depression region 中文意思是什麼

depression region 解釋
低壓區
  • 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 【...
  • region : n. 1. 地方，地域，地帶；地區；行政區，管轄區，區；左近，鄰近；（大氣、海水等的）層，界，境。2. 【解剖學；動物學】（身體的）局部，部位。3. （學問等的）范圍，領域。4. 〈罕用語〉天空。
  1. 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。
  2. 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。
  3. The results show that the long - flame coal distributs in the six coal - rich regions, the lignite distribute in southwest and north central region and gas coal distribute in south central of eastern depression on plane

    在平面上，長焰煤在東部凹陷的6個賦煤區均有分佈，褐煤分佈於東部凹陷西南端和中北部，氣煤則集中分佈於該凹陷的中南部。
  4. Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin

    通過對平莊盆地基礎地質資料、國內外大量地熱地質資料的分析和野外地質調查、礦井實測地溫以及上升泉、斷層涌水的地球化學分析等工作基礎上，指出地處低地溫梯度背景區的平莊盆地地溫梯度異常是由於盆地基底隆起和坳陷引起傳導型大地熱流再分配所致；運用州sys數值模擬了大地熱流向地表傳導背景下的盆地地溫場，從而揭示了盆地基底（義縣組）頂界面地溫分佈特徵；闡明了盆地具有形成中低溫對流型地熱系統所必需的導水斷裂、補給水源等的良好條件，中低溫對流型地熱系統是地熱勘查的主要對象；圈定了平莊盆地北部朝陽溝?駱駝營子地熱勘查遠景區。
  5. The cover faults in daqing region are mainly developed in formation of huoshiling member late jurassic and its cover formations. according to their formation period, activity characteristics and penetrating relationship, four types of faults were divided, that is fault - depression faults, depression faults, inverted - strike - slip faults and inverted - extension faults ; according to the activity history of the faults, five types of faults were divided, that is long - term active faults, early active faults, early - medium - term active faults, medium - term active faults and terminal active faults

    大慶地區內發育在晚侏羅世火石嶺組及其以上的沉積蓋層中的蓋層斷裂，依斷層形成時期、活動特徵及切割層位可將蓋層斷層細分為四種類型，即斷陷期斷裂、坳陷期斷裂、反轉走滑斷裂和反轉張性斷層；按其活動歷史可以分為五種類型：即長期活動斷層、早期活動斷層、早-中期活動斷層、中期活動斷層和晚期活動斷層。
  6. In 1999, the dipole existed in between the okhotsk high and the depression in the north of northeast china, thus the okhotsk high became active and maintained, the subh was located to an area quite further south than usual. the high persisted in the east region of nw china, the cold air flowed to the mid - lower reaches of the yangtze river along the high. in the east region of nw china, air steam under troposphere was strong sinking motion, and formatted the negative vorticity region, the vapour flux divergence was divgence. lt was apparently that the rain could n ' t occur in the eastern portin of nw china. in 2000 year, okhotsk high was very weak or did n ' t exist in, there was high in the east asia - japan, the subh is located to an area further north than usual. in the east region of nw china, the trough maintained, air stream under troposphere was strong ascending motion, the cycolonic circulation was prevailing, the vapour flux divergence was intensive convergences the rain easy happened in the east areas of northwest china

    4多梅雨1999年鄂霍茨克海阻塞高壓與我國東北北部低壓形成偶極子，使得阻塞高壓穩定少動，西太副高位置偏南，西北地區東部持續受高壓控制，冷空氣沿此高壓流經長江中下游地區上空；在西北地區東部對流層中下層氣流下沉運動較強，呈反氣旋渦度，水汽通量散度輻散，不利於西北地區東部降水。空梅雨2000年相反，鄂霍茨克海高壓減弱甚至不存在，東亞-日本為高壓，西太副高位置偏西偏北，西北地區東部處于西風槽中，對流層中下層氣流上升運動增強，盛行低壓環流，水汽通量散度強烈輻合，有利於降水生成。
  7. Sedimentary filling models and types of fault - bounded margin in actic region of the northeastern dongpu depression

    東濮凹陷陡坡帶北部控凹斷裂樣式及砂體充填模式
  8. 5. by summarizing the distribution regularity of existing oil & gas fields, it is found that all kinds of oil & gas reservoirs are distributed around the qikou depression like rings, which are divided into inner ring oil - bearing belt, infer ring oil - bearing belt and outer ring. the inner ring is central of oil - bearing region in qikou depression, which is controlled by haihe faults and qidong faults. the inter ring is in regions which are prospect for oil and regions with paleogeographic background of low - gradient slogze. the outer ring is regions. which are outside the oil - bearing region and inside the oil & gas migration region, with paleogeographic background of buried - hill and faults controlling the basin, ect

    5 、通過對已知油氣藏分佈規律的總結，發現各類油氣藏圍繞歧口凹陷生油中心呈環帶狀分佈，分為內環、中環、外環三個含油帶。內環為海河斷裂和歧東斷裂控制的歧口凹陷生油中心區，中環為有利生油區范圍內和緩坡古背景上的地區，外環為生油區范圍以外、油氣側向運移范圍以內的以古潛山為背景或控盆斷裂帶等區域。
  9. Depositional system and its hydrocarbon characteristics of shahejie group of shengtuo region in dongying depression

    東營凹陷勝坨地區沙河街組沉積體系及其油氣源特徵
  10. Deep viscous crude oils, with depth more than 1800m, widely occur in jiyang depression, especially in loujia - kenxi region. here, based on geological, geochemical and geophysical data, these oils were described and studied extensively in physical properties, sulfur contents, gross compositions, geochemical characteristics and reservoir features. finally, we discussed the formation mechanism and outlined some exploration strategies of these viscous oils

    本論文從石油地質、地球化學和地球物理多方面系統研究了濟陽坳陷（尤其是羅家-墾西地區）深層稠油的物性、地球化學特徵、儲層特徵以及源巖地球化學特徵，探討本區域深層稠油的形成機理和分佈、富集規律。
  11. The importance results and achievements in this thesis are follow : ( 1 ) stratum sequence qikou depression, huanhua basin is partitioned using sequence stratigraphy theory. 6 third class sequences are identified. each sediment sequence system region and system distributing law is studied

    通過理論分析、實驗研究和實際資料綜合分析，取得了如下主要成果： （ 1 ）利用層序地層學學原理對歧口凹陷第三系地層進行了層序劃分，識別出6個三級層序，並對每個層序體系域與沉積體系展布規律進行了研究。
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