馬山巖 的英文怎麼說
中文拼音 [mǎshānyán]
馬山巖
英文
masanite-
Long term immersing marshall test and frozen - thaw cycle test were used to investigate the anti - stripping performance of andesite asphalt mixture using cement and anti - stripping agent
摘要採取長時間浸水馬歇爾試驗和多循環凍融劈裂試驗方法，對摻加了水泥、抗剝落劑的安山巖集料瀝青混凝土水穩定性能進行研究。Laiwu hydrothermal metasomatic iron deposit is located at contact zone of ordovician carbon - ate rock ( majiagou formation ) and late yanshanian diorite or nearby
摘要萊蕪接觸交代熱液鐵礦賦存於奧陶系馬家溝組碳酸鹽巖與燕山晚期閃長巖的接觸帶及其附近。B87c breaker is a pneumatic instrument manufactured with the mature technology of america gardener denver corporation. it is more powerful in breaking ferroconcrete, rocks and asphalt. boasting greater efficiency and durability, it suits the requirements of breaking outsized, super - thick and hard objects. it is ideal machinery for the substructural construction of mines, bridges, roads and civil infrastructure
B87c破碎機採用美國迦納德?丹佛氣動集團公司成熟技術，是以壓縮空氣為動力的破碎工具，能高效完成鋼筋混凝土、巖石、瀝青等破碎工作，具有馬力更大、效率更高、壽命更長等特點，特別適宜對特大、特厚、特堅硬物體的破碎作業，是礦山、橋梁、道路、市政建設等基礎工程施工的理想工具。And apatite. by these analyses and comparison with general granite both in china and the world and with the granite in other au or cu belt in china, the characteristics of the granite in this area are concluded as follows. it belongs to magnetite - i or syntectic granite and has crust - mantle mixed characteristics ; it was formed mainly by crystallization differentiation of melting magma and multiphase varied intrusion ; the degree of differentiation evolvement is not high ; the granite and its enclaves p. re congenetic ; the range of temperature is about 500 - 700, the range of pressure is about 2. 50 gpa - 4. 35 gpa, and the range of oxygen fugacity ( lg fo2 ) is - 15. 53 - - 14. 00 ; most granite bodies formed before the collision of plates, and few formed after the collision of plates
通過對測試數據的分析與綜合研究，並同中國和世界一般花崗巖類以及中國主要金、銅成礦巖體的花崗巖類進行對比，得出本區花崗巖類巖石具有以下特徵：屬磁鐵礦-型或同熔型花崗巖，其巖漿物質具殼幔混源特徵：主要由熔融態巖漿經結晶分異作用，通過多期變速上侵而形成；其分異演化程度較低；寄主巖基和包體具有同源性；巖石的形成溫度范圍約為500 - 700 ，壓力大約為2 . 50gpa - 4 . 35gpa ，氧逸度值1gfo _ 2為- 15 . 53 ? 14 . 00 ；該巖帶主要形成於板塊碰撞前消減的活動板塊邊緣期，為燕山至喜馬拉雅早期的大陸邊緣火山弧環境的產物。Millions of years ago, metamorphic schists, gneisses and quartzites formed impressive, flat - topped inselbergs on a vast plain in the shadow of kilimanjaro
百萬年前，變質的石板片麻巖和石英巖，在乞力馬札羅山附近廣闊的平原形成壯觀島嶼似的The romans discovered that a mixture of quicklime, volcanic ash and aggregate would harden under water - the roman cement or hydraulic lime was born
生石灰，火山巖灰燼和其它混合物在水的作用下會變硬的特性由此羅馬水泥或水化石灰就誕生了。2. 38. 6ma and 36. 7ma isotopic ages of quartz - monzonite - porphyry in lianhuashan and alkaline porphyry in zhuopan have respectively been obtained. those results are consistent with the ages of the porphyries in both lanping - shimao basin and changdu basin related igneous rocks, representing the first episode ( lanping movement ) of tectonics - magmatism - metallogenic event during the himalayan movement
獲得了蓮花山石英二長斑巖及卓潘堿性斑巖的ar - ar年齡，分別為38 . 6ma與36 . 7ma ，與整個蘭坪?思茅盆地與昌都盆地及兩側的斑巖與相關火山巖一致，代表喜馬拉雅運動第一幕（蘭坪運動）的重要構造?巖漿?成礦事件。" we ' re going to call him volcano, " said mungo, 37, sitting in a hospital bed in goma next to the baby swaddled in a pink and white chequered blanket
上周，剛果金戈馬城附近的火山爆發，熾熱的熔巖幾乎摧毀了這個依山傍湖的城市。Like an estimated 300, 000 other residents, mungo fled across the border from goma to the town of gisenyi in neighbouring rwanda when rivers of lava bulldozed through much of the city last thursday
上周四，剛果金境內尼拉貢戈火山開始大規模噴發，熔巖來勢洶洶，穿過戈馬城的大部分地區。Cancelled kr41 beacon heights - somerset road, kowloon tong kr42 beacon heights - wai chi street, shek kip mei hr36 ap lei chau san shi street - causeway bay pak sha road refer to gmb 36x hr41 pok fu lam gardens - wan chai cancelled hr42 baguio villas lower - edinburgh place hr43 baguio villas upper - edinburgh place hr44 no. 57 - 61 south bay road - repulse bay hr45 hk parkview - edinburgh place hr46 hong kong parkview - wan chai hr48 repulse bay - central circular hr49 robinson heights - central circular hr50 no. 57 - 61 south bay road - edinburgh place hr51 beverly hill - causeway bay circular hr53 pacific view - edinburgh place hr54 dynasty court - edinburgh place hr55 dynasty court - wan chai circular hr56 grand panorama - central circular hr57 redhill peninsula - stanley hr58 redhill peninsula - shau kei wan mtr station hr59 redhill peninsula - central hr60 repulse bay road - causeway bay hr61 conduit road skyview cliff - central hr62 conduit road realty gardens - central admiralty hr63 a kung ngam village - shau kei wan mtr station circular hr64 conduit road imperial court - admiralty tamar street hr65 seymore road goldwin heights - central queen s pier hr66 tregunter path branksome - central connaught place circular hr67 old peak road hillsborough court - central queen s pier hr68 garden terrace - admiralty mtr station drake street hr69 magazine gap road harbourview - admiralty tamar street circular hr70 kennedy road bamboo grove - central ice house street circular hr71 old peak road tregunter - central queen s pier circular hr72 old peak road tregunter - admiralty tamar street circular hr73 conduit road pearl garden - admiralty circular hr74 no. 150 kennedy road - central queen s pier hr75 pokfield road university heights - sheung wan shun tak centre circular hr76 may road the mayfair - admiralty drake street circular hr77 may road clovelly court - central queen s pier circular
（已取消） hr42下碧瑤灣- -愛丁堡廣場hr43上碧瑤灣- -愛丁堡廣場hr44南灣道57 - 61號- -淺水灣hr45陽明山莊- -愛丁堡廣場hr46陽明山莊- -灣仔hr48淺水灣- -中環（循環線） hr49樂信臺- -中環（循環線） hr50南灣道57 - 61號- -愛丁堡廣場hr51比華利山- -銅鑼灣（循環線） hr53浪琴園- -愛丁堡廣場hr54帝景園- -愛丁堡廣場hr55帝景園- -灣仔（循環線） hr56嘉兆臺- -中環（循環線） hr57紅山半島- -赤柱hr58紅山半島- -筲箕灣地鐵站hr59紅山半島- -中環hr60淺水灣道- -銅鑼灣hr61干德道（華庭閣） - -中環hr62干德道（聯邦花園） - -中環/金鐘hr63亞公巖村- -筲箕灣地鐵站（循環線） hr64干德道（帝豪閣） - -金鐘（添馬街） hr65西摩道（高雲臺） - -中環（皇后碼頭） hr66地利根德里（蘭心閣） - -中環（康樂商場） （循環線） hr67舊山頂道（曉峰閣） - -中環（皇后碼頭） hr68舊山頂道（花園臺） - -金鐘（德立街） hr69馬己仙峽道（港景別墅） - -金鐘（添馬街） （循環線） hr70堅尼地道（竹林苑） - -中環（雪廠街） （循環線） hr71舊山頂道（地利根德閣） - -中環（皇后碼頭） （循環線） hr72舊山頂道（地利根德閣） - -金鐘（添馬街） （循環線） hr73干德道（明珠臺） - -金鐘（循環線） hr74堅尼地道150號- -中環（皇后碼頭） hr75蒲飛路（翰林軒） - -上環（信德中心） （循環線） hr76梅道一號- -金鐘（德立街） （循環線） hr77梅道（嘉富麗苑） - -中環（皇后碼頭） （循環線）Sediments from this period are represented by the carboniferous marble of yuen long and ma on shan. the sandy and muddy sediments of the permain rocks of tolo harbour are of alternate marine and continental deposits
巖土其後遭淺海淹沒，沉積物不斷積聚，元朗和馬鞍山的石炭紀大理巖，便是這個時候的產物。分佈於吐露港的二疊紀砂巖和泥質巖，則屬海陸交互沉積而成。To evaluate the mine engineering geological conditions and for making - up an engineering activity plan that guides the mine development, an engineering geological environmental analysis of aoshan mining area in nanshan mine, maanshan iron and steel co. was made. through rock property analysis, single factor analysis and comprehensive evaluation, the coordinability of various factors were determined
為評價礦山工程地質狀況，指導礦山開發的工程活動規劃，開展了馬鋼南山礦凹山礦區的工程地質環境分析，通過巖性分析、單因素分析及綜合評價，得出各因素的可協調性結果。Tarbarrels and bonfires were lighted along the coastline of the four seas on the summits of the hill of howth, three rock mountain, sugar - loaf, bray head, the mountains of mourne, the galtees, the ox and donegal and sperrin peaks, the nagles and the bograghs, the connemara hills, the reeks of m gillicuddy, slieve aughty, slieve bernagh and slieve bloom
柏油桶和篝火沿著四海625的海岸，在霍斯山三巖山糖錐山626布萊岬角莫恩山加爾蒂山脈627牛山多尼戈爾斯佩林山嶺納格爾和博格拉628康尼馬拉山麥吉利卡迪629的霧靄奧蒂山貝爾納山和布盧姆山630燃起。3. it was rocky hills and relatively high in the yangtze river mouth area along changzhou, wuxi, changshu, kunshan and qingpu, which belonged to changzhou - kunshan zone according to holocene delimitation from the final stage of the liangzhu culture to the stage of the maqiao culture, due to the expansion of taihu basin and large water areas, maqioa cultural sites were concentrated on rocky hills and cheniersin the east of taihu to the west of shanghai
3 、蘇南常州、無錫、常熟、崑山和青浦一帶曾經是長江河口地區的基巖山地，在全新統地層分區上屬于常州一崑山區，是古地面地勢相對較高的地方。良渚文化末期至馬橋文化期，為太湖湖盆體系擴大時期，水域較大，所以馬橋文化遺址集中於太湖東部與上海西部地勢較高的基巖山地和砂堤之上。Then proceed to the unique beauty of mont st. michel, which stands on an island reached by a causeway. the crowning glory of mont st. michel is its abbey, which seems to be hanging in mid0air on the side of the rock
午後來到海上巖島聖米歌爾山，在常年海霧迷漫的山頂上，巍然矗立一座結合羅馬式和哥德式建築精華的古世紀修道院，許多遊客專程前來朝聖。There are innumerable sheer precipices and overhanging rocks in danyun gorge : stone horse pass, kuanyin rock, zou kong rock and the squating cat, standing facing each other
石馬關觀音巖灶孔巖貓兒蹲雄踞對峙滴水凌冰瀑飛流直下，綿延18公里的深山峽谷蔚為險峻壯觀。During this evolution, seven second - order tectonic units were formed ; from north to south are the mingqianri cretaceous residual sea basin, the arsuo tectonic melange zone, the taricuo - wenbu yenshan magmatic arc belt, the cuoqin - bangduo late paleozoic composite back - arc basin, the jiangrang - geerdi faulted uplift, the gangdise - chazi himalayan magmatic arc belt, and the xigaze - anba fore - arc basin. these units comprise important parts of a poly - arc - basin system and exhibit evolutional features of mesozoic to cenozoic arc - basin systems. mosaic pattern of these tectonic units delineates the lithosphere coupling processes of the gangdise tectonic belt under mechanisms such as back - arc basin attenuation and arc - continent collision
自中新生代以來，岡底斯構造帶經歷了洋殼俯沖、弧陸碰撞、陸內俯沖-碰撞、走滑和塊段隆升的多階段構造演化歷程，形成了由北向南七個二級構造單元，即岷千日白堊紀殘余海盆、阿索構造混雜巖帶、它日錯?文部燕山期巖漿弧帶、措勤?幫多晚古生代復合弧后盆地、江讓?格爾耿斷隆、岡底斯?查孜喜馬拉雅期巖漿弧帶、日喀則?安巴弧前盆地。The study of geological characteristics and geochemical conditions of mazhuangshan gold deposit shows that it is closely related with old metamorphic basement and volcano - magmatic activities as well as volcanics and volcaniclastics of mazhuangshan - mingshui superimposed volcanic basin, and controlled by structures derived from closure of late palaeozoic honghe basin
摘要對馬莊山金礦地質特徵及地球化學條件研究表明，馬莊山金礦的形成與古老變質基底、火山巖漿活動及馬莊山一明水上疊火山巖盆地的火山巖、火山碎屑巖緊密相關，並受到晚古生代紅河盆地閉合而派生的構造控制。The jinan spring catchment is a complicated karst water system, the following major work had been done in order to discuss the proplem of spring protection and water supply. 1. having conduced exploration, experiment and comprehensive research, the southern boundary of the jinan spring catchment is determined to be the surface water divide ( changecheng mountain ), the source of yufu river and baedasha river ; the northern one is the carbonniferous and permian strata, together with the igneous rock mass in the north of jinan, and the eastern and the western ones are dongwu and mashan faults respectively, which are weakly permeable boundaries. the total area of the spring catchment is 1486 km2
濟南泉域為一復雜的巖溶水系統，為了探討保泉供水問題，主要做了以下工作： （一）經過勘查、試驗和綜合研究確定濟南泉域邊界是：南邊界為玉符河、北大沙河源頭的地表水分水嶺（即長城嶺） ；北邊界為濟南北部的石炭、二迭系煤系地層和巖漿巖體；東、西兩側分別以弱透水的濟南東部的東塢斷裂和西部的馬山斷裂為邊界。It is proposed that there are promising areas including tashilazi - wendilou, xiaotazi - madaigou, daqingshan - yingbishan for volcanic type gold deposit through the study of ore - forming geological conditions, deposit characters and prospecting indications
研究了該區火山巖型金礦的成礦地質條件，礦床特徵和找礦標志，提出了紅石砬子?溫滴樓、小塔子?馬岱溝、大青山?影壁山等找火山巖型金礦有望地區。分享友人