crust movement 中文意思是什麼
crust movement
解釋
地殼運動-
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。 -
Continental drift is now believed to reflect the movement over geological time of underlying plates in the earth ' s crust - the theory of plate tectonics
板塊構造學說提出后，大陸漂移說又獲得了新的含義，它反映了地殼運動和大州大洋的分佈規律。 -
The movement and deformation of the crust are the comprehensive effects of various kinds of the geodynamical processes on the ground, and the systematical response of the crustal medium to the plate tectonic and deeply dynamic evolution. therefore, the research for them becomes one of important contents in the geodynamic studies
地殼的運動和變形是各種地球動力學過程在地表的綜合顯現，是地殼介質對板塊構造和深部動力過程作用的綜合響應，因此，對地殼運動和變形的研究構成了地球動力學研究的重要內容之一。 -
Such features might result from the rotation movement of the earth crust and exert serious impact on the geotectonic evolution and large scale metallogeny in hunan province and adjacent regions
這種特徵可能是地殼的旋轉運動所造成，它對湖南及鄰區大地構造的演化、大規模成礦作用等具有重大的影響。 -
Through the analysis of the deduction process of harmonic function model, it is illustrated that some hypotheses in the deduction process are unreasonable and the harmonic function can not reflect the objective regularity of the vertical crust movement, so that it isnt an effective method to compile isoline map of the vertical crust movement rate
對有關文獻提出的「地殼垂直運動調和分析」模型的建立過程作了全面分析，指出：該模型建立過程中所做的一些處理是不合理的，由此建立的模型不是地殼垂直運動規律的客觀反映，因而尚不足以成為編制地殼垂直運動速率面等值線圖的可靠手段。 -
The characteristics of the movement and deformation of the crust were traditionally determined with the geological and seismographic methods. however, the result obtained with the geological and seismographic methods is virtually an average one on the time scale of millions and / or hundreds of years, and the current movement and deformation of the crust cannot be described well
傳統上，一般用地質和地震學方法來確定地殼的運動和變形特徵，但二者確定的地殼形變結果分別是百千萬年和百年左右的平均結果，難以描述現今地殼運動和變形的特徵。 -
" but at the same time, a horizontal pulling power inside the lower continental crust and mantle of the earth counteracts this upward movement, " said bian
「但同時，從下地殼一直到地幔上部在產生一種東西拉張的力量，這種拉力對喜馬拉雅山的繼續升高起到了阻礙作用。 」 -
A physical model for describing the fault movement along plate boundary is proposed, i. e., the crust movement along plate boundary equals to the relative rigid plate motion plus negative dislocation distributions on the fault planes
提出了一種描述板塊邊界斷層運動的力學模型，即將板塊邊界的地殼運動表述為板塊的相對剛體運動加邊界斷層面上的負位錯分佈。 -
Second part - the main contribution and research results of this paper are focused on as follows : ( 1 ) how to use the measurements of a dual frequency gps receiver to determine the ionospheric delay correction model for single frequency gps of a local range ; ( 2 ) how to separate the instrumental biases with the ionospheric delays in gps observation ; ( 3 ) how to establish a large range grid ionosphere model and use the gps data of chinese crust movement observation network to investigate the change law of ionospheric tec of china area ; ( 4 ) how to improve the effectiveness of correcting ionospheric delays for waas ' s users under adverse conditions. ( 5 ) how to establish the basic theory and the corresponding framework of monitoring the stochastic ionospheric disturbance using gps ( 6 ) how to improve the modelling ability of ionospheric delay according to its diurnal, seasonal, annual variations based on gps ; ( 7 ) how to meet the demand of correcting the ionospheric delay of high - precision orbit determination for low - earth satellite using a single frequency gps receiver 1 extracting ( local ) ionospheric information from gps data with high - precision the factors are systematically described and analyzed which limit the precision of using gps data to extract ionospheric delays
二、具體研究工作的系統報告，主要集中在以下幾方面：研究如何利用單臺雙頻gps接收機的觀測信息確定電離層延遲改正模型，為小范圍的單頻用戶服務；研究如何實時分離gps觀測中的儀器偏差與電離層延遲；研究如何建立較大區域的電離層格網模型，進而初步設想利用中國地殼運動觀測網路深入研究我國領域的電離層的電子濃度變化規律；研究單頻用戶在不利條件下，如何更好地利用電離層延遲改正信息；研究利用gps監測隨機電離層擾動的基本理論和框架方案；研究如何綜合顧及電離層的周日、季節和年變化，進一步提高利用gps模擬電離層延遲的能力；研究如何實現星載單頻gps低軌衛星的精密測軌中的電離層延遲改正要求。 -
Perhaps you have seen colorful limestone cave and underground river, but the eighteen caves here are mesozoic lava land forms, which is produced by the movement, cracking and weathering of the earth ' s crust
或許你見過絢麗多彩的石灰熔洞和地下暗河，但在這里的十八個山洞卻是中生代火山巖地貌，由於地殼運動斷裂風化形成的。 -
The continental orogenesis is characterized with the following features, such as sudden start, global synchronicity and horizontal movement, occurring mainly in the upper part of the crust and weakening with depth, and so on
摘要大陸皺造山運動具有突發性、全球同步性，以水平運動為主，主要表現在地殼上部且具有上強下弱等特徵，除水平運動一項外，與基於地幔對流的板塊構造理論缺少共同之處。 -
Structural movement of earth crust from north to south cause the riverway move from north to south
自北向南的構造掀斜運動造成了河道自北向南移的特點。 -
From the viewpoint of neotectonic movement, the formatio n and characteristics of natural landscapes controlled by neotectonic movement i n the strong crust raising area, slightly raising area, subsiding area and trans ition area of northeast poyang lake region are discussed, and some suggestions a bout tour land planning and development in different areas are made
從新構造運動的觀點出發，討論了在鄱陽湖東北地區新構造運動強烈抬升區內、沉降區內、輕微抬升區內及過渡區內的旅遊自然景觀的形成、特點，並提出了合理規劃和開發不同區域內旅遊用地的建議。 -
Coefficients of ocean tidal displacement corrections for china crust movement observatory network
中國地殼運動觀測網路的海潮位移改正系數 -
Earth ' s layered structure - - a relatively thin crust of mobile plates, a solid mantle with gradual overturning movement, and the outer and inner core of molten and solid iron
地球是分層結構?相對運動變化的板塊薄的外殼，一塊具有逐漸加強的顛覆運動形式的固態硬殼，具有遠離中心的外層和內部熔化的內核和固態鐵。 -
Correction problem of the ocean loading signals to strain field variation at foundational stations in crust movement observation network in china
中國地殼運動觀測網路基準站應變場變化的海潮負荷信號改正問題 -
Correction problem of the ocean loading signals on tilt measurements at fundamental stations in crust movement observation network in china
中國地殼運動觀測網路基準站傾斜固體潮觀測中的海潮負荷信號改正問題 -
Ocean tidal displacement correction for crust movement network of china
中國地殼運動網路的海潮位移改正 -
As well, many prospects will be shown here, like ancient biology models, demo of the earth ' s crust movement and life disaster
在這里遊客可以看到各種古生物模型，地殼運動演示、生命大災難等圖景。 -
At the same time, pulsating compressive force due to the crust movement including earthquake also made the crystallized rock ruptured and form ore control fault fracture and the host fracture
殘漿的形成與排出，控礦構造的發生、發展與控礦過程，都是在這次地殼運動過程中完成的。
分享友人