chagan 中文意思是什麼

chagan 解釋
恰甘
  1. The method has triumphantly applied in sag evaluation in chagan depression, and enhanced the forecast of exploration targets, and achieved favorable effect, and auspicated a new way of exploration for similar lower exploration mid - small basins

    該方法成功地應用於查干凹陷的凹陷評價中，提高了勘探目標的預測能力，獲得了良好效果，為類似中小盆地的低勘探程度地區的勘探創出了一條新路。
  2. 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。
  3. 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。
  4. Through studying it is shown that in chagan sag, the geothermal gradients in the center are higher than those around the sag margin and major factors influencing the characteristics of temperature field distribution are the property of geotectogenesis and the differences in tectonic portion, lithology and underground water behaviour ; there are three types of mudstone compaction, i. e. normal compaction, undercompacition and overcomepaction ; there are two pressure systems in sandstone reservoirs, i. e. normal pressure and negative pressure systems and the strata ' s being uplifted and denuded is the key factor leading to the formation of the negative pressure system in reservoir ; and the distinctive temperature - pressure field characteristics in the sag are possessed of important petroleum geological significance in hydrocarbon source maturity, hydrocarbon generation, widening on oil and gas exploration domain and selecting exploration targets, etc

    研究表明，查干凹陷中心的地溫梯度高於凹陷邊緣，大地構造性質及所處構造部位、巖性與地下水活動的差異是影響凹陷地溫場分佈特徵的主要因素；泥巖壓實存在正常壓實、欠壓實和過壓實三種類型，砂巖儲層段壓力類型可分為正常和負壓兩個系統，地層抬升剝蝕是導致儲層負壓系統形成的主導因素；凹陷獨特的溫壓場特徵對烴源巖成熟、油氣生成、油氣勘探領域的擴大及勘探方向的選擇等具有重要的油氣地質意義。
  5. The hanging wall of sag extended in southeast direction, with the tulage fault being the boundary fault. yinggete - bagemaode metamorphic core complex developed adjacent to northwest of chagan sag, which evolved from late jurassic to cretaceous with three - layer construction style. the kinematics mechanism of metamorphic core complex and chagan sag is a simple shear model, chagan sag extended and faulted as the metamorphic core complex rised

    在查干凹陷西北側發育英格特?巴格毛德變質核雜巖帶，可能具有三層結構模式，其形成與演化時代為晚侏羅世末?白堊紀；該變質核雜巖與查干凹陷的運動學機制為統一的簡單剪切模式；在變質核雜巖隆升的同時，查干凹陷發生伸展斷陷。
  6. Guided by the theory of sequence stratigraphy and petroleum system using cores, lithologic log or well - logging, biostratigraphic and seismic data, adopting seismic inversion constrained to well data, digital analysis technology, basin modeling, test method and so on, and adopting an integrated study technology, aiming at lower exploration in chagan depression, this work put forward a new research thoughtfulness, technic flow and method system that is an integrated study by " looked upon sequence stratigraphy as a base, looked upon petroleum system as a integer, combing with each other closely " and tie in qualitative analysis and quantitative analysis and applied synthetically new theory, new technology and new method

    以層序地層理論和含油氣系統思想為指導，利用巖心、鉆/測井、古生物以及地震資料，採用井約束下的地震資料反演技術、計算機技術、盆地模擬技術和各種分析實驗手段等綜合分析方法，針對查干凹陷勘探程度低的特點，提出了斷陷盆地「以層序地層分析為基礎、含油氣系統為整體（系統）和二者緊密結合」以及定性與定量相結合，綜合應用新理論、新技術和新方法的研究思路、技術路線和方法體系。
  7. The main structure style of chagan sag included four kinds, such as extension, compression, inversion and strike - slip structure, in which the extension structure was the principle part

    查干凹陷的主要構造樣式包括伸展、擠壓、反轉和具有走滑分量的構造，其中伸展構造是主體。
  8. It could be divided into six paleogeotemperature evolution stages from early cretaceous to recent based on the result of apatite fission - tracks analysis ; subsidence - buried history analysis shows that chagan experienced fault depression stage during early cretaceous bayingebi - suhongtu period, transional stage from fault depression to sag in yingen period, and sag stage since wulansuhai stage

    磷灰石裂變徑跡模擬分析結果認為早白堊世至今大致可分為6個古地溫演化階段；沉降?埋藏史模擬揭示查干凹陷經歷了早白堊世巴音戈壁?蘇紅圖期的斷陷期、銀根期的斷?坳陷轉化期和晚白堊世烏蘭蘇海期以來的坳陷期。
  9. After have systematically studied sequence stratigraphy of chagan depression, a analysis method of high precision sequence stratigraphic framework in fault - depressed lacustrine basin. the core of the establishing framework is exploration - significant identify of sequence, division of 2, 3, 4, 5 grades sequence and analysis of base - level based on lithologic log or well - logging, high - resolution seismic inversion constrained to well data. then using the results of 2d seismic data, and interpret sequence to enhance the precision of interpretation

    斷陷盆地高精度層序地層格架建立的核心是用鉆/測井和井約束條件下的高解析度儲層橫向預測剖面等高解析度資料進行具有勘探意義的二、三、四和五級層序的界面識別、層序劃分和基準面變化分析，在此基礎上標定常規地震剖面，進行區域層序地層分析，達到提高層序地層解釋精度的目的。
  10. Evolution and sequence stratigraphic framework of lower cretaceous in chagan depression

    查干凹陷下白堊統層序地層格架與演化
  11. The sixth, build the floodwater utilization model, put forward the concrete measure and way to solve chagan lake water resources, and analyzed the effect on the flood detention of jilin chagan lake wetland the seventh, analyzed the influence of floodwater utilization to the environment, and put forward water resources protection measure of jilin chagan lake wetland

    6 、建立了吉林省查干湖濕地洪水利用模型，提出解決查干湖濕地水資源的具體措施和途徑，分析查干湖濕地蓄滯洪作用。 7 、分析評價了吉林省查干湖濕地洪水利用對環境的影響，提出查干湖濕地水資源保護措施。
  12. With jilin chagan lake wetland and the western chiefly river flood resources of jilin province as studying the focal point, this research analyzed wetland restoration necessity on making use of floodwater resources, and has put forward the allocation model of chagan lake wetland water resources and the concrete measure of recovering wetland and protesting the wetland water resources

    本研究以吉林省查干湖濕地及吉林省西部主要河流洪水資源為研究重點，分析利用洪水資源恢復查干湖濕地的必要性和濕地滯洪的重要作用，提出了查干湖濕地水資源配置模型及恢復濕地和保護濕地水資源的具體措施。
  13. Yinggete - bagemaode metamorphic core complex belt with three - layer construction is put forward, which evolved from late jurassic to cretaceous. the extensional simple shear model of the chagan fault depression is established. the tectonic evolution and the dynamics character of chagan fault depression and its adjacent mesozoic - cenozoic basins are discussed : at the end of triassic continental orogeny increased crust thickness crust uplift and denudation were happened ; jurassic was a period of local partly extensional collapse of erogenic belt and cretaceous was a period of widely extensional collapse of postorogenic erogenic belt ; cenozoic was a period of the development of stable intracontinental depression with the character of long distant collision response and weaked compression flexure

    討論了查干凹陷及鄰區中-新生代盆地構造演化及其地球動力學特徵，三疊紀（印支期）為陸內造山作用與地殼增厚、隆升剝蝕階段；侏羅紀（燕山早期）為造山後造山帶的局部伸展垮塌階段；白堊紀（燕山晚期）為造山期后大規模伸展垮塌作用與伸展盆地的發育階段；新生代（喜山期）為遠距離碰撞效應與弱擠壓撓曲性質的穩定大陸內坳陷的發育階段。
  14. The structure evolution and the earth dynamics mechanism of chagan sag and its adjacent area during miocene - cenozoic. divided four favorable places for prospecting based on the discussion of relation between the structure character and petroleum and gas of chagan sag

    論文還討論了查干凹陷及其鄰區中?新生代的盆地構造演化及其地球動力學特徵，探討了查干凹陷構造特徵與油氣的關系，劃分了四個有利勘探區帶。
  15. The structure units are redivided. the main structure style of chagan fault depression is summarized, in which the extensional structure are the principle part. its kinematics characteristics are analysed

    對查干凹陷的構造單元重新進行了劃分，總結了查干凹陷的主要構造樣式，伸展構造是主體，並對其運動學特徵進行了分析。
  16. The third, analyzed the cause of formation type resource situation and the major development and degenerating course of jilin chagan lake wetland the fourth, analyzed jilin chagan lake wetland water resource situation as well as the floodwater characteristics of western chiefly river of jilin province : the tender river the tao river the huolin river and the second songhua river

    3 、分析了吉林省查干湖濕地的成因、類型、資源狀況及濕地演變退化的主要原因和過程。 4 、分析研究了吉林省查干湖濕地水資源狀況，以及吉林省西部主要江河：嫩江、洮兒河、霍林河、第二松花江流域的洪水特性及洪水資源特點。
  17. The sediment stratum in chagan depression is devised into tree supersedences. among them, lower cretaceous can be devised into eight sequences and twenty - two system tracts which have been studied in characteristics of sedimentary cycle, distribution and genetic analysis. after this study, formed mechanism, distribution model and evolvement of sequence have been put forward

    查干凹陷共劃分出3個超層序，研究目的層下白堊統劃分出8個層序， 22個體系域，並進行了層序地層格架的層序沉積旋迴特徵、層序展布特點和層序成因分析，提出了斷陷盆地層序的形成機制、層序地層分佈模式與演化模式。
  18. Study on leachability of silver in oxidized zone of the chagan silver deposit in inner mongolia

    內蒙查干銀礦床氧化帶中銀的氰化浸出可行性研究
  19. The fifth, confirmed the wetland restoration object and the balance of supply and need of water resources of jilin chagan lake wetland

    5 、確定了吉林省查干湖濕地恢復目標及水資源供需平衡分析。
  20. Chagan fault depression has favorable petroleum geology conditions, the evolution of its source rocks could be divided into three stages

    查干凹陷具有較好的石油地質條件，烴源巖有機質演化在垂向上可劃分為三個階段。
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