盆地內的 的英文怎麼說
中文拼音 [péndenèide]
盆地內的
英文
intrabasinal-
Further research of lithofacies pvove : lode country output points belongs to tidal - flat facies. and the two sides belong to littoral facies - estuarine facies. ore area petrochemistry analyse also prove : intraclast congeries silica rock in basin have higher cu, ag abundance than circumference pena. the prominence inhomogeneity of the cu distribution indicates reconstruct of the late construction
礦區內巖石化學測量也證明:盆地內發育的內碎屑堆積硅質巖比周圍巖石具有更高的cu 、 ag元素地球化學豐度值, cu元素分佈的顯著不均一性,表明了後期構造的改造作用。In addition, the dq - q curves behave in different shapes. it can be concluded that the scaling properties depend colsely on the way, intensity. acting scale and distribution in space of inogenic and exogenic processes. according to the scaling natures of the two landform profiles, it is proposed that the 5km scale is the low limit of the inogenic process effects which begin to dominate landscape patterns in landform systems
該結果對理論地貌研究具有重要意義:不同地貌類型表面的多重分形譜值域表現為高山區中低山區盆地區的總體特徵,地貌表面多重分形譜特徵表明了內外營力地貌作用類型和強度在空間上分佈的不均勻程度。The city had over 250 thousand inhabitants in 2000, of which the majority was uyghurs. because of its geographical condition, the foehn phenomenon occurs and raises average temperature to 32. 7 degrees in july
由於吐魯番盆地四周的山嶺高聳,盆地內部受熱快而散熱慢,形成了那裡夏天高溫乾燥的氣候,在舉辦自行車賽的7月,平均氣溫高達32 . 7度。Compared with lehua manganese deposit in pingxiang - leping faulted basin, which is a sedimentary hydrothermal superimposed type, both orebodies are different obviously in orebody scale, ore type and tenor of manganese etc., it should be a deposit with different genetic type
並與萍一樂斷陷盆地內的沉積加熱液疊改型樂華錳礦床進行了對比分析,二者在礦體規模、礦石類型、錳品位等方面存在顯著差別,應屬不同成因類型的礦床。Occurred in the neozoic, the strong himalayan movement made the first order and the second order structure units uplift to form maintains in the basin, which are unfav orable to preserve oil and gas
新生代發生的強烈的喜山運動,促使盆地內部各一、二級正向構造單元進一步沖斷上隆、甚至生長為盆內山脈,對古油氣藏保存不利。The regional structure interpretation with 3d seismic data shows that the graben and shied mode faults of the baigezhuang, which developed a series of normal faults which stroked in ne ( nee ) and dipped nw or nw, came into being in the rift development stage of ii act of the bohai bay rift basin in mesozoic and cenozoic and resulted from the protrudent boundary of the basin, i. e. the strike - slip and stretch processes of baigezhuang fault
同時,用三維地震資料進行區域構造解釋分析,論述了柏各莊地區的構造樣式,是中新生代渤海灣裂谷盆地的幕斷陷發育階段,同時由於盆地內凸起邊界?柏各莊斷層的走滑兼伸展作用,使柏各莊凸起的中生界形成壘、塹斷塊群構造樣式,發育一系列ne ( nee )向,傾向nw或sw的正斷層。The sankeng geothermal field is located on the northeastern side of the wuchuan - sihui deep fault and in the sankeng synclinal karstic basin
摘要廣東三坑地熱田位於吳川四會深大斷裂帶的東北側,三坑向斜巖溶盆地內。The result is as follows : ( 1 ) cu - ag polymetallic mineralization field lied in the north of lanping basine between jinshajiang fissure and lancangjiang fissure, whose internal mid - axis fissures and different subfissures formed the fissure system of the basin. they were the transport system of the ore - forming fluid, which was important to the formation of copper - silver polymetllic deposits
研究結果表明: ( 1 )蘭坪白秧坪地區銅銀多金屬礦田位於金沙江斷裂和瀾滄江斷裂的之間的蘭坪盆地的北端,盆地內部的中軸斷裂和不同方向的次級斷裂,構成了盆地的斷裂系統,是成礦流體的運移系統,對銀、銅多金屬礦床的形成具有重要意義。Yanqi basin, located in the northern wing of the " v - type " thrust - fold belt, is related to the reversion of the kuluketage aulacogen
因此庫魯克塔格裂陷槽的構造反轉是焉耆盆地構造變形的主要力學來源。 2 、描述了盆地內的構造樣式。In the interim from highstand systems tract to transgressive systems tract, faulting is violent in the basin, different kind of fluids coming from dissimilar position of lithosphere enter into synsedimentary faults served as a place fluids mixed to form ore - bearing hydrocarbon alkali - fluids
在從高水位體系域向海侵體系域的盆地相迅速轉化時,盆地內斷裂構造活動強烈,斷裂溝通不同部位的熱水流體,使成礦烴堿流體沿斷裂上升,在海底沉積成礦。The tectonic style inside the basin is characterized by occurrence of anticlines from the margins to center of the basin, with two limbs mostly starting from reverse faults, developing a tectonic pattern of two faults sandwiching an uplift
盆地內部的構造樣式以自盆地邊緣至中心以此形成背斜構造為顯著特徵,背斜兩翼多發育逆斷層,構成「兩斷夾一隆」的構造格局。Runoff is also governed by the number and the length of streams in the basin.
盆地內的河流數量和長度也能調節徑流。( 4 ) through the analysis on the spread of inner structure, thickness change of strata and seismic and geological data in the southern basin of sertengshan - xitieshan, this paper discussed the response of oblique - thrust effect on basin
( 4 )通過對賽什騰? ?錫鐵山南側盆地內部構造展布、盆地內地層厚度變化以及地震地質資料分析,探討了賽什騰? ?錫鐵山斜沖斷裂作用在盆地內的響應。The depositional character of zhuxiang formation in the basin reads as follows : a series of nne alluvial fan were formed along the fault. the half - deep lake to deep lake faces appeared by west side of the fault, towards the west the saucer lake faces, shore deposit and flood plain face appeared in proper order. the depositional center of lower cretaceous was formed in eastern part of the basin, and the depositional depth was pinch - out and thinning out from the east to the west
盆地內下白堊統朱巷組沉積特徵表現為:沿郯廬斷裂帶呈北北東向廣泛發育了沖積扇體系,從近斷裂帶西側出現的半深湖-深湖相,向西依次為濱淺湖相到泛濫平原相的規律性分佈,沉積厚度由東向西尖滅、超覆,構成了明顯的東斷西超的盆地構造格局,表明下白堊統的沉積中心依然位於盆地東部。Based on crater densities within the basins, spa appears to be the oldest and orientale the youngest
根據盆地內的隕石坑密度估算, spa盆地似乎最古老,而東方海則最年輕。According to t he major controlling factor, passage of fluid migration, to thermal fluid flow, it divides thermal fluid flow into four types : ( 1 ) lithologic - type, ( 2 ) conformity - t ype, ( 3 ) fault - type and ( 4 ) compound - type
根據控制熱流體活動的主要因素之一- -流體活動通道,將沉積盆地內的熱流體活動類型劃分為巖性型、不整合型、斷裂型和復合型四大類。Through studying it is indicated that in sedimentary basin the thermal fluid flowing process belongs to a dynamic balance between accumulation and dispersion under the action of the principal drive mechanism formed by pressure system essentially
研究表明,沉積盆地內的熱流體活動過程,實質上是一個在壓力系統這一主要驅動機製作用下的流體聚散動平衡過程。There are coherent between the spread of oblique - thrusting structure, fold and fault structure. there were close relationships between oblique - thrust structure and the reverse " s " structure in the basin. both of them are result of the left oblique - thrusting
逆沖推覆構造呈斜列式形展布與盆地內的也呈斜列式反「 s 」形展布的構造具有密切關系,都屬于斷裂左行斜沖的產物。Rong hua plastics and hardware manufacture in jin sha, nan hai was established in 1998, covering an floorage of 4, 000m2above. located if guo jia development district of jin sha, nan hai in the abundant peal river delta, we make good use of the favorable resources environment in guang dong and rich experience in manufacture and sales. we adopt advanced designing philosophy, purchase brand new precision manchinery and strictly follow the iso9001 mannagement system for production and quality control. we also have applied for a number of national patents in industrial design and utility model. by researching and developing more variety for local and overseas preferences, we ride with the latest trend in the world
南海金沙榮華塑料五金廠,創建於1998年,實用面積四千多平方米,位於富饒的珠江三角洲注入盆地內的南海金沙郭家開發區內,自成立以來憑借廣東優厚資源環境和成熟的生產、銷售經驗,先進的設計理念,全新、精密的機械設備,嚴格效仿iso9001國際標準生產和品質管理體系,並申辦多項外觀,實用型國家專利,研製開發適合本土,海外各處風土喜愛、品味、格調的品種來迎接潮流發展走勢。The calculated results of the model indicated that from year 2000 - 2020, the groundwater usage keeps a tendency of increase, while the amount of water introduced from yellow river is decreasing. this result is not only in favor of improving the eco - environment of yin - chuan basin, keeping the sustainable development of society and economy, but also play an important role in solving the problem of drying up of yellow river in downstream areas
根據模型的運行結果,直到2020年,在總用水量未超過區內水資源允許使用量的前提下,盆地內的地下水開采量呈增長趨勢,而地表水引用量則呈下降趨勢,這不但有利於銀川盆地生態環境的改善,保持當地社會經濟的可持續發展,而且對于解決黃河斷流問題也有重要的意義。分享友人