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1.Metamorphic rock having porphyritic texture.
斑岩斑岩状结构的变质岩收藏指正
2.A conspicuous, usually large, crystal embedded in porphyritic igneous rock.
斑晶嵌在斑状火成岩中的一种显眼的、通常很大的晶体收藏指正
3.The fine-grained crystalline base of porphyritic rock in which larger crystals are embedded.
基质斑岩中均匀的水晶质石基,其中嵌有大粒水晶收藏指正
4.Theearly stage comprises fine grain adamellite and medium coarse grained porphyritic adamel-lite,while the late stage, it consists of medium grain adamellite with huge phenocryst.
早期由细粒二长花岗岩、含斑中粗粒二长花岗岩构成; 晚期由斑状中粗粒二长花岗岩、巨斑状中粒二长花岗岩构成。收藏指正
5.There are large quantities of fine-grained,porphyritic dioritic enclosures in the Shimen rockbody,southeastern part of Antu County,Jilin Province Through the study on the form of the enclosures,mode of occurrence,characteristic,texture,mineralogical composition and mineral growth habit,it is preliminarily definited that the Shimen magma is at least composed of the acidic and basic magma in a complete uncrystallized state,and proposed for the first time that the rockbody has some characteristics of the migmatitic granite,belonging to mixed magmatic granite
位于吉林省安图县东南的石门岩体中,含有大量细粒、斑状闪长岩包体,通过对其形态、产状及特征,特别是包体的结构、矿物成分及矿物生长习性等岩相学特征的研究,初步确定石门岩体岩浆至少是由酸性、基性两种不同成分的岩浆在未完全结晶状态下相互混合形成,首次提出该岩体具岩浆混合花岗岩特征,为浆混成因花岗岩。收藏指正
6.The Chifengshan gold-polymetallic deposit is located in the Beishan polymetallic mineralization belt. There are 114 gold-polymetallic veins in the area, among them 19 are gold veins and auriferous veins, they occurred in the marble of Jixian System Pingdingshan Group which located in the north contact zone between biotite adamellite rock body and porphyritic granodiorite stock of Later Variscan, and controlled by the contact zone skarnization belt and EW, NE, NW and NNW strike fault.
赤峰山金 多金属矿位于北山多金属成矿带,区内共发现金 多金属矿脉114条,其中金和含金矿脉19条,均产于华力西晚期黑云二长花岗岩体和斑状花岗闪长岩株北接触带上的蓟县系平顶山群大理岩中,受接触带夕卡岩化带及近EW、NE、NW和NNW向断裂所控制。收藏指正
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汉英释义
adj. 斑岩的