甘巖 的英文怎麼說
中文拼音 [gānyán]
甘巖
英文
ka'ngai-
In view of the natural conditions in loess area of gansu, in the light of investigation conditions of seepage of built loess and weak rock highway tunnels in this area and classification of water gushing conditions for railway tunnels, and by engineering analogism, the classification of tunnel water gushing types suited the structure design of highway tunnel waterproof and drainage, and the three methods for checking and subdividing water gushing types are presented
摘要針對甘肅黃土區的自然條件，依據該地區已建黃土及軟巖公路隧道滲漏水調查情況和鐵路隨道涌水狀態分類，運用工程類比法提出適合該地區公路隧道防排水結構設計的隧道涌水類型劃分及對涌水類型校核與細分的三種方法。The yanchang formation of upper triassic in north shaanxi is major terrigenous clastic system deposited in fluvial - latchstring environment, under the influence of the llocyclicity factor which include indosinian tectonic, eustacy, sedimentary supplies and the autocyclicity factor. in late triassic, north shaanxi was divided into two parts bounded by zhidan - ganquan - yichuan demarcation line
陜北地區上三疊統延長組是以河流一湖泊相為特徵的陸源碎屑巖系，當時的陜北地區，以志丹?甘泉?宜川沿線為界，南側以明顯的斜坡向深湖盆地過渡，北部則為一地形平緩的淺水臺地。The quaternary system is characterized by high geothermal gradient, with low scope of overpressure in its deep and shale caprock saturated with formation water of high salinity
第四系具有較高的地溫梯度，深部發育了低幅超壓；甘森泉小柴旦基底斷裂影響氣藏構造的完整性；第四系飽含高礦化度地層水泥巖構成的蓋層可以起到一定的封蓋作用。The research of large igneous rock province - ermei basalt extrusion - mantle plume shows that songpan - ganzi folded belt is a hopeful target for breakthrough of petroleum exploration, and the key issue is how to make well a coupling and optimization among its faults, structures, traps and reservoirs
根據地震測深、重、磁、電等的探查，發現該褶皺帶深部有一低速高導層，而對大火成巖省峨眉玄武巖噴溢地幔柱的認識深化均表明，四川松潘甘孜褶皺帶是可望獲得油氣勘探突破的靶區，重要的是斷裂構造、圈閉、儲集層的耦合與優化。Metamorphic history of eclogites from beishan, gansu province
甘肅北山榴輝巖的變質歷史Geochemical characteristics and significance of triassic sandstones of songpan - ganze block
甘孜地塊三疊系砂巖的地球化學特徵及其意義There are plentiful mineral resources of nickel, cobalt, and copper in the northwest region of china, specially jinchuan superlarge copper - nickel sulflde magmatic deposit in gansu province, known for its large scale and typical metallogenetic feature in the world, is an important source of ni - cu metal mineral resource in our country. in contrast, jianchaling large cobalt - bearing nickel sulflde deposit in shannxi province is not famous and unmined, but many problems about the deposit are researched because of its special geologic settings and mineralization characteristic
我國西北地區有著豐富的鎳、鈷、銅等金屬的礦產資源，尤其是甘肅省金川超大型銅鎳硫化物巖漿礦床，以其超大規模及其典型的成礦特徵而聞名於世，是我國重要的鎳、銅金屬礦產基地，而相比之下，陜西省煎茶嶺大型鎳（鈷）礦床規模較小且未開采，但因其獨特的地質背景和成礦特徵而具有重要的研究意義。The representative scenic spots are : sunrise at tiantai platform, evening bell of huacheng temple, sitting on east stone with pleasure, fairy mark of tianzhu, taoyan waterfall, clouds around lotus peak, snow at pinggang, moon reflected in shu pond, sound of jiuzhi spring, mountains at five streams, longchi waterfall, bamboos in minyuan garden, ganlu temple, mokong palace, flowers at hua platform, lion peaks, blue valley, fish - and - dragon cave, and phoenix pine
九華山山水風景最著者，舊志載有九華十景：天臺曉日化城晚鐘東崖晏坐天柱仙蹤桃巖瀑布蓮峰雲海平崗積雪舒潭印月九子泉聲五溪山色。此外，還有池飛瀑閔園竹海甘露靈秀摩空梵宮花臺錦簇獅子峰林青溝探幽魚洞府鳳凰古松等名勝。Abstract : yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure
文摘:陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲油田，儲集層主要為三角洲砂體，壓實作用和膠結作用強烈，儲層非均質性非常嚴重，因此預測次生孔隙發育帶是尋找油氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析，認為陜甘寧盆地延長統次生孔隙的形成除了受沉積有利相帶控制外，還與地層異常壓力的作用密切相關.研究認為隴東地區異常壓力的形成機理主要由於成巖過程中粘土礦物脫水作用.粘土礦物大量脫水時間正好與有機質脫羧期相一致，從而在異常壓力作用下將生油巖中的大量有機酸及co2帶到與之相鄰的儲集層中，並沿著有利儲集相帶運移，在酸性水經過的地方形成大量的次生孔隙，為後期油氣運聚提供有利通道及宿住空間，從現今的勘探結果來看，通過研究地層異常壓力縱橫向分佈特徵，並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法Yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure
陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲油田，儲集層主要為三角洲砂體，壓實作用和膠結作用強烈，儲層非均質性非常嚴重，因此預測次生孔隙發育帶是尋找油氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析，認為陜甘寧盆地延長統次生孔隙的形成除了受沉積有利相帶控制外，還與地層異常壓力的作用密切相關.研究認為隴東地區異常壓力的形成機理主要由於成巖過程中粘土礦物脫水作用.粘土礦物大量脫水時間正好與有機質脫羧期相一致，從而在異常壓力作用下將生油巖中的大量有機酸及co2帶到與之相鄰的儲集層中，並沿著有利儲集相帶運移，在酸性水經過的地方形成大量的次生孔隙，為後期油氣運聚提供有利通道及宿住空間，從現今的勘探結果來看，通過研究地層異常壓力縱橫向分佈特徵，並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法Characteristics of early cretaceous prototype basin and its control on source rock in mongolia - gansu - qinghai area
蒙甘青地區早白堊世原型盆地特徵及其對烴源巖分佈的控制Throughout researching it has been found that three main types of copper deposits, which mafic - ultramafic rock, marine volcanic rock and porphyry, with middle proterozoic, paleozoic and mesozoic in gansu, china. the cu - bearing formation, deep major faults and late structural - magmatic zones formed in specific geotectonic setting are main ore - controlling and metallogenic factors for copper, gold and polymetallic minerals in this area, and their convergent positions are effective ones formed ore bodies in space
通過研究認為：鎂鐵質-超鎂鐵質巖型、海相火山巖型及斑巖型三種銅礦類型，是甘肅的主要銅成礦類型，其主成礦階段為中元古代、古生代以及中生代；特定大地構造背景下形成的含礦建造、區域性深大斷裂以及後期斜向構造-巖漿活動帶，是該區銅、金及多金屬成礦的主要控礦因素，三者在空間上的復合是礦床體形成的有利部位。Geochemical constraint on the origin and sources of early - middle cambrain acidic volcanic rocks from baiyin ore deposit
甘肅白銀廠礦田早中寒武世酸性火山巖成因及源區特徵的地球化學制約Mount wuyi luxury hotel with the most unique style luxury performing arts hall, advanced lighting audio equipment to visual and hearing you enjoy unlimited surprises ; input type comments to the tea room operated with the special rock music back to wuyi opposed gan, away from the tired eyes, small goods and leisure life rare pleasure
酒店內有武夷山高檔風格最獨特的豪華演藝大廳，先進的燈光音響設備，帶給您無限驚喜的視覺和聽覺享受投入清雅嫻致的茶藝棋牌室，隨著武夷巖茶特殊的巖韻回甘，遠離俗世的喧囂，細品人生難得的閑適與愉悅。The north - eastern structural zones which become intensity from the western part to the eastern one in gansu show a influence of marginal - west pacific indosinian - yanshan tectonic - magmatic belt on the western part of china ' s continent, and not only a important regional metallization had developed but also early - formed minerals were intense changed and enriched with the tectonic - magmatic activity
甘肅境內由西向東增強的北東向構造帶，是我國東部濱西太平洋印支-燕山期構造巖漿活動帶向大陸西部的延伸表現；伴隨該期構造-巖漿活動，區內發生了重要的區域性成礦作用，並使處于該期構造活動帶的先期金屬礦產遭受了較強的疊加與再生改造。3 ) according to the dayi conglomerate " s gravel composition and direction when water flowed during geological age, comeback the paleogeograph of the longmenshan foreland basin, speculates that the dayi conglomerate " material source is located in the songpan - ganzi fold belt to the east, the pengguan fault to the west of the western sichuan plateau region
3 ）根據大邑礫巖礫石成分及古流向分析，推測大邑礫巖物源區為松潘-甘孜褶皺帶以東、彭灌斷裂以西的龍門山地區，並恢復大邑礫巖沉積時期巖相古地理，認為大邑礫巖物源主要來自龍門山沖斷帶一側。It is very important that the understanding of regional metallogenic rules should be emphasized and the thinking of exploration and research opened up. in this thesis, mainly metallogenic types, tectonic setting, space - time distributions and the ore - controlling and metallogenic conditions for copper ore deposits in gansu province are studied on based inducing past formation which basic theories and methods of the modern geology, mineral deposits and related learning are applied and a serious of formation synthesized throughout depending on guide of regional. - metallogenic theories. a rule of development, enrichment and regional metallogeny would be preliminary summaries in terms of analyzing mineral prospecting for gansu ' s copper, gold and polymetallic minerals, and the relation between the indosinian - yanshan structural - magmatic activities is studied and exploration prospect and positions analyzed as well as a new countermeasure and thinking about research for minerals in this area be suggested
本論文在總結、分析前人成果資料基礎上，以區域成礦學理論為指導，運用現代地質學、礦床學及相關專業、學科的基本理論與方法，綜合多種成礦信息，對甘肅省銅礦主要成礦類型及其成礦地質構造背景、時空分佈特徵與主要控（成）礦條件進行了研究；從礦產勘查的角度，初步總結了甘肅銅、金及多金屬礦產的發育、富集與區域成礦規律；探討了印支-燕山期構造-巖漿活動與大型-超大型銅礦床的形成關系；研究分析了甘肅銅礦資源的勘查前景與找礦方向，提出了該區礦產勘查研究新思路。Rise amid ups and downs, xiongqi style, forest green, hotel towering ; there are holes rock, rock qiao unseen wall, a stone - chuen, a quan warms
峰巒起伏，雄奇秀拔，林木青翠，古榕參天；有巖有洞，巖幽壁峭，有石有泉，出泉甘冽。Crude asp has two components, the molecular weight of component 1 was 67600. it was composed of glucose, mannose, galactose and fructose, as well as trace fucose and xylose
黃芪粗多糖由2種組分組成，組分（ aps1 ）分子量為67600 ，紙色譜表明主要由葡萄糖組成，氣相色譜顯示還有甘露糖、半乳糖、果糖、木糖和巖藻糖。Characters of mesozoic stratum in gongpo spring basin and analyses about the uranium mine condition of the type of sandstone of beishan in ganshu
甘肅北山公婆泉盆地中生代地層特徵與砂巖型鈾成礦條件分析分享友人