巖片 的英文怎麼說
中文拼音 [yánpiān]-
The high - pressure metamorphic rocks in northeastern jiangxi province include such types of rocks as jadeite - bearing aegirine - augite albite amphibole schist, jadeite - bearing aegirine - augite quartz albitite, aegirine - augite - bearing amphibole quartz albitite, aegirine - augite - bearing albite amphibole schist, winchite quartz albitite, and magnesio - riebeckite quartz albitite
摘要贛東北高壓變質巖包括含硬玉霓輝石鈉長角閃片巖、含硬玉霓輝石石英納長石巖、含霓輝石角長閃石英鈉長石巖、含霓輝石鈉長角閃片巖、藍透閃石石英鈉長石巖、鎂鈉閃石石英鈉長石巖等巖石類型。Amphibole - cholrite schist
閃綠泥片巖Based on the 1 : 50000 regional geological survey, the sertengshan rock group is revised, involving the schist and marble of low - amphibolite to high - greenschist facies, which are distributed in middle and west inner mongolia
摘要根據近年完成的1 : 5萬區域地質調查成果及綜合研究，將分佈於內蒙古中部色爾騰山、大青山、西部烏拉特后旗以及阿拉坦敖包、疊布斯格等地的低角閃巖相高綠片巖相的片巖、大理巖系釐定為色爾騰山巖群。Based on the studies of petrotexture, structural deformation and the relevant metamorphism, this paper indicates that this peridotite massif is the product of ultramafic magma cumulated at the crust - mantle transtion zone and has undergone the early stage of plastic deformation under the condition of granulite facies （ 800 ） and late ductile shearing at amphibolite and greenschist facies in relevance to uplifting
本文通過巖體的結構、構造變形及相應的變質作用研究，提出了該橄欖巖體是由超基性巖漿在殼幔過渡帶結晶而成，並經歷了與圍巖一致的麻粒巖相（ 800 ）條件下的早期塑性變形以及角閃巖相和綠片巖相退化變質條件下與逆沖上升有關的韌性剪切變形。Detail mapping shows that the yagan mcc consists of crystallized metamorphic core ( low plate ), detachment zone and upper plate. the metamorphic core consists of can be further subdivided into two level parts low - level high metamorphic and upper - level shallow metamorphic structural slice and between them there exists a ductile shear zone. thus the whole texture of the mcc is characterized by " three layers and tow zones " this reveals a process of extensional uplift of poly - level slices by poly ductile shear zones, a characteristics of poly - level extensional structural systems. the deformational environments change vertically in a sequence of high amphibolite facies
亞干變質核雜巖由下盤結晶巖系變質核、拆離帶和上盤巖系構成，其中，變質核由四個單位及許多花崗巖體（脈）組成，可進一步分為中深和中淺變質兩個構造單位（巖片） ，之間發育次級韌性拆離帶（花崗質糜棱巖帶） ，加上上盤總體構成「三層兩帶」的結構特點。Andalusite - mica schist
紅柱雲片巖Its applicability might be questioned on the grounds that carbonaceous shale is not known to occur near any of these deposits.
其實用性是有疑問的，因為還不知道在上述礦床附近存在著碳質片巖。The nickel mineralization is contained in a layered basic mass if surrounded and underlain by an archean gneiss complex.
此處鎳礦化產於一層狀基性巖塊內，其四周和下面都為太古代片麻巖雜巖圍繞。Isua ' s four - kilometer - wide belt of archean rocks stretches 35 kilometers along the western edge of the bluish - gray monolith of the greenland ice cap
這片礦藏可不好找，它是四公里寬的太古代巖層，沿著藍灰色格陵蘭冰帽硬塊的西緣延伸35公里。It was followed by the swift flashes of the rifles, which sent their leaden messenger across the rock in volleys, as though the assailants would pour out their impotent fury on the insensible scene of the fatal contest.
緊接著，火光閃閃，槍彈越過雙方之間的巖石，成排地飛射過來，彷彿他們要把自己無可奈何的憤怒，全都發泄在進行這場殊死搏鬥的這片無知無覺的土地上似的。The minerals are disseminated in the schist and hornfelsed schist near the dolerite contact.
這些礦物也浸染在靠近粗玄巖接觸帶的片巖和角巖片巖中。The ultrabasic rocks form a complex of large tectonic slices with intercalated slices of sebakwian sedimentary rocks.
超基性巖與塞巴奎沉積巖巖片相間構成一巨大的構造巖片的雜巖體。The coqen basin in xizang lies between the bangong - nujiang suture zone and yarlung zangbo suture zone, and once extended northwards and southwards, respectively centred by the qiekan - goicang - asog rift zone as the center of deposition and subsidence during the middle jurassic to the early creatceous. ( 1 ) during the middle - late jurassic, the rift zone was occupied by deep - water turbidites, radiolarian siliceous rocks, shallow - water carbonate rocks, clastic rocks and basic - ultrabasic rocks, while both sides of it by littoral and shallow marine elastic rocks and carbonate rocks
摘要位於班公湖怒江縫合帶與雅魯藏布江縫合帶之間的措勤盆地，在中侏羅世早白堊世期間具有以且坎古昌阿索裂谷帶為沉積、沉降中心向南北兩側展開的古地理格局：中晚侏羅世時期，裂谷帶內由深水濁積巖、放射蟲硅質巖和淺水碳酸鹽巖、碎屑巖巖片及基性超基性巖等組成；裂谷帶兩側由濱淺海相碎屑巖和碳酸鹽巖組成。( 3 ) ensemble character of structural planes as follows : in left dam abutment, meta basalt schistosity is main, and the structure is clockwise. low dip angle jointing did n ' t develop in rock mass ; in right dam abutment, rupture and jointing structural plane is main, and the structure is reversed. the structure was of obvious macroscopical slaty character
（ 3 ）通過對上述結構面的分析，得出其總體特徵為：左壩肩以變玄武巖片理為主體，呈順向結構，巖體內緩傾角節理極不發育；右壩肩主要為斷裂及節理型結構面，呈反向結構，且具有明顯的宏觀板狀結構特徵，並發育有一定厚度的構造軟巖帶。The rock slices are truncated by the pre-bulawayan erosion surface.
巖片受前布拉瓦約侵蝕面切割。Camp belong to the south qinling orogenic belt middle segment palaeozoic strench basin fold indo - chinese epoch drape north part, and belong to the miliangchuan schiefer
礦區所在部位屬南秦嶺造山帶中帶古生代伸展盆地疊加印支期沖褶帶的北部，隸屬于米糧川逆沖巖片。The pre - jurassic basement of hefei basin was composed of thrusts. indosinian foreland thrusts in pre - jurassic bedrocks of the basin increase towards the tan - lu fault zone, indicating indosinian activity of the fault zone
合肥盆地在印支期的前侏羅紀基底主要表現為大別造山帶前陸逆沖推覆構造，由一系列逆沖斷層和逆沖巖片所組成。In order to explain the spatial and temporal distribution of volcanic rocks with different ages and tectonic regimes, one archipelagic model is proposed. the shizong - mile zone in se yunnan was composed of different tectonic blocks with different ages, lithological features and provenances, and contacted each other by a shear zone
滇東南師宗彌勒帶主要以一系列逆沖斷層為骨架，剪切包容古生界、少量三疊系和元古界地層的構造巖塊、以及火山巖構造巖片，共同構成一個由多條斷層控制不同時代、不同性質構造巖塊的混雜帶。The sedimentary rock formations lying across the island is uncommon in hong kong, and has earned tung ping chau a listing as one of the seven wonders of hong kong
島上顏色赤紅的粉砂巖，片片交疊灘頭，以特有的自然景貌及奇巖怪石，被稱為香港七大奇景。Underneath the surface was a layer of sedimentary yellow soil, which was regarded as coming from somewhere else. it was found that some of the rock materials was the same as on the walkway, which shows that this soil layer had some connections with the the reforming of the pedestrian walkway
表土層底下露出黃褐色堆積土層，屬外來堆土，其中還發現幾片與地表人行步道上的板巖片相同材質的遺留，顯示該土層應與整修人行步道有關。分享友人