secondary depression 中文意思是什麼
secondary depression
解釋
副低氣壓- secondary : adj 1 第二（位）的，第二次的；中級的 （opp primary）。2 副（的）；從屬的；附屬的；輔助的；補充的...
- depression : n 1 壓低，降低，陷落。2 凹窪；窪地，沉降地。3 不景氣，蕭條，不振。 4 沮喪，消沉。 5 低氣壓。6 【...
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Chagan sag is a secondary tectonic unit in chagandelesu depression, northeastern yingen - eji ' naqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate, with the character of erogenic belt. in working area and its adjacent area, the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase
查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元，其盆地基底為古生代時期華北板塊、哈薩克斯坦板塊和塔里木板塊交接部位形成的陸緣或島弧褶皺帶，具有古生代造山帶的性質。研究區及鄰區印支期侵入巖形成於造山帶強烈擠壓陸內俯沖的構造環境；燕山早期侵入巖形成於由擠壓轉向拉伸、造山帶的增厚陸殼開始發生伸展垮塌的構造環境；早白堊世火山巖形成於造山期后進一步發生伸展垮塌的區域構造環境。 -
Chagan fault depression is a secondary tectonic unit in chagandelesu subbasin, northeastern yingen - ejinaqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc with the character of erogenic belt at the connection region of north china plate, tarim plate and kazakstan plate
查干德勒蘇凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元。其基底為古生代時期華北板塊、塔里木板塊和哈薩克斯坦板塊交接部位的陸緣或島弧褶皺帶，具有古生代造山帶的性質。 -
Analysis of petroleum geology, reservoir types and distribution in lujiapu depression indicates that : the forming and distribution of reservoirs had been controlled by source area, source - reservoir relationship, petrophysical characteristics, sedimentary facies and secondary structure, and oil is most abundant in reservoirs around hydrocarbon kitchen ; the upper member of jiufutang formation which was entrained or embedded in the main oil source layer has well developed reservoir and good petrophysical property and is the principle oil - bearing interval ; the mid - fan and fan delta front of nearshore submarine fan is the most favorite facies ; the steep slope of the depression mainly consists of structural reservoirs, the slope belt mainly consists of structural - lithologic and updip pinchout reservoirs, the depressed belt mainly consists of lenticular lithologic reservoirs
摘要對陸家堡凹陷油藏形成的石油地質條件、已知油藏類型及分佈的分析認為：生油區、生儲配置關系、儲集物性、沉積相帶和二級構造帶控制了油藏的形成和展布，其中圍繞生油窪陷的油藏含油最豐富；夾持或嵌入主要生油層中，儲層發育、儲集物性又相對較好的九佛堂組上段是主要含油層段；近岸水下扇的扇中和扇三角洲前緣是最有利的相帶：凹陷的陡坡帶以構造油藏為主，斜坡帶以構造巖性及儲層上傾尖滅油藏為主，深陷帶主要為透鏡狀巖性油藏。 -
In summary, we constructed a structure framework on the eastern district of the nanpanjiang depression, made a new structure regionalism, confirmed that the border of nanpanjiang depression was nandan - du ' an fault and xialei - lingma fault, and analyzed the structural characteristics of secondary structure units in detail
在上述研究的基礎上，對南盤江坳陷東部地區進行了構造格架的建立和構造區劃，確定了南盤江坳陷的東部邊界為南丹-都安斷裂帶，南部邊界為下雷-靈馬斷裂帶；並對二級構造單元的特徵進行了分析。 -
The northeast ehen secondary fault depression, maoxi fault - nose and maonan slope should be favorable places for prospecting in the near future
提出了額很窪陷東北部和毛西斷鼻構造以及毛南斜坡，是近期首選的有利勘探目標區帶。 -
It is suggested that " maodun intrusion " may be an pre - cretaceous intrusion, that the early cretaceous " hantamiao secondary depression " divided by the predecessor may not exist. maonan fault might activited strongly during pre - cretaceous
「毛敦侵入體」可能為一前白堊紀的侵入體，前人所劃分的早白堊世「罕塔廟次凹」可能不存在，毛南斷層可能為一前白堊紀強烈活動的老構造。
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