western basin 中文意思是什麼
western basin
解釋
西海盆-
Structural features and evolution of contemporaneous reversed faults in gas faulted depression in western qaidam basin
柴西地區尕斯斷陷同生逆斷裂構造特徵與形成演化 -
Holocene extreme floods and environmental change of qishuihe river in western guanzhong basin
關中西部漆水河全新世特大洪水與環境演變 -
The topography and the physiognomy of the south china sea are very complex such as continental slop, continental shelves, seamounts, sea basin, etc. the south china sea lies between qingzang plateau, which is as the main driver of the variety of climate, and the western part of the pacific, which is called warm pool, and is influenced by some current systems, such as coastal current, kuroshi, etc. the south sea has considerable species
南海具有陸坡、陸架、海溝、海盆等復雜的地形、地貌；南海位於作為地球氣候變化的主要驅動力的青藏高原和西太平洋暖池之間；南海受到沿岸流、南海暖流水、黑潮入侵水等流系的影響；南海具有豐富的物種分佈；上述因素共同影響南海生源要素的分佈、輸送和遷移。 -
The results indicate : ( 1 ) the distribution of magmatic rocks shows the feature that in the middle and western part of the study area basic igneous rocks dominate, and in the middle - eastern part intermediate rocks are predominant, while in the southeastern part acid ones are developed. ( 2 ) in the area west to the shiwandashan basin, intermediate magmatites were controlled by deep ne - striking and nw - striking faults, especially at the conjunction site of these two group faults, magmatic activity was strong ; and its tectonic background can be attributed to extensional continental rift
其中，在十萬大山盆地以西地區的偏基性巖漿活動受北東和北西向深斷裂控制明顯，尤其以此兩組斷裂交匯處的巖漿活動強烈，盆地構造背景屬大陸伸展裂谷環境；在十萬大山盆地以東地區為偏酸性巖漿活動，主要受東吳運動形成的欽防造山帶的控制，屬大陸邊緣造山帶或島弧造山帶環境。 -
By the application of the method in eighteen wells in the western depression of sichuan basin, it achieves good effect in the recognition of low permeability and low porosity tight clast of the western depression of sichuan basin
通過對川西坳陷十八口井的實際應用，此方法在低孔低滲的緻密碎屑巖巖性劃分中取得了良好的效果。 -
Geological characteristics and natures of mesozoic continental basin in western liaoning, china
遼西中生代波羅赤盆地特徵及盆地性質探討 -
According to these results combined with exploration practice, foot favorable exploration zones are selected, these are the integrated anticline traps below the tertiary gypsum halite, gypsum mudstone in kuqa foreland thrust belts, the second and the third row structural bells in southern junggar foreland thrust belt, the unconventional natural gas pools in die yanshan palaeohigh in north and south of western sichuan basin, the gentle fold structural belt in central sichuan basin and the deep depression in sichuan basin, and the cold take and nanbaxian structural belt in northern margin of qaidam basin
依據理論分析及勘探實踐，優選出4個有利的勘探區帶，它們是：庫車前陸沖斷帶古近系、新近系膏鹽巖、膏泥巖之下的完整背斜圈閉；準南前陸沖斷帶第二、第三排構造帶；川西北部及南部燕山運動期古隆起、川中平緩褶皺構造帶以及深坳陷內部的非常規天然氣；柴北緣冷湖南八仙構造帶。 -
Hytrocarbon exploration prospect of jurassic in the western qaidam basin
柴達木盆地西部侏羅系油氣勘探前景 -
Paleokarst cave features of the western fringe of e ' erduosi basin
鄂爾多斯盆地西緣古巖溶洞穴特徵 -
Based on the core description, logging analysis and classification at home and abroad, the reefs in western qaidam basin may be classified into algal reef, stromatolites and thrombolites
通過巖心描述、測井分析，並根據國內外生物礁的分類標準認為，柴西地區的生物礁主要包括藻礁、疊層石和凝塊石礁。 -
The western hubei - eastern sichuan area is located at the junction belt between the eastern sichuan folded belt in the sichuan basin and xianexi folded belt, belong to eastern extended part, which is similar to the eastern - sichuan structure in many aspects. for example, they share a structural unit, resulting in the same sedimentary history and the same generation - reservoir - seal assembly as each other
鄂西渝東區處於四川盆地川東褶皺構造帶與湘鄂西褶皺帶的接合部位，屬川東褶皺帶東延組成部分，具有與川東相似的沉積發育史與生儲蓋組合；相同的構造發育史與構造形式；類似的天然氣藏類型與保存條件。 -
Through the regional background analysis in which western structures developed, it suggested that there did not exist a united and steady block to the west of ordos basin. alashan block neighboring on the north of the western margin was largely influenced by the action of qilian and tianshan - xingmeng folded belt which is respectively to the south and north of alashan block, was narrow in the steady block and was limited by the longshou mountain - zhongwei strike fracture in the south area
通過對鄂爾多斯盆地西緣構造發育的區域構造背景分析，認為在鄂爾多斯盆地之西，一直沒有一個統一的穩定地塊相鄰，與盆地西緣北部相鄰的阿拉善地塊，受南北相鄰的祁連褶皺帶和天山興蒙褶皺帶活動的影響，較穩定地塊的范圍比較狹窄，其南又有龍首山-中衛走滑斷裂構造帶存在。 -
In the link party of qinling - qiliang - kunlun belt, the polyarc - basin systemic characteristic is discussed with strengthen and standout study on the detail relationship analysis between the arc - basin. the bayan har basin thought to be the preexistence of the songpan - garze belt, is a back - arc basin among a series of polyarc - basin systems behind the qiangtang - taniantawong front the arc beginning in the late paleozoic. the eastern margin started as the western passive continental margin of the yangtze block ( d - t2 ), then changed into a foreland basin related to the north china block and the qiangtang block during the middle to late triassic
在秦祁昆侖結合部研究中，加強和突出了精細的島弧盆分析和造山作用關系的研究，探討了秦、祁、昆結合部多島弧盆特徵；通過巴顏喀拉地區沉積特徵，沉積體的空間展布和形態，面式物源供給方式，礦物成分和地球化學背景分析，其沉積盆地屬性總體上反映出一個從過渡地殼-洋殼基礎上發育起來的周緣前陸盆地的發展和演化過程。 -
( 1 ) abnormal high velocities mainly exist around qingzang plateau, especially in junggar, tarim, qaidam and sichuan basin, velocities there are higher than 8. 2 km / s. ( 2 ) low velocities only exist in the middle of qingzang plateau and western part of sichuan and yunnan region. in eastern china, low velocities are predominant
整體上中國東西部存在明顯差異，西部地區速度變化以高速異常為主：高速異常區主要是沿青藏高原隆起區的周邊分佈，特別是準噶爾盆地、塔里木盆地、柴達木盆地及四川盆地都呈明顯的高速，均超過8 . 2km / s ；青藏高原隆起區的中部，顯示出速度的低異常帶；位於青藏高原東南緣的川滇西部地區速度呈現低異常。 -
In himalayan, the first era ( 45ma ) the basin is titled ; the second era ( 23ma ) it is differential uplift and denude ; the third era it is brittle defonnation. in eastern ore belt, ore - controlling is mainly strike - slip fault and fold ; but in western ore belt, it is block
喜馬拉雅運動第一期45ma盆地掀斜；第二期23ma以差異隆升剝蝕為主；第三期4ma為脆性變形期，東礦帶近盆邊以走向斷裂及褶皺控礦為主，西礦帶為斷塊控礦。 -
Genetic features of western geothermal resources in tai - lai downfaulted basin
泰萊斷陷盆地西部地熱資源的成因 -
In liaohe rifted basin, du66 block is situated on the middle part in the western slope in the western depression, and is a typical thin - interbedded reservoir with heavy oil
摘要杜66塊位於遼河斷陷盆地西部凹陷西斜坡中段，為一典型的薄互層狀普通稠油油藏。 -
The tholeiite with late trassic age has been found in helanshan area on the north part of western margin of ordos basin
在盆地西緣北部賀蘭山地區，發現典型拉張環境形成的拉斑玄武巖，測年時代為晚三疊世。 -
Study on slope breaks of the late cretaceous depression basin around the western slope in the southern songliao basin
松遼盆地南部西部斜坡區晚白堊世坳陷盆地坡折帶研究 -
This extensional activity is similar to the basin - and - range province of western america, and can be thought as an intra - continental tectonic system
此外，揚子地塊西緣二疊紀的大陸伸展作用類似於美國西部的盆嶺區，總體表現為大陸板塊陸內構造體制。
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