橄石 的英文怎麼說
中文拼音 [gǎndàn]
橄石
英文
olivin-
During diagenetic process, there may exist the fractional crystallization of clino - pyroxene, plagioclase, olivine and ti - fe oxide, and the accumulation of olivine. the alkalic - ultramafic dikes formed by low degree partial melting ( 3. 4 % ) of enriched mantle, consist of single olivine pyroxenolite, the dominating olivine fractionation is evident
成因上為富集地幔部分熔融作用的結果,但在成巖過程中也可能存在單斜輝石、斜長石、橄欖石和ti - fe氧化物等礦物的分離結晶作用。Olivine has been completely altered to serpentine, talc, and amphibole in the bore-hole examined in detail.
鉆芯詳細檢查的結果,橄欖石全部蝕變為蛇紋石、滑石及角閃石。Colorful crystal necklace crystal aquamarine olivine
水晶海藍寶橄欖石Clear crystal, irregular shape nature gemstones aquamarine, olivine
白水晶,橄欖石,綠長石,海藍寶And all came with nimbi and aureoles and gloriae, bearing palms and harps and swords and olive crowns, in robes whereon were woven the blessed symbols of their efficacies, inkhorns, arrows, loaves, cruses, fetters, axes, trees, bridges, babes in a bathtub, shells, wallets, shears, keys, dragons, lilies, buckshot, beards, hogs, lamps, bellows, beehives, soupladles, stars, snakes, anvils, boxes of vaseline, bells, crutches, forceps, stags horns, watertight boots, hawks, millstones, eyes on a dish, wax candles, aspergills, unicorns
他們手執棕櫚葉豎琴劍橄欖冠,袍子上織出了他們的職能的神聖象徵:角制墨水瓶595箭麵包壇子腳鐐斧子樹木橋梁浴槽里的娃娃們貝殼行囊596大剪刀鑰匙597百合花鹿彈胡須豬燈風箱蜂窩長柄杓星星蛇598鐵砧一盒盒的凡士林鐘丁字拐鑷子鹿角防水膠靴老鷹磨石盤子上的一雙眼球599蠟燭灑聖水器獨角獸600 。On the basis of the study on the petrology, trace element, and isotopic geochemistry, the primary magma of volcanic rocks can be divided into two series according to their originated rocks and degree of partial melting. one is the basanite - alkaline basalt - olivine tholeiite magma series, which are generated by partial melting from spinel iherzolite ; the other is nephelinite magma - alkaline picritic basalt magma, which are generated by partial melting of the garnet iherzolite
巖石化學、微量元素、同位素地球化學證據都表明,華北、華南地區的火山巖根據源巖和局部熔融程度的不同,可以分為兩個原生巖漿系列:一個是源巖為尖晶石二輝橄欖巖,隨著局部熔融程度的增加,形成的碧玄巖巖漿-堿性玄武巖巖漿-橄欖拉斑玄武巖巖漿;另一個是源巖為石榴石二輝橄欖巖,隨著局部熔融程度的增加形成的霞石巖巖漿-堿性苦橄玄武巖系列。The chromite deposits in the muskox complex occur only in feldspathic peridotite.
在穆斯科克斯雜巖體中,鉻鐵礦礦層僅產于長石質橄欖巖中。With regard to the oxide minerals, chromite is almost entirely contained in the olivine-rich ultramafic rocks in the lower part of the intrusion.
關于氧化礦物,鉻鐵礦幾乎全部含于侵入體下部的富橄欖石的超鎂鐵質巖石中。It is the only precious stone known to exist in outer space as it has even been found in meteors that have fallen to earth. peridot ranges in color from light yellow - green to intense bright green and on to olive green. the purer green a peridot is the higher the value
古羅馬的哲學家普林尼曾用chrysolite一詞,這個字是來自希臘文,是「金色」和「寶石」的意思,是用來形容黃水晶,黃玉的,但今天,在歐洲常常用於黃綠色及綠黃色的橄欖石。The purer green a peridot is the higher the value. gem quality peridot comes from zagbargad ( zebirget ) island in the red sea off the coast of egypt, mogok, myanmar ( burma ), kohistan, pakistan, brazil, germany, mexico, ethiopia, australia, and arizona and hawaii in the united states
古羅馬的哲學家普林尼曾用chrysolite一詞,這個字是來自希臘文,是「金色」和「寶石」的意思,是用來形容黃水晶,黃玉的,但今天,在歐洲常常用於黃綠色及綠黃色的橄欖石。Elongate olivine crystals were aligned to produce a flow texture as this liquid phase crystallized.
在液相結晶時,長形橄欖石晶體的成行排列產生了流狀構造。The ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical ophiolite suite
摘要該蛇綠巖帶的巖體由地幔橄欖巖組成,主要巖石類型是方輝橄欖巖和純橄欖巖,缺少典型蛇綠巖剖面中的洋殼單元。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
最後,綜合本區幔源礦物和地幔巖石的特徵以及地球物理資料,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、金雲母二輝橄欖巖、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徵,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並產生殼幔混合作用;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徵、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。Electrical conductivities of quartz, olivine, dunite, iherzolite, pyroxenite, and megaaugite were measured by virtue of the new system ; whereas, the electrical conductivity of gabbro was measured by means of the old one. an interesting outgrowth of the present study is the measurement of the complex impedance of a series of quartz plates with different orientations
石英(人造水晶) 、橄欖石、純橄欖巖、輝石巖、二輝橄欖巖、巨晶輝石的電導率測量是在新的測量系統下獲得的,而輝長巖的電導率測量是基於lcr儀為測量儀器的測試系統下獲得的。Siziwangqi of inner mongolia is located on the north margin of north china craton, the junction of north china craton and siberia. granulite xenoliths are found there in cretaceous basalt. these xenoliths are mainly plagioclase - pyroxenite
內蒙古四子王旗地區地處華北板塊北緣,與西伯利亞板塊的接合部,其早白堊世橄欖玄武巖中發現大量下地殼麻粒巖捕虜體,並可見輝石長石捕虜晶。The determinative characteristics of common rock forming minerals containing quartz group, feldspar group, mica group, hornblende group, pyroxene group, olivine group and carbonatite minerals will be discussed in greater detail
對常見造巖礦物,如石英類、長石類、雲母類、角閃石類、輝石類、橄欖石類、碳酸鹽類礦物的鑒定特徵將予以詳細的說明。Below the lithosphere is the rheosphere comprising partly fused peridotite.
巖石圈之下是由部分熔融的橄欖巖所組成的軟流圈。High - mg volcanic rocks approach the primitive mantle compositions, and their magmatic source is close to the composition of bse, derives from the lower mantle and formed by this type - mantle rocks " fractional melting highly ( > 25 % ). high - mg volcanic magma, formed in the axis of the emei mantle plume, underwent the crystallization differentiation of olivines and some pyroxenes ; some olivines reflect fair cumulus crystallization
高鎂火山巖接近於原始巖漿的組成,巖漿源區與地球平均成分bse的成分特徵相近,起源深度為下地幔,為該地幔巖較高程度的部分熔融( 25 )而形成的。高鎂火山巖處于地幔柱的軸部,經歷了橄欖石及一定程度的輝石分異結晶,並且橄欖石顯示出一定的堆晶作用。Forsteritic olivine almost invariably represents primary precipitate material.
鎂質橄欖石幾乎總是代表了原生沉澱物。The olivine grains in the troctolite of the upper zone are rather short and thick.
上巖帶橄長巖中的橄欖石顆粒相當短粗。分享友人