basaltic adj.(含)玄武巖的，似玄武巖的。
adj. (含)玄武巖的，似玄武巖的。 “basaltic achondrite“ 中文翻譯： 玄武質無球粒隕石“basaltic andesite“ 中文翻譯： 玄武安山巖“basaltic augite“ 中文翻譯： 玄武輝石“basaltic blister“ 中文翻譯： 玄武巖皰“basaltic clay“ 中文翻譯： 玄武質粘土“basaltic crust“ 中文翻譯： 玄武巖殼“basaltic dome“ 中文翻譯： 盾狀火山; 玄武巖丘“basaltic flow“ 中文翻譯： 玄武巖流“basaltic form“ 中文翻譯： 玄武巖狀; 柱狀“basaltic glass“ 中文翻譯： 玄武玻璃“basaltic hornblende“ 中文翻譯： 玄閃石; 玄武角閃石; 玄武閃石; 玄武巖角閃石“basaltic jointing“ 中文翻譯： 玄武巖節理“basaltic lava“ 中文翻譯： 玄武熔巖; 玄武質熔巖; 玄武質熔質“basaltic layer“ 中文翻譯： 玄武巖層“basaltic magma“ 中文翻譯： 玄武巖漿; 玄武質巖漿“basaltic melt“ 中文翻譯： 玄武質熔漿“basaltic neck“ 中文翻譯： 玄武巖頸“basaltic nephlinites“ 中文翻譯： 玄武質霞巖“basaltic parting“ 中文翻譯： 玄武巖節理“basaltic rock“ 中文翻譯： 玄武質巖石“basaltic rocks“ 中文翻譯： 玄武巖類“basaltic shell“ 中文翻譯： 玄武巖殼; 玄武巖圈“basaltic soil“ 中文翻譯： 玄武巖土壤“basaltic stratum“ 中文翻譯： 玄武巖層“basalteclogitetra formation“ 中文翻譯： 玄武巖榴輝巖轉化“basaltic achondrite best initial“ 中文翻譯： 玄武質無球粒隕石最佳初始比值
The control of the deep - seated structural - magmatic process over the metallogenic system around the middle - lower yangtze river reaches is shown as : ( 1 ) the mantle uplift belt is closely related to the general geological background of the metallogenic system ; ( 2 ) the primitive magma originated from different parts of the mantle uplift belt ( mantle ridge or mantle slope ) shows differences in style of formation and composition and results in different magmatic series and metallogenic subzones , respectively ; ( 3 ) the varying depths of structural - magmatic chambers may form a “ three - layered structure “ ( central type , network - like and ring - like ) and this is the primary factor that controls the different magmatic series and the concerned cluster of ore deposits ; ( 4 ) the alkaline basaltic magma derived from the mantle ridge forms high - potassium and calcium alkaline magma and shoshonitic magma due to its altering intensity of afc process with the lower crustal material , which has something to do with the copper - gold and iron - sulphur metallogenic subsystems , respectively 深部構造巖漿作用對長江中下游成礦帶安徽沿江地區成礦系統的控制表現為： ( 1 )地幔隆起帶與成礦系統的總體地質背景的演變密切相關； ( 2 )源于地幔隆起帶不同部位(幔脊與幔坡)的原始巖漿，其生成方式和物質組成不盡相同，它們分別產生相應的不同巖漿巖系列和成礦亞帶； ( 3 )不同深度的構造巖漿房組成中心式網格式環帶式“三層結構” ，是控制區內不同巖漿巖系列及有關礦床集中分布的主要因素； ( 4 )源于地幔隆起帶脊部的堿性玄武巖漿，由于與下地殼物質發生的afc作用強度不同，形成了高鉀鈣堿性巖漿和橄欖安粗巖漿，分別與銅、金成礦亞系統和鐵、硫成礦亞系統有關。 |
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basan |
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An article of headgear since ascertained to belong to the much respected clerk of the crown and peace mr george fottrell and a silk umbrella with gold handle with the engraved initials , coat of arms and house number of the erudite and worshipful chairman of quarter sessions sir frederick falkiner , recorder of dublin , have been discovered by search parties in remote parts of the island , respectively , the former on the third basaltic ridge of the giant s causeway , the latter embedded to the extent of one foot three inches in the sandy beach of holeopen bay near the old head of kinsale 搜查隊在本島的偏僻地區發現了一頂帽子，已查明系屬于那位備受尊重的法庭書記喬治弗特里爾640先生還有一把綢面雨傘金柄上鐫刻著都柏林市記錄法官641博學可敬的季審法院院長弗雷德里克福基納爵士姓名的首字盾形紋章以及住宅號碼。也就是說，前者位于巨人堤道642第三玄武巖埂上后者埋在古老的金塞爾海岬643附近霍爾奧彭灣的沙灘深達一英尺三英寸的地方。 |
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2 . early jurassic mafic volcanic rocks in yanshan area were derived from decompression melting of an ancient continental lithospheric mantle , which had been previously metasomatized by subducted slabs during the closure of paleo - asian ocean ; the mantle source of late jurassic mafic volcanic rocks were contributed by dominant emi and insignificant subducted metasomatic components ; early cretaceous mafic volcanic rocks were derived from decompression melting of an ancient continental lithospheric mantle ( emi ) . with regard to the basaltic lavas , the felsic rocks resulted from partial melting of continental crust , which closely related to basaltic underplating 2燕山地區早侏羅世中基性火山巖來自于早期俯沖交代的古老巖石圈地幔部分熔融作用，俯沖交代作用可能與早期古亞洲洋閉合事件有關；晚侏羅世中基性火山巖更多來自于類似于emi型地幔源區的部分熔融作用，俯沖交代成分貢獻很弱；早白堊世基性火山巖則來自于emi型地幔源區的部分熔融作用。 |
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Four major rock types are found within the reserve . from the oldest to the youngest , they are the tuffs with volcanic bombs , granodiorites , porphyritic rhyolites and basaltic dykes , respectively . geomorphologically , the marine reserve has typical exposed rocky shore of south - easterly - directed capes and headlands in hong kong 鶴咀海岸保護區內可以找到四種主要巖石種類，以巖石形成的年代計算，最古老的是火山爆發形成的凝灰巖，然后依次是花崗閃長巖,流紋斑巖及玄武巖。 |
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Geologists have long known that water leaking into faults can trigger earthquakes , and nine days is about the same amount of time that they estimate it takes water to work its way down through cracks and pores in kilauea ' s fractured basaltic rock to a depth of five kilometers ? where the silent earthquake occurred 科學家早就知道，水要是滲進斷層之內便會引發地震，而他們估計，雨水從裂縫和孔隙滲入奇勞亞火山破裂的玄武巖所需的時間，正好就是九天；滲透的深度達五公里，也就是無聲地震發生的地方。 |
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The paper based on synthesize domestic and foreign ' s study achievement about basalt , systematical review basalt research history , present condition about basalt formation contributing factor and it ' s magma source area quality , uses the basalt to distinguish the earth ' s mantle type , the connection basaltic magma evolution and continent dynamics , and uses the basalt to distinguish tectonic environment 系統地綜述了玄武巖的成因和巖漿源區性質、利用玄武巖判別地幔類型、玄武質巖漿的演化與大陸動力學關系，以及判別構造環境等方面研究的現狀。 |
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According to the sr - nd isotopic characteristics of peridotite xenoliths and their host basalts , it indicates that xenoliths in hannuoba , puning area may represent source area of the host basalt because of the xenoliths and host rocks being in the same plot ; however , the xenoliths is not directly related to their host rocks of the others area for the xenoliths plot out of the range of their host basaltic rocks . thermal dynamics calculation shows that the peridotite xenoliths are formed in the condition of pressure of 9 . 45 - 25kb and temperature of 945 - 1281 橄欖巖包體及其寄主玄武巖的sr - nd同位素研究表明，漢諾壩與普寧地區部分包體樣品投點落在其寄主玄武巖nd和sr同位素的分布范圍內，表明橄欖巖包體代表了寄主玄武巖的源區，而其它大部分地區的包體其寄主玄武巖范圍之外，表明寄主玄武巖和橄欖巖包體無成因聯系，橄欖巖包體只是偶然包體。 |
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The alkaline basalts in southern hunan are suggested to have formed by small degrees of decompression melting of the asthenosphere mantle during the initial extension . the transitional ( the chebu gabbro ) and tholeiitic basaltic magmas were generated by relatively larger degrees of partial melting of the mantle 在裂谷初期，軟流圈地幔的小比例部分熔融形成堿性玄武巖(湘南) ，在裂谷拉張作用比較強、地幔部分熔融比例比較大時形成贛南和湘南的過渡型(車步輝長巖)及拉斑質玄武巖。 |
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The control of the deep - seated structural - magmatic process over the metallogenic system around the middle - lower yangtze river reaches is shown as : ( 1 ) the mantle uplift belt is closely related to the general geological background of the metallogenic system ; ( 2 ) the primitive magma originated from different parts of the mantle uplift belt ( mantle ridge or mantle slope ) shows differences in style of formation and composition and results in different magmatic series and metallogenic subzones , respectively ; ( 3 ) the varying depths of structural - magmatic chambers may form a “ three - layered structure “ ( central type , network - like and ring - like ) and this is the primary factor that controls the different magmatic series and the concerned cluster of ore deposits ; ( 4 ) the alkaline basaltic magma derived from the mantle ridge forms high - potassium and calcium alkaline magma and shoshonitic magma due to its altering intensity of afc process with the lower crustal material , which has something to do with the copper - gold and iron - sulphur metallogenic subsystems , respectively 深部構造巖漿作用對長江中下游成礦帶安徽沿江地區成礦系統的控制表現為： ( 1 )地幔隆起帶與成礦系統的總體地質背景的演變密切相關； ( 2 )源于地幔隆起帶不同部位(幔脊與幔坡)的原始巖漿，其生成方式和物質組成不盡相同，它們分別產生相應的不同巖漿巖系列和成礦亞帶； ( 3 )不同深度的構造巖漿房組成中心式網格式環帶式“三層結構” ，是控制區內不同巖漿巖系列及有關礦床集中分布的主要因素； ( 4 )源于地幔隆起帶脊部的堿性玄武巖漿，由于與下地殼物質發生的afc作用強度不同，形成了高鉀鈣堿性巖漿和橄欖安粗巖漿，分別與銅、金成礦亞系統和鐵、硫成礦亞系統有關。 |
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Based on the petrological , petrochemical and geochemical analyses about these rocks , it is concluded in this paper that the xenoliths were originated from the upper mantle , and comprised of both primitive pyrolite and the infusible solid residual of the upper pyrolite while the basaltic magma was melted out of it , which were brought up to the earth ' s surface via o1carnc eruption 根據其巖石學、巖石化學及地球化學特征分析，包體來源于上地幔，其成因既有原始地幔巖，亦有上地幔巖經部分熔融出玄武巖漿后的難熔固相殘留物，被火山噴發攜帶至地表。 |
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Secondly , based on the microbeam analytical technique , on the one hand , through investigating the characteristic of major elements in the mantle minerals the author acquired the static information from mantle ; on the other hand , through multi - point analysis of a part of the minerals from mantle , the auther got dynamic information from mantle . finally , generalizating the fruits of this study and predecessors , the autor holds that the constituents of lithospheric mantle possibly includes spinel lherzolites , clinopyroxenites , websterite , dunite , harzburgites , garnet lherzite , phlogopite lherzite , eclogites , clinopyroxene megacrysts ; compared with east china and north china platform , the research field mantle shows the characteristics of higher degree of partial melting processes and more depleted mantle ; the . upper mantle beneath north hetian area is heterogeneous , with a tendency of deficit in a12o3 and lree from kaliyang in west hetian to the river basin of kalakshi river and yulongkashi river ; the subduction of the crust beneath north hetian has ever occurred in geological history and caused the mixing of mantle - crust ; the depth of the origination of basaltic magmas beneath north hetian exceeds 73km ; the thickness of the lithosphere beneath the research area amounts to 204 . 9km ; the mantle beneath north hetian has geological condtions for forming diamond deposits 最后，綜合本區幔源礦物和地幔巖石的特征以及地球物理資料，得出如下結論：本區上地幔的物質組成有尖晶石二輝橄欖巖、二輝巖、單斜輝石巖、純橄欖巖、方輝橄欖巖、石榴石二輝橄欖巖、金云母二輝橄欖巖、榴輝巖；與中國東部以及華北地臺上地幔相比，研究區上地幔具有富集主元素中相容元素和虧損其中的不相容元素的特征，局部熔融程度較高；上地幔存在橫向和縱向的不均一性，從西部的克里陽到喀拉喀什河和玉龍喀什河流域， al和lree富集程度呈下降趨勢，不同來源的相同礦物中主元素的含量差異較大；地質歷史時期這里可能發生過地殼俯沖并產生殼幔混合作用；玄武巖漿的起源深度73km ；從幔源重砂礦物的溫壓估算結果，可以推斷出巖石圈厚度可達204 . 9km ；綜合巖石圈物質組成特征、巖石圈熱狀態、地幔溫壓狀態、氧逸度以及幔源巖石和幔源礦物的化學成分，認為研究區具備了金剛石成礦地幔地質條件。 |
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Whereas the rocks in the ancient heavily cratered terrains were basaltic , the younger rocks of the northern lowlands resembled a more highly evolved type of lava called andesite : they contained more glass , more silica - rich minerals and fewer iron - bearing minerals 古老、充滿坑洞的地區，巖石屬于玄武巖，但北方低地較年輕的巖石卻類似一種更高度演化、稱為安山巖的熔巖：它們含有較多玻璃質、較多富矽礦物、以及較少含鐵礦物。 |
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Notice that they are all five - sided more or less . and notice , from a distance as you start your hike , how geological movements as the basaltic magma congealed have produced a wall of bent basalt columns 向前走，你不妨留意遠處一堵高聳的巖柱墻，一條條的巖柱因巖漿凝固時遇地殼移動，都呈現了扭曲的形狀。 |
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The bulk of the volcano is basaltic , but the slopes are dotted with cones and lava flows consisting of glassy , silica - rich lavas called dacites 此火山的主體是玄武巖，但是山坡卻點綴著由石英安山巖（一種玻璃質、富含矽的熔巖）形成的熔巖錐和熔巖流。 |
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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，玄武巖質的沙披覆在湖床沉積物上，顯示此地已經乾涸了20 ~ 30億年。 |
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Existence of charcoal fragments in sedimentary basaltic volcanoclastic rock and its implication in geology , in longtan formation of southwesten guizhou 黔西南地區龍潭組玄武質火山碎屑巖中木炭碎屑的存在及地質意義 |
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Basaltic ( when this card is put into graveyard from anywhere , shuttle it into its owner ' s library 玄武化(當此牌被從任何地方放到墓地，把此牌洗回其擁有者牌庫中。 |
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The report on variolitic basaltic andesite in the dabieshan collisional orogenic belt 大別山造山帶中球顆結構玄武質安山巖的報道 |
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Basaltic lava first erupted from the center and built up the volcano 首先是玄武巖漿從中間噴發，構成火山。 |