花崗質巖 的英文怎麼說

中文拼音 [huāgǎngzhíyán]
花崗質巖 英文
granitics
  • 花 : Ⅰ名詞1 （種子植物的有性繁殖器官） flower; blossom; bloom 2 （可供觀賞的植物） flower 3 （形狀像花...
  • 崗 : 名詞1. （不高的山） hillock; mound 2. （平面凸起的一長道） ridge; welt; wale3. （崗位;崗哨） post; sentry
  • 質 : Ⅰ名詞1 （性質; 本質） nature; character; essence 2 （質量） quality 3 （物質） matter; substance;...
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 花崗 : granodiorite
  1. Three main rock types make up the geology of singapore : igneous, sedimentary and alluvium. where is the main source of granite found

    形成新加坡地質的三種主要巖石類型：火成巖、沉積巖和沖積巖。哪裡是花崗巖的主要來源地？
  2. 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。
  3. ( 5 ) the kd values of tc on biotite are higher than that on granite and the sorption properties is similar to that of granite ; the kd values of tc on quartz are very low

    （ 5 ）黑雲母對tc的吸附kd值高於花崗巖，且吸附的性質與花崗巖相似；石英對tc吸附的kd值很低。
  4. Discussion on physico - mechanical properties and deformation characters of eluvial soil of granite

    花崗巖殘積土物理力學性質及變形特性的探討
  5. Car platform pvc floorboard, marble, tiles or hardened wood

    塑料木質或花崗巖地板
  6. ( 7 ) by studying of ore - forming fluid and the micas ( using the f, cl contents in micas to calculate the halogen fugacity of the hydrothermal fluid, eg

    （ 7 ）通過對成礦流體和花崗質巖石黑雲母、白雲母中鹵素相對逸度的研究（ 109擔20 / fh 。
  7. 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。
  8. In the granites and related rocks the alkalis are, of course, noticeably in excess of the femic constituents.

    在花崗巖及有關的巖石中，堿質當然顯著地超過鐵鎂組分。
  9. Geochemistry of the carboniferous - permian post - collisional granitic rocks from tianshan

    二疊紀后碰撞花崗質巖石地球化學研究
  10. The granitic rocks in zhuluke area, western liaoning, emplaced during late hercynian - indosinian cycle, with rb - sr isochronal dating age of 226. 8 260 ma

    摘要朱碌科地區花崗質巖石侵位時間為二疊三疊紀。
  11. East qinling - dabie mountains ; lithosphere delamination ; granitoid ; uhpm ultra - high pressure metamorphite

    東秦嶺大別造山帶巖石圈拆沉花崗巖類超高壓變質巖
  12. 2. 6 2. 7ga, these granitoids are most likely to be derived from the partial melting of hybrids both 2. 6ga metavolcanic materials in archean wutaishan magmatic arc and older continent crustal materials under lower than 1. 2gpa. petrological and geochemical characteristics of wangjiahui granitoid intrusion suggest that is probably fored under post - collisional tectonic background

    2 . 1ga在- 3 . 82 - 2 . 80范圍，表明王家會古元古代花崗巖最有可能形成於大約2 . 6ga五臺山大洋島弧火山巖物質和更老的陸殼物質在
  13. Gneissic granite did not experience ultrahigh - pressure metamorphism from bixil

    大別山碧溪嶺未經歷超高壓變質的片麻狀花崗巖
  14. There are two kinds of rock mass seen in the region, one is jiaodong group to the moderate metamorphose extent, another one is the granite

    區內出露巖性主要有兩大類，一類是中深變質程度的膠東群，另一類是花崗巖。
  15. Through the study of characteristic of macroelement, microelement, rare - earth element, oxyhydrogen isotope, sulfur isotope, lead isotope, fluid inclusion etc, a conclusion can be drawn that metallogenic substance comes from the upper mantle with mixing of some substance from the upper crust latter. it is likely to have the same source with the surrounding rock

    通過對礦床的常量元素、微量元素、稀土元素、流體包裹體特徵、氫氧同位素、硫同位素、鉛同位素等特徵的研究，認為成礦物質主要來源於上地幔，與周圍巖石存在著同源的可能性，後期有一定的上地殼物質混入，成礦作用有三期，分別與區內的花崗巖、二長花崗巖脈、雲煌巖脈有關。
  16. Specification for straightedges - steel or granite straightedges of rectangular section

    直尺規范.第2部分:鋼質或花崗巖矩形截面直尺
  17. Geochronological, geochemical and sr - nd isotopic data are reported for the alkaline igneous rocks ( syenites and zhaibei aluminous a - type granite ) and chebu gabbro in southern jiangxi province. shrimp zircon u - pb dating results indicate that the quannan syenite, zhaibei a - type granite and chebu gabbro formed during the early yanshanian period

    對贛南燕山早期的富堿火成巖（正長巖和寨背鋁質a型花崗巖）和車步輝長巖進行了詳細的年代學、元素和sr - nd地球化學研究。
  18. Genesis of the dashiqiao granite and its significance in borate mineral exploration

    遼寧大石橋花崗質巖石成因分析及其在硼礦勘查中的意義
  19. The helong olivine komatiite within the granitc - grcenstone belt in the eastern part of north china platform

    華北地臺東段花崗綠巖帶中和龍橄欖石質科馬提巖
  20. Cl, s, f, tongchang porphyry copper deposit and the dajishan tungsten deposit are selected as the studying objectives, detailed investigations have been conducted into the geological and geochemical characteristics of the granitic rock, biotite, trace element and ree geochemistry, fluid inclusion geochemistry and the partitioning coefficients of the f, cl, cu, w. based on these data, the following conclusions are drawn : ( 1 ) fluorine can reduce the viscosity and density of magma, temperature of solide - liquidus line and change the melt frame, but cl has little effect on the melt

    主要的認識如下： （ 1 ） f在花崗質巖漿中，可以降低巖漿的粘度、密度、固液相線溫度、改變熔體結構，而cl對熔體結構沒有多大的影響。 f在流體?花崗質熔體相間，絕大多數配分系數小於1 . 0 ，趨向于熔體相中配分， d _ f隨體系中f濃度的升高而增加。
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