paleogene 中文意思是什麼

paleogene 解釋
古近紀
  1. Extreme climates events in the cretaceous and paleogene

    白堊紀至早第三紀的極端氣候事件
  2. It is believed that three northeast - striking dextral slip fault zones, i. e. the baxian - shulu - handan fault zone, the huanghua - dezhou - dongming fault zone, and the linyi - huanghekou fault zone, are the result of the tectonic transform of paleogene extending to neogene - quaternary laterally slipping of north china plain rift systems, which extend along the central axis of rifts and accord with the quaternary centers of subsidence as the main seismic structures within the rifts

    認為壩縣束鹿邯鄲斷裂帶、唐山河間磁縣斷裂帶和黃驊德州東明斷裂帶3條北東向右旋走滑斷裂帶為華北平原裂谷系從早第三紀伸展拉張作用進入晚第三紀第四紀走滑剪切拉張作用的產物，這3條斷裂帶分別位於3個北東向坳陷帶中部，並構成了第四紀沉降中心，與營口濰坊斷裂帶起構成華北平原內的主要強震構造。
  3. Synthetic model of sedimentation, diagenesis and pool formation of paleogene for dongying sag

    成巖和油氣成藏綜合模式
  4. Paleogene extensional fault - bend folding in north depression of southern yellow sea basin

    南黃海盆地北部凹陷古近紀伸展斷層轉折褶皺作用
  5. Paleogene - neogene lithologic reservoir prediction in the western slope of damintun depression

    大民屯凹陷西斜坡古近系巖性油藏預測技術與應用
  6. Sedimentary characteristics of oil shale deposit of the huadian formation of paleogene in huadian basin

    樺甸盆地古近系樺甸組油頁巖礦床沉積特徵
  7. The upper cretaceous and paleogene are of continental sediments in henan province, and the boundary between them considered to be unconformable or disconformable because of the very difference in sedimentation and biological assemblages

    摘要河南省上白堊統與古近系均為陸相沉積，在全省范圍內，兩者間呈假整合或不整合接觸，在沉積特徵上顯示出較大的差異，在古生物群的演化方面，也各自具有不同的特色。
  8. The question whether transgression happened in paleogene of bohai bay basin has been discussed for more than 20 years, yet it was not resolved

    摘要有關渤海灣盆地古近紀是否發生過海侵的問題爭論了二十多年，至今尚無定論。
  9. Sr isotope ' s analysis of the paleogene of dongpu depression

    東濮凹陷下第三紀鍶同位素地球化學分析
  10. The fossil birds of the early cenozoic ( paleogene - neogene ) are clearly attributable to the modern birds, and the earliest well - estabished record of most traditional orders and families of modern birds occur then

    新生代早期（包括古近紀和新近紀）鳥類的分類已被清晰地歸入到現生鳥類中，並且現生鳥類傳統的「目」 「科」類型在早期已經出現並確立。
  11. Shifting of lake shoreline and lithofacies palaeogeographic characters during sedimentary period of the member 3 of shahejie formation of paleogene in dongpu sag

    東濮凹陷古近系沙河街組沙三段沉積期湖岸線的變化及巖相古地理特徵
  12. The structure evolution o f cenozoic experienced rifting subsidence of paleogene and rifting thermal subsidence of neogere and quartenary

    新生代構造演化經歷了老第三紀裂陷沉降和新第三紀至第四紀後期裂陷熱沉降階段。
  13. The reverse structure appears in three styles. they are regional structure reverse occurred as angle unconformity between paleogene and neogene, thrush fault and local reverse structures

    反轉構造以三種形式出現，即上下第三系之間角度不整合的區域性構造反轉，逆沖斷層，局部構造的反轉。
  14. Sequence stratigraphy and subtle hydrocarbon reservoir of paleogene in chezhen sag, bohai bay basin

    渤海灣盆地車鎮凹陷古近系層序地層與隱蔽油氣藏
  15. Types of the paleogene slope - break zones and distribution of the subtle traps in gaoliu area of nanpu sag

    南堡凹陷高柳地區古近系坡折帶類型及隱蔽圈閉分佈特徵
  16. The extensional activities of hefei basin occurred in the period between late cretaceous and paleogene. as a result, the extensional normal faults were took place along the pre - existing nearly ew faults and the tan - lu fault zone. the deposition of half - graben was formed

    合肥盆地的伸展活動發生於晚白堊世至早第三紀，伸展活動是疊加在前兩期走滑構造之上，形成了以半地塹式楔形為主的沉積。
  17. The structural active period was between jurassic with cretaceous, and stopped in the early paleogene

    構造活動期在侏羅紀?白堊紀，第三紀初期構造活動基本停止。
  18. Sedimentary facies types of the third member of the shahejie formation in the paleogene of the dongying depression, the bohaiwan basin and their distribution characters on plane

    渤海灣盆地東營凹陷古近系沙河街組三段沉積相類型及平面分佈特徵
  19. Under the guidance of new principles and methods of modern sedimentology, detrital petrography, reservoir geology, diagenesis, this thesis has carried out detailed study on paleogene formation correlation, sedimentary environment, characteristics of sedimentary facies and diagenesis of the eastern kuche depression, tarim basin, dina area being taken as the main target of the study. based on the core, geology logging, log and seismic data from 9 typical wells, combined with the data of the adjoining area, the dominant sedimentary types of the study area have been recognized and illustrated, such as fan - delta, lacus and normal delta. in terms of the analysis on the sedimentary facies of typical and connecting wells in different areas and facies belt, together with the paleogene tectonic evolution characteristics of foreland basin, the distribution and evolution of the sedimentary facies of the study area have been clearly discovered both vertically and laterally

    通過對該區9口井的巖芯、錄井、測井、地震資料及鄰區資料的分析，識別並闡述了庫車坳陷東部下第三系的幾種主要的沉積相類型，如扇三角洲相、湖泊相和正常三角洲相；通過對不同地區、不同相帶典型井及連井的沉積相分析，結合前陸盆地在下第三系的構造演化特點，弄清了迪那地區下第三系沉積相的縱橫相發育展布和演化規律，並建立了沉積相模式；同時，初步開展了成巖作用、儲層孔隙演化和儲層發育模式的研究工作，科學合理地解釋了現今迪那地區下第三系儲產層主要發育在粉砂巖中的特殊現象，首次建立了下第三系儲層的發育演化模式，為庫車坳陷東部地區進一步尋找下第三系大儲量、高產油氣藏和有利的勘探區塊提供科學的、可靠的和最直接的地質依據。
  20. Based on the analysis of distribution of upper jurassic and lower cretaceous strata and basin - controlled faults, tanlu fault zone strike slip to develop the three nw - trending grabens from north to south western to tanlu fault zone in late jurassic and early cretaceous, which are bohai graben, jiyang graben and luxinan graben. based on the analysis of regional geology, the basic tectonic pattern of bohai basin is the cenozoic basin pattern since early paleogene. the outline, structure, deposit characteristics and heat flow distributions show that the basin is pull - apart basin in cenozoic time. the tectonic evolution pattern can be reconstructed based on the analysis of cenozoic strata, deposit thickness, location and activity of basin - controlled faults in the different depresses in bohai basin. the characteristics of structure and depositment in this mesozoic and cenozoic time show that bohai basin is a mesozoic and cenozoic composite basin

    根據中生界上侏羅統和下白堊統地層和控盆斷裂分佈分析，中生代晚期晚侏羅早白堊世郯廬斷裂帶的左旋走滑平移導致郯廬斷裂帶以西自北向南發育了3個北西向斷塹系，即北部的渤海斷塹系中部的濟陽斷塹系和南部的魯西南斷塹系。從區域資料綜合分析，渤海灣盆地的基本格局是早第三紀以來的新生代盆地格局。渤海灣盆地的形態構造和沉積特徵及熱流值分佈表明該盆地在新生代為拉分盆地。
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