dolomite, especially sedimentary structures such as the bird ? s eye, stromatolite, cross bedding and tepee structures

    但筆者新近研究發現，其頂、底均為古巖溶不整合面，並有大量顆粒（鮞、豆、核形石）白雲巖和藻紋層白雲巖夾層，還有許多鳥眼構造、疊層石構造、交錯層理、帳蓬構造存在。
  2. We conclude the reservoir is of complex pore - cave - fracture type. 5. the karst reservoir is studied by paleography, leaching time, hydrological regime, lithofaces - paleography, combined with outcrops and drilling data, the karst reservoir model is established

    8 、本區巖溶儲層的空間分佈呈帶狀，非均質性強，並受水動力帶、巖性、沉積相、構造、風化剝蝕持續時間和古地形的影響。
  3. 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。
  4. Gpr is a newly developed hi - tech survey technique used to detect shallow ground electric differences. we applied gpr to more than 100 projects in zhujiang river delta and hongkong, and obtained good reputations. the application scope involves stratigraphics division, outining of filled stones in the muddly beach, geotechnical prospecting of old wall, karst detecting in the limestone terrain, caving detecting, landslide and slop surveing, the division of wea - thering zone, onion weathering zone, fracture zone and fau - lted zone in the granite area, detecting of buried objects cable, metal nonmetal pipe, channel, air raid she - lter etc. underground in the urban city, archaeology, tracing of orebody, coal measures strata division, testing of the dam and grouting site, quality checking of the surface and foundation of the highway

    的一種高新技術。我公司運用世界最先進的探地雷達設備在珠江三角洲地區和香港開展了百余項探地雷達檢測項目，獲得了良好的聲譽，並被作為深圳市建設局1998年度建設科技成果推廣項目。它主要應用於：山體土石方檢測路基不同回填物界面檢測填海回填物巖溶檢測樁基無損檢測地下管道探測地下隱蔽物探測考古斜坡滑體探測地質結構探測湖底探測高速公路路面及路基檢測。
  5. It is indicated that the karsts denudation surface in the mount lu and that of southern shandong province are the same denudation surface. based on the relation between the level of cave and denudation surface, the hilltop on the north of mount tai is also the denudation surface formed in the same period

    在前第四紀地貌面研究中，根據萊蕪平州頂上發現的白彥礫巖，確認以平州頂?仰天槽為代表的仰平期（中新世至上新世）巖溶剝夷面與魯南地區白彥礫巖代表的古地面屬同一期古剝夷面。
  6. The formation of carbonate reservior is controlled by the overlaid c - p strata and the intensity of karstification which was related to the palaeo geomorphy and palaeodrainage system

    下古生界碳酸鹽巖裂縫溶蝕型儲集層的發育特徵以有無上古覆蓋是巖溶發育的前提；古地貌、古水系控制巖溶發育強度。
  7. The lay - like karst aquifer formed by some special strata and fossil karst are very important in the groundwater exploitation in this area

    特殊巖性和古溶蝕形成的似層狀巖溶含水層具有重要的開發價值。
  8. Paleokarst cave features of the western fringe of e ' erduosi basin

    鄂爾多斯盆地西緣古巖溶洞穴特徵
  9. The occurrence of the palaeokarstification is closely associated with the sequence boundaries and lowstand systems tract created by the guizhou - guangxi, ziyun and dongwu movements

    古巖溶作用的發生與黔桂運動、紫雲運動、東吳運動等所形成的層序界面和低位體系域密切。
  10. The paper takes an example of condensed gas feild in qianmiqiao buried - hills. based on the research of formation and development of the buried - hills, three important subjects in the research are discussed with the application of advanced technical and methods ( namely, balanced cross sections, analysis of carbon isotope, mensuration of reservoir fluid inclusion ) : ( 1 ) the development of karstification and characters of reservoir in ordovician ; ( 2 ) lower tertiary ( es3 ) source in the depression nearby ; ( 3 ) the hydrocarbon generation history, migration phase and reservoir formation history

    論文以千米橋潛山凝析氣藏為例，在研究潛山形成演化基礎上，採用先進技術手段（平衡剖面技術、碳同位素分析、儲層流體包裹體測定） ，討論了該潛山油氣藏研究中三個重要問題： （ 1 ）古巖溶發育與奧陶系儲層特徵； （ 2 ）臨近凹陷下第三系油氣源： （ 3 ）油氣生成史與運移期次以及成藏歷史。
  11. It was considered that karstification is the base of reservior formation, and lithology and faulting control the formation and development of internal reservior

    其發育規律為：巖溶作用是下古生界儲集層發育的基礎；巖性和斷裂作用決定內幕儲層的形成與發育。
  12. In this research, some conclusions are followed : l ) in the tahe oilfield, multiphase tectonic movement and pleokarst were so deeply worked on the diagenesis that the types of diagenesis are various, and the relation of those are complicated

    本次研究最終得出如下結論： 1 ）研究區由於受到多期構造運動的影響，又受到多期古巖溶作用的疊加改造，成巖作用類型多樣，關系復雜。
  13. One to three karst cycles may be recognized mostly at the top of the upper permian strata, top of the middle permian maokouan strata and top of the carboniferous strata and subordinately at the top of the devonian strata

    這些古巖溶作用主要存在於上二疊統頂部、中二疊統茅口組頂部和石炭系頂部，其次是泥盆系的頂部。
  14. The genetic types include weathering, regional meteoric corrosion, regional dolomitization regional paleokarstification, regional dedolomitization and regional fresh - water cementation and filling

    研究區存在包括風化、區域性大氣淡水溶蝕、區域性白雲巖化、區域性古巖溶、區域性去白雲巖化和區域性淡水膠結充填等6種巖溶作用的層序成因類型。
  15. This paper summarizes seven kinds of geological factors advantageous for karstification, such as the lithology, the strata framework, the geological strature, the paleo - relief, the paleo - climate, the former pore space system and the later reconstruction in embedding period

    摘要分析了巖溶發育的7種地質因素，即巖性、地層結構、地質構造、佔地貌、古氣候、先存孔洞系統以及埋藏期的後期改造等。
  16. Abstract : according to observation and study, the paleokarstifications of ordovician could be classified into 6 periods, i. e. depositional karstification, weathering curst karstification, burial karstification, semi - burial structural karstification, second burial karstification stage, its karstic types have mainly deposition karst, emergence karst, burial karst, wqueezing - water and structural karst or hot - water karst, and its karst - rocks can be distributed to two kinds of types, i. e. karst - sedimentary rock and karst - regenerated rock, and further to 8 subcategories and 5 sub - sub - categories in the north of anhui, china

    文摘:研究表明，皖北奧陶系古巖溶可劃分為沉積巖溶作用期、風化殼巖溶作用期、埋藏巖溶作用期、構造巖溶作用期和二次埋藏巖溶作用期；其巖溶類型主要有沉積巖溶、風化殼巖溶、埋藏巖溶或壓釋水巖溶和構造巖溶或熱水巖溶四種類型；其巖溶巖包括巖溶沉積巖和巖溶改造巖兩個大類，並可進一步劃分出8個亞類和5個子亞類。
  17. According to observation and study, the paleokarstifications of ordovician could be classified into 6 periods, i. e. depositional karstification, weathering curst karstification, burial karstification, semi - burial structural karstification, second burial karstification stage, its karstic types have mainly deposition karst, emergence karst, burial karst, wqueezing - water and structural karst or hot - water karst, and its karst - rocks can be distributed to two kinds of types, i. e. karst - sedimentary rock and karst - regenerated rock, and further to 8 subcategories and 5 sub - sub - categories in the north of anhui, china

    研究表明，皖北奧陶系古巖溶可劃分為沉積巖溶作用期、風化殼巖溶作用期、埋藏巖溶作用期、構造巖溶作用期和二次埋藏巖溶作用期；其巖溶類型主要有沉積巖溶、風化殼巖溶、埋藏巖溶或壓釋水巖溶和構造巖溶或熱水巖溶四種類型；其巖溶巖包括巖溶沉積巖和巖溶改造巖兩個大類，並可進一步劃分出8個亞類和5個子亞類。
  18. As to human scenery, there are many overhanging coffins and inscriptions on escarpments in danxia and karst landform areas, in addition, there are also many famous mountains of taoism and grottoes of buddhism in danxia landform areas, and many paleoanthropological sites and charming landscapes of national culture in karst landform areas

    人文景觀方面，丹霞地貌區與巖溶地貌區均遺存眾多懸棺崖墓和摩巖題刻；此外，前者還以道教名山和佛教石窟眾多而見長，後者則在古人類遺址和民族風情方面占據優勢。
  19. The carbonate reservoir rock includes many influence factors that it is through many phases structure bursts and the ancient karst to act on jointly the formation and with which the rock karst gives first place. the complicated oil field of karst cave and crack are controlled by limestone reservoir and the crevices - cave system, which have many characteristics such as vivid and great in style, irregular distribution, the limestone cave in crack and unhomogeneity of rock etc. these kinds of reservoir belong to a world difficult and extreme problem on valuation and cognition

    它是經多期構造破裂與古風化巖溶共同作用形成的、以灰巖巖溶為主控因素、以儲集體控藏和縫洞系統控藏為主的溶洞?裂縫型復雜油氣藏，表現為其不規則形態和不均勻分佈、裂縫溶洞發育不均一、儲層非均質性極強等特點，認識和評價該類儲層屬世界性難題。
  20. The analysis results of hydrocarbon generating history, paleotemperature history, the homogenization temperature distribution of fluid inclusions and individual fluid inclusion compounds show that the natural gas charging times in the center gas field is two. the first is at the age of late triassic. at that time, natural gas migrated from the east to the west and from the south to the north

    根據鄂爾多斯盆地中部的沉積史、構造發育史、古巖溶形成史、生排烴史等等，按其時空配置關系，歸納氣藏的形成可分為四個演化階段：儲集層孕育階段（ 0 ； c ； ） 、圈閉形成階段（ c 。
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