eogene 中文意思是什麼

eogene 解釋
始新世
  1. Analysis of sequence stratigraphy of eogene system in yi - shu graben

    舒地塹下第三系層序地層分析
  2. The basin has dual texture in which it is horst - graben in mesozoic - eogene and " plate " depression in tertiary - quaternary. the basin is the complex basin with wresting and extending dynamic properties, called as torsion - extension basin

    「盆地」具有雙層結構的特徵，下部的中生界及下第三系為壘?塹結構，上部的第三系及第四系為「碟」狀的坳陷結構。
  3. The basin tectonic model : it is intermont basin during late jurassic to early cretaceous, developed into faulted - lacustrine basin in eogene, and evolved into depression in neogene and quaternary

    「盆地」構造發育模式為：從晚侏羅世到白堊紀末期發育的山間「盆地」開始、發展到早第三紀斷陷湖盆的發育、再演化為晚第三紀及第四紀地陷發育階段。
  4. There are nine depressions and forty - four drilled wells in lin qing sag that has an area of 5910 square kilometers and has been explored for more than forty years. only two oil wells were found in the eogene system indicates that petroleum entrapment in this area is complicated

    臨清坳陷經歷四十余年油氣勘探歷程，在約5910km ~ 2面積上有九個窪陷，鉆探了44口，僅有兩口在下第三系見低熟油流，說明該區油氣成藏的復雜性。
  5. In a word, the stress field variation since mesozoic can be divided into five periods such as indosinian epoch, early yanshan epoch ( j3 - k1 ), end of yanshan epoch, eogene, neogene and quaternary, it is mainly affected by the active pattern of tanlu large fault

    綜合研究認為，本區自中生代以來的應力場變化可分為印支期、早燕山期（ j3 - k1 ） 、燕山末期、早第三紀、晚第三紀及第四紀五個階段，應力場的變化主要受郯廬大斷裂活動方式的影響。
  6. The characteristics of compaction curves, the evolution of organic matter, the direction of migration and assignment, conduit system, fluid potential are studied it is concluded that the low maturity of the source of the eogene age is the main factor to control the entrapment. it controls the direction of the primary migration, confines the location of mature source rock and the special carrier rock, controls the time of expulsion and the amount of petroleum, therefore ; the effective traps should be near to oil kitchen and on the pathways of migration

    認為下第三系油灶的低熟是影響其運聚成藏的關鍵因素，生油巖低熟決定油氣初次排烴的方向指向沙三下段；生油巖低熟決定成熟生油巖分佈的局限性和輸導體的特殊性；生油巖低熟決定起排烴時間晚、生烴量不足，從而決定有效的圈閉應是近源的、在運移主路線上。
  7. From late - mesozoic to eogene, northern edge of mesozoic tarim basin became uplift gradually and the sedimentary range migrate to south. present u ' erdusi basin, yanqi basin, kumishi basin became uplift one by one and experienced strong deformation, denudation and reformation and some strata are denuded

    中生代晚期到早第三紀，塔里木中生代盆地北緣逐步隆升，沉積范圍向南遷移，今尤爾都斯、焉耆和庫米什盆地范圍先後隆升，缺失沉積，並造較強烈變形、剝蝕等改造。
  8. The evolution of faulted - basin and development of hydrocarbon source rocks in eogene of the jinxian sag, the jizhong depression

    冀中坳陷晉縣凹陷下第三系斷陷湖盆的演化與烴源巖的形成
  9. Braided stream delta deposit of eogene es102 in haojia - shinan area of dongying depression

    史南地區下第三系沙二10辮狀河三角洲沉積
  10. Even if the same genetic face, the velocity is very different because of different location. for example, the velocity of the vicinity and beyond of estuary bar is respectively 238. 33mm / ka and 0. 89 mm / ka. the paper has also related the deposital velocity of delta with quite deep lake of eogene of jiyang basin and the okinawa trough of quaternary and contemporarily shore

    即使是同一成因相，其所處的位置不同，沉積速率也有較大的差距，如分流河口壩（近端）與分流河口壩（遠端）的沉積速率分別為238 . 33mm / ka和0 . 89mm / ka 。
  11. Sequence stratigraphy models and controlling factors of eogene in raoyang depression

    饒陽凹陷下第三系層序類型及發育模式
  12. Sedimentary characteristics of eogene pinghu formation and huagang formation in chunxiao zone of xihu lake depression

    塔河油田奧陶系碳酸鹽巖儲層特徵
  13. High resolution sequence stratigraphy for the first member of eogene dongying formation in miao 28x1 tract of jidong oilfield

    1區塊東一段高解析度層序地層學研究
  14. The zone related to sha er member is more related to sedimentary velocity. 3. three dynamic systems of entrapment are divided in the eogene of de nan depression in terms of stratigraphic, tectonic characteristic and the vertical distribution of abnormal formation pressure

    3 、從成藏動力學系統的角度可將德南窪陷下第三系劃分為三個成藏動力學系統，即上部、內部和下部成藏動力學系統。
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