- 更多网络例句与斜长岩的相关的网络例句 [注：此内容来源于网络，仅供参考]
-
The chemical composition of Pingyang gneissic granite with high contents of SiO〓, Na〓O, Sr and Ba was inherited and developed from that of mainly biotite gneiss through anatexis under the background of regional migmatisation, it might also be introduced the fluid material from deep.
平阳片麻状花岗岩的化学成分是在区域混合岩化对岩石成分总体改造趋势的背景下，在黑云斜长片麻岩成分的基础上，通过黑云斜长片麻岩的深熔以及可能的变质脱水反应流体和深部流体的加入演变而成，富SiO〓、Na〓O以及Sr和Ba。
-
Composed mainly of anorthosite and plagiogranite, the leucocratic rocks show distinct Eu positive anomaly.
浅色岩类的岩石类型包括斜长岩和斜长花岗岩，它们均呈岩块状包裹于蛇纹岩中。
-
SHRIMP zircon U-Pb ages of gabbro, anorthosite, and plagiogranite from the ophiolitic complex, and related marginal granite in the Jinshajiang area, provides important geochronological constraints for the oceanic spreding, the subduction and final collision, therefore, which constructs a time framework for the Jinshajiang Paleo-Tethys evolution.
应用SHRIMP方法测定了金沙江蛇绿岩中的各类辉长岩，斜长岩，斜长花岗岩，及沿金沙江带分布的陆缘型花岗岩的年龄，提供了洋壳形成，俯冲消减和碰撞造山事件等古特提斯演化的重要的同位素地质年代学制约，从而建立了金沙江古提斯演化的年代格架。
-
The volcanic rocks of the Xiong'er Group is also widespread in the Baoji and Lvliang area and also appear as 1.75Ga-old mafic dyke swarms, A-type granites, later anorthosite and rapakivi granites (1.75-1.70Ga), and alkaline granitoids (~1.65Ga). These intrusive rocks are assumed to have genetic link to the volcanic rocks of the Xiong'er Group.
熊耳期岩浆活动在华北陆块广泛分布，除了陕西宝鸡附近及山西吕梁地区的火山岩，还广泛分布1.75Ga前后的基性岩墙群、A-型花岗岩以及比熊耳群稍晚的斜长岩、奥长环斑花岗岩等(1.75-1.70Ga)和碱性花岗岩类(~1.65Ga)。
-
Pyroxene grains in gabbroic anorthosite,troctolite,microporphyritic crystalline impact melt breccia,and Ti-bearing clasts are mainly low-Ca pigeoniteEn_(63Fs_(32)Wo_5,En_(66)Fs_(23)Wo_(11),En_(55)Fs_(38)Wo_7,and En_(57)Fs_(35) Wo_8,respectively,and those in anorthositie gabbro,gabbro,and the matrix display a wide range of compositionEn_(31～33Fs_(35～48) Wo_(19～34),En_(18～48)Fs_(23～51)Wo_(24～38)+En_(1～9)Fs_(65～86)Wo_(14～26),En_(11～53)Fs_(23～63)Wo_(6～36),respectively,mainly occurring as pigeonite,augite, and trace amounts of pyroxferroite.
辉长质斜长岩、橄长岩、微斑熔融角砾岩等岩屑和含钛玻屑中的辉石相对贫钙，主要为易变辉石(分别为En63 FS32 WO5，En66FS23WO11，En55FS38Wo7和En57FS35WO8)，而斜长岩质辉长岩和辉长岩岩屑中的辉石和晶屑辉石的成分变化比较大(分别为En31～33 FS35～48 WO19～34，En18～48 FS23～51 WO24～38+En1～9 FS65～86 WO14～26和En11～53 FS23～63WO6～36)，为易变辉石和普通辉石，以及少量三斜铁辉石。
-
Below 1100℃, the amount of argon released from irradiated samples is in an order of: plagioclase rock＞striped migmatite＞granite＞garnetiferous mica schist＞calciummuddy shale＞basalt.
在1100℃之前，辐照样释放的氩气量按顺序排列为：斜长岩＞条带状混合岩＞花岗岩＞含石榴石云母片岩＞钙泥质页岩＞玄武岩。
-
Any of a common rock-forming series of triclinic feldspars, consisting of mixtures of sodium and calcium aluminum silicates.
斜长岩三斜晶长石系列中一种普通的成岩石，由钠和钙铝硅酸盐组成
-
Any of a common rock - forming series of triclinic feldspar s,consisting of mixtures of sodium and calcium aluminum silicates.
斜长岩三斜晶长石系列中一种普通的成岩石，由钠和钙铝硅酸盐组成
-
Any of a common rock - forming series of triclinic feldspars,consisting of mixtures of sodium and calcium aluminum silicate s.
斜长岩三斜晶长石系列中一种普通的成岩石，由钠和钙铝硅酸盐组成
-
Composed mainly of anorthosite and plagiogranite, the leucocratic rocks show distinct Eu positive anomaly.
浅色岩类的岩石类型包括斜长岩和斜长花岗岩，它们均呈岩块状包裹於蛇纹岩中。
- 更多网络解释与斜长岩的相关的网络解释 [注：此内容来源于网络，仅供参考]
-
amphibolite：角闪岩
斜长角闪岩(amphibolite) 斜长角闪岩 主要由角闪石和斜长石组成的中,高级区域变质岩.又称角闪岩.角闪石和斜长石的含 量相近.可含少量石英,铁铝榴石,黑云母,单斜辉石和斜方辉石.常为中,细粒纤状变晶 结构,可具有块状,
-
quartz anorthosite：石英斜长岩
quarto 四开;四开本;四开的 | quartz anorthosite 石英斜长岩 | quartz crystal oscillator gauge 石英晶体振荡压力计
-
Bigwig：要人, 有重大影响的人
biguanide | 双胍 缩二胍(降血糖药) | bigwig | 要人, 有重大影响的人 | bigwoodite | 钠长微斜正长岩
-
gabbro：岩
辉长岩(gabbro) 主要由基性斜长石和单斜辉石组成的深成基性岩浆岩. 闪长岩(diorite) 主要由中性斜长石和角闪石组成的深成中性岩浆岩. 花岗岩(granite) 主要由石英、长石、云母和少量其他深色矿物组成的深成酸性岩浆岩.
-
quarto：四开;四开本;四开的
quartimin method 四次幂极小法 | quarto 四开;四开本;四开的 | quartz anorthosite 石英斜长岩
-
anorthic：三斜
anorogenic 非造山的 | anorthic 三斜 | anorthitite 钙长岩
-
orthosymmetric：正交对称的(斜方对称的)
"钾质正长岩","orthosyenite" | "正交对称的(斜方对称的)","orthosymmetric" | "陨正镍纹石","orthotaenite"
-
plagioclastic：斜交解理的
"斜长岩类","plagioclasolite" | "斜交解理的","plagioclastic" | "斜长片麻岩","plagiogneiss"
-
syenodiorite：正长闪长岩
而正长闪长岩(syenodiorite)和正长辉长岩(syenogabbro)分别是正长岩和闪长岩或正长岩与辉长岩之间的过渡岩石,亦即包括二长岩10 区- 本区岩石有三个基本名称,即闪长岩(diorite),辉长岩(gabbro)和斜长岩(anorthosite),以斜长石(PI)、辉石(Px),
-
syenogabbro：正长辉长岩
而正长闪长岩(syenodiorite)和正长辉长岩(syenogabbro)分别是正长岩和闪长岩或正长岩与辉长岩之间的过渡岩石,亦即包括二长岩10 区- 本区岩石有三个基本名称,即闪长岩(diorite),辉长岩(gabbro)和斜长岩(anorthosite),以斜长石(PI)、辉石(Px),