斜长花岗岩,plagiogranite
1)plagiogranite斜长花岗岩
1.Geochronology,Geochemistry and Geological Implications of the Mengku Synorogenic Plagiogranite Pluton in Altay,Xinjiang;新疆阿尔泰蒙库同造山斜长花岗岩年代学、地球化学及其地质意义
2.U-Pb isotope zircon age of Baiyanhua plagiogranite in Seerteng area,Inner Mongolia;内蒙古色尔腾地区白彦花斜长花岗岩锆石U-Pb年龄
3.Dating and tectonic significance of plagiogranite from Guoganjianian Mountain,central Qiangtang, northern Tibet, China藏北羌塘中部果干加年山斜长花岗岩定年及其构造意义
英文短句/例句

1.All orebodies are gold quartz vein type and hosted in New Archaean metamorphic quartz diorite and plagiogranite.容矿岩系为新太古代变质石英闪长岩、斜长花岗岩
2.Dating and tectonic significance of plagiogranite from Guoganjianian Mountain,central Qiangtang, northern Tibet, China藏北羌塘中部果干加年山斜长花岗岩定年及其构造意义
3.Studies on the U-Pb ages and Hfisotopes of zircons in the Aoyitake plagloclase granite.west Tarim.塔里木西部奥依塔克斜长花岗岩锆石U-Pb年龄和Hf同位素研究
4.Geochemical characteristics of Early Palaeozoic plagioclase granite from ophiolitic cumulate in central Qiangtang, northern Tibet, China藏北羌塘中部早古生代蛇绿岩堆晶岩中斜长花岗岩的地球化学特征
5.Volcanic Rocks of the Pingshui Group and Plagiogranite of This Period in Jiangshan-Shaoxing Fault: Petrogenesis and Its Tectonic;江绍断裂带平水群火山岩及伴生斜长花岗岩的成因与大地构造意义
6.The Petrogenesis of Tuwu Plagiogranite Porphyry from East Tianshan:Evidence from Wallrock东天山土屋斜长花岗斑岩的成因——来自围岩的证据
7.granit is S-type and its evolution sequence might begranomonzonite → muscovite-granite(outcrop) → feldspar-granit →muscovite-granite(core);花岗岩演化顺序可能为二长花岗岩→露头白云母花岗岩→钾长花岗岩→白云母花岗岩芯。
8.Study on Crystal Chemistry and Spectra of Feldspar from Zhoukoudian Granodiorite周口店花岗闪长岩中斜长石晶体化学及谱学特征研究
9.Application of Plagioclase Solution Degree to Evaluating the Weathering Degree of CDG of Granites斜长石溶蚀度:一种评价花岗质岩石风化度的新指标
10.TILT CHANGE ACCOMPANYING SLOW FRACTURE PROCESS IN LARGE SCALE TEST SAMPLE OF GRANODIORITE大尺度花岗闪长岩试件缓慢破裂过程的倾斜变化
11.Any of various dark, granite - textured, crystalline rocks rich in plagioclase and having little quartz.闪长岩一种黑色花岗岩的纹理的结晶质火岩石,富有斜长石,含有少量石英
12.Talking about the Hole-site Correcting Technology in Drilled Pile Construction on Granite Plagioclase Strata花岗岩斜岩地层钻孔桩施工孔位纠偏技术
13.Early Yanshanian intrusions are mainly adamellite,biotite K-feldspar granite with small amount of granodiorite.燕山早期侵入岩以二长花岗岩、黑云钾长花岗岩为主,其次为花岗闪长岩。
14.The main diagenetic stage and relevant rock types are the Middle Proterozoic assemblage of gneissoid granodiorite-adamellite and the Sinean schistosity diorates.主要成岩期及代表性岩类有:中元古界为片麻状花岗闪长岩-二长花岗岩,震旦纪为片理化闪长岩。
15.The Penshan granitic body is a calc-alkaline pluton composed of muscovite alkali granite, two-mica alkali feldspar granite and biotite adamellite.彭山岩体是由白云母碱长花岗岩、云母碱长花岗岩和黑云母二长花岗岩组成的钙碱性花岗复式岩体。
16.The deposit is an alkali-feldspar granite type Ta deposit.该矿床为碱性长石花岗岩型钽矿床。
17.Study on the Roughness Coefficient of Slope Face in the Granitic Region of Three- Gorge of the Yangtze River长江三峡花岗岩区坡面糙率系数研究
18.igneous rock that has solidified beneath the earth's surface; granite or diorite or gabbro.已经在地表凝固的火成岩;花岗岩、闪长岩或辉长岩的。
相关短句/例句

porphyritic granite闪云斜长花岗岩
1.In this paper,the data of the uniaxial compressive strength of porphyritic granite at micro-new status is analyzed from the experiment of the Three Gorges Project,in which the time span is from April in 1956 to May in 1999.从三峡工程岩石力学试验报告中整理出闪云斜长花岗岩微新状态的单轴抗压强度数据,时间跨度自1956年4月至1999年5月。
3)plagioclase granite porphyry斜长花岗斑岩
1.It was reported that they were the same unit,and all the time denominated biotite plagioclase granite porphyry.安徽省石屋岩体和岑山岩体在地质产状、形成时代及岩石学特征上十分相似 ,前人将其划为同一单元 ,并一直将其定名为黑云母斜长花岗斑岩。
4)oceanic plagiogranite大洋斜长花岗岩
1.Geochemistry and petrogenesis of oceanic plagiogranitein the ophiolite from Northeast Jiangxi Province;赣东北蛇绿混杂岩带中大洋斜长花岗岩的地球化学和岩石成因
5)yosemitite斜长黑云花岗岩
6)plagio-monzonitic granitic gneiss斜长-二长花岗质片麻岩
1.Late Paleozoic plagio-monzonitic granitic gneiss with complex deeplevel folds or ductile deformation in Altai orogen belt is associated with the middle grade of metamoprphic rock series.钕模式年龄在 14 0 0 Ma~ 180 0 Ma,εNd(t)为正值 ,反映斜长-二长花岗质片麻岩源于年青地壳 ,并不是前寒武纪结晶基底 ,结晶成岩作用和变质变形作用几乎是同时发生的 ,年龄为 35 5 Ma± 5 M
延伸阅读

更长环斑花岗岩  一种花岗岩类的岩石。红色或灰色,常含暗色矿物角闪石和黑云母。它的主要特征是具有一种特殊的斑状结构──更长环斑结构。斑晶为球形-卵形的钾长石(条纹长石、微斜长石),外绕更长石环(个别为钠长石、中长石环)。钾长石斑晶或为具卡氏双晶的单个晶体,或为几个不规则状、扇状晶体组成的集合体。在钾长石斑晶中常见有环状分布的更长石、石英、黑云母、角闪石等矿物包裹体。这种花岗岩的基质矿物主要为石英、钾长石、黑云母,有时还有角闪石。副矿物为锆石、磷灰石、金属矿物等。更长环斑花岗岩是主要形成于前寒武纪时期,与它近似的岩石有更长环斑细晶岩及更长环斑正长岩等。它们常与其他中酸性侵入岩共生。在中国产于北京密云、河北赤城、江西上饶、辽宁桓仁、陕西商县、福建漳州等地。