沉巖 的英文怎麼說

中文拼音 [chényán]
沉巖 英文
hydrogenic rock
  • : Ⅰ動詞1 (沉沒; 墜落) sink 2 (沉下 多指抽象事物) keep down; lower 3 [方言] (停止) rest Ⅱ形容...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  1. The sedimentation is the foundation, affecting the basic pattern of the reservoir, and the sedimentary facies zones beneficial to the formation and evolution of the reservoir includes platform edge bank facies, introplatform point beach facies and acclivity sedimentary facies, etc. ; the diagenesis is the key factor, determining the pattern and scope of the final distribution of the reservoir and being of great influence on reservoir structure, and the diagenesis of promoting the formation of storage rooms is mainly the dissolution occurred during hypergene stage and burial stage ; and the tectonism is the condition of influencing the connectivity among various reservoir bodies and among the storage rooms within a single reservoir body

    該套儲層是在4億年左右的地質歷史中,由積、成和構造作用相互影響而形成的最終成果:其中積作用是基礎,影響著儲層的基本形態,有利於儲層形成與演化的積相為臺地邊緣灘、臺內點灘和上斜坡等積相帶;成作用是關鍵,決定了儲層的最終分佈形態和范圍,對儲層結構的影響至關重要,促進儲集空間形成的成作用主要有表生期和埋藏期的溶解作用;構造作用是條件,影響著各儲集體之間以及單一儲集體內部儲集空間的連通情況。
  2. ( 4 ) based on the analysis and summary of typical orogenic belt in china, advancing the marker to distinguish the exist of delamination occurred in orogenic belt, especially giving up some new marker such as ring ultrabasic - basic - medium acid rock body, local bimodal continental rifting volcanic activity ; rapakivi granite, etc. ( 5 ) collating the main stages of south part of sanjiang orogenic belts evolution after the close of old nanchangjiang ocean, i

    較全面地提出了判別造山帶成熟拆作用發生的標志,特別是根據對我國典型造山帶的總結分析,提出了一些新的標志,如環狀超基性一基性一中酸性雜體;局部雙峰式大陸裂谷型火山活動;二長花崗、堿性花崗和奧長環斑花崗;地殼局部短暫下;等等。
  3. Sedimentary control of coalbed methane in this region were expounded according to the control and influence of sedimentation on coal gathering action ( thickness of coal reservoirs, distributing and coal - bearing characteristics ), on forming and distributing, maceral, organic facies and coalfacies, cap formation types and their sealing capability of adjoining rock

    根據積作用對聚煤作用(煤儲層的厚度、分佈及含煤性特徵) ,對煤儲層的形成與展布、煤組成、有機相和煤相、頂底板蓋層類型與封蓋性能的控制和影響,討論了積作用的控氣特徵。
  4. There are three genetic types of mineral deposits in the beiya ore district : cu - au polymetallic deposits related to alkaline porphyries, comprising porphyritic cu - au deposits and polymetallic skarn deposits related to quartz - albite porphyry and quartz - k - feldspar porphyry ; fe - au deposits related to gabbro or basalt magma, consisting of magmatic fe - au deposits and sedimentary polymetallic deposits formed in caves and lakes ; and palaeo - placers formed at the weathering surface, in lakes and in karsts

    北衙金礦有3種成因不同的礦床:與堿性斑有關的銅金多金屬礦,包括與石英鈉長斑和石英正長斑有關的斑型銅金礦床和矽卡型多金屬礦床;與輝長玄武漿有關的鐵金礦床,包括熔漿型鐵金礦床和噴流積型多金屬礦床,後者又有洞穴和湖相積環境之分;及古砂礦,有古風化殼型砂礦、河湖相古砂礦和洞穴積古砂礦。
  5. Three main rock types make up the geology of singapore : igneous, sedimentary and alluvium. where is the main source of granite found

    形成新加坡地質的三種主要石類型:火成和沖積。哪裡是花崗的主要來源地?
  6. North america has vast deposits of shale.

    北美有大量油頁積。
  7. On earth, andesites typically form when descending tectonic plates mix water into subterranean molten rock

    在地球上,安山通常是板塊的下使水混入地下熔融的石而形成。
  8. Under the circumstances, gypsum or anhydrite could accumulate to form beds many meters thick, without any co-precipitation of halite.

    在這種環境下,石膏或硬石膏可以堆積成許多米厚的層,而沒有任何石鹽伴生澱。
  9. Perhaps the future role of the sedimentary petrologist will be as an interpreter and an arbiter of cases too complex for the machine to decide unaided.

    石學家將來的作用也許是作為機械不能獨立解決復雜情況的解釋者和仲裁者。
  10. Under the guidance of theories of sedimentology, petroleum geology and sequence stratigraphy, and through the comprehensive analysis of outcropsrock, cores, well logs and testing outcomes of rock gas, this paper studies the depositional systems of neopaleozoic and the character of aeration zone in tabamiao area of ordos basin. the result indicates that the object layers are divided into two depositional systems, the barrier seacoast depositional systems are recognized on upper carboniferous taiyuan phase with tidal flat, lagoon and barrier bar sedimentary deposit

    本文根據積學、石油地質學和層序地層學理論,綜合利用地表露頭、鉆井芯、測井曲線資料和試氣成果資料,對鄂爾多斯盆地塔巴廟區塊晚古生代積體系及含氣層特徵進行了研究。結果表明,研究區內目的層段可以劃分為2個積體系: ( 1 )上石炭統太原期為有障壁海岸積體系,發育潮坪?瀉湖?障壁砂壩積。
  11. For the determination of the thickness of basaltic layers the survey area has to be extended into sedimentary area.

    為了測定玄武層的厚度,測區必須擴大到區。
  12. Even at meridiani, basaltic sands lie atop the lake sediments, indicating that the site has been parched for two billion to three billion years

    甚至在子午線地盤,玄武質的沙披覆在湖床積物上,顯示此地已經乾涸了20 ~ 30億年。
  13. The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ), micritic limestone, grainstone and micritic dolostone which were laid down in the shallow - water to bathyal, high - salinity and enclosed to semi - enclosed lake systems

    五道梁群湖相碳酸鹽分為生物粘結灰(疊層石) 、泥晶灰、顆粒灰與泥晶白雲四大類,反映出積環境為一個具有淺水半深水、高鹽度、半封閉封閉特點的綜合湖泊系統。
  14. Based on available data, the study on regional structure, sedimentary reservoir and source rock characteristics shows that the basins in south china sea had experienced sedimentary evolution in faulting period and depression period, deposited thick cenozoic formation, upwardly developed alluvial fan facies, river - lake facies coastal swamp facies coastal facies, neritic facies and bathyal deposit system, regionally had 3 source rocks of eocene, oligocene and miocene, 3 reservoirs of pre - cenozoic basement buried bill, oligocene sandstone and miocene reef, with pliocene and pleistocene neritic facies and bathyal shale as regional caprock

    摘要以現有資料為基礎,通過對區域構造、積儲層、烴源特徵等基礎石油地質條件研究,認為南海海域各盆地經歷了斷陷期和坳陷期積演化,積了巨厚的新生代地層,自下而上發育了沖積扇相、河湖相、濱岸沼澤相、濱海相、淺海相、半深海相積體系,區域上存在始新統、漸新統和中新統3套烴源,前新生代基潛山、漸新統砂、中新統生物礁3套儲層,區域蓋層為上新統和更新統淺海半深海相泥
  15. The hydrofracturing breccia is formed by deep rich - sodic and gold - hosted fluid hydrofracturing in a set of devonian system hot - water sedimentary rich - sodic rocks

    認為該水壓角礫體是深源富?含金流體在泥盆系一套熱水積的富鈉質系中發生水力壓裂作用形成的。
  16. There are typical laminated structure, soft sedimentary - slipping deformed structure, syngenetic brecciated structure in the ore which are the mirror of syngenetic sedimentation. the other type of ore has the charactristic of epigenetic mineralization, which is called as telescoped ore. the ore occurs in vein, pocket, lensoid and bedd

    礦石中發育典型的紋層狀構造、軟積滑動變形構造、同生角礫構造等反映同生積特徵的礦石構造;另一類礦石具有明顯的後生成礦特點,稱之為疊生改造型礦石,礦石產于脈狀、囊狀、透鏡狀及似層狀礦體中,與燕山期漿及斷裂裂隙構造關系密切。
  17. Calcareous sediments accumulated on a sea floor and eventually were compacted and cemented to form limestone.

    鈣質積物堆積在海底,最後壓緊並膠結形成石灰
  18. Distant effect of jurassic collisions of qiangtang terrane, lasa terrane and paleo - pacific land onto the eurasian land made east qinling - dabie mountains in a compressional circumstance for a long time, and suppressed its orogenic extension ; whereas, cretaceous late - collisional extension and appearance of west pacific trench - arc - basin system relieved east qinling - dabie mountains of external compression, instantly result in violent orogenic lithosphere delamination - extension and depressurized - calefactive melting, and consequently, led to the formation of large scale early cretaceous granitoids and intermediate - acidic volcanic rocks

    羌塘地體拉薩地體和西太平洋古陸在侏羅紀與歐亞大陸拼貼碰撞的遠距離效應使東秦嶺大別造山帶長期處于擠壓環境,伸展作用被抑制白堊紀的碰撞晚期伸展和西太平洋溝弧盆體系的遠距離效應使東秦嶺大別地區的外部擠壓消失,導致造山帶石圈迅速強烈拆伸展和減壓增溫熔融,從而形成大規模早白堊世花崗類和中酸性火山
  19. Celestite is usually diagenetic but commonly forms very early in the history of the sediment.

    天青石一般是成期的,但通常是在積史的極早期形成的。
  20. The results of the experiments indicate that : thermal plumes in the mantle ( i. e. mantle plumes ) should be divided into two types, vertical plumes, as mentioned traditionally, and non - vertical plumes, including those of inclined - columns, vortexes, etc., and the former may be only a particular case of the latter ; under the condition of the coriolis force to be ignored

    在忽略科里奧利力的情況下,板塊的下插和滯積下石圈根的存在以及地幔介質粘度的非均勻分佈等都可能構成不同形狀的障礙導流體,導致地幔的渦旋運動。
分享友人