subhedral [sʌb'hi:drəl]

subhedral的基本解释

adj.

[晶]半形的, 仅有部分晶面的

与subhedral相关的网络例句 [注：此内容来源于网络，仅供参考]

Deep buried dolostones in study areas mainly consist of fine or medium dolomites, which crystals are euhedral or subhedral.

认为研究区深埋藏白云岩主要由细晶或中晶白云石组成，白云石呈自形或半自形晶。

Ore structures appeared euhedral and subhedral granular, polygonal cleavage, anhdral granular and sheet texture.

矿石构造主要出现致密块状矿石，条带状磁铁矿和浸染状磁铁矿；矿石结构包括自形、半自形粒状结构，多边形解理结构、他形粒状结构和片状结构(1∶20万富蕴幅，1978)。

Little quantity of sulphur occur in forms of enclave and anhedraal,subhedral,euhedral crystal. The crystal size ranges from0.01mm to1. 00mm and little of size around 1μm.

少量呈包体形式产出，它形～半自形～自形晶，粒径在0.01mm～1mm间，极少量的在1μm这些硫化物中的硫，含量略低于其相应矿物的硫的含量。

There are two kinds of spinels in a granulite terrain of Yushujgou, South Tianshan Mountain. One occurs in the intermediate and basic granulite units and is characterized by enriched Al and poor Cr, belonging to Al_spinel. In thin sections it shows dark green color and subhedral to anhedral form, and coexists with other metamorphic minerals, suggesting a neogenic metamorphic mineral of granulite facies. The other occurs in the adjacent ultramafic rock unit, belonging to Cr_spinel. In thin sections, it is dark brown in color and is scattered among olivine, clinopyroxene and orthopyroxene as irregular grains, indicating a stable residual mineral in the process of granulite facies metamorphism.

新疆榆树沟麻粒岩地体中发育两类尖晶石：一类见于中、基性麻粒岩体中，其化学成分富 Al贫 Cr ，属铝尖晶石，镜下为深绿色，呈半自形至他形粒状，与其它变质矿物共生，表现为麻粒岩相的新生变质矿物；另一类发育在空间上与麻粒岩体紧密相邻的超镁铁质岩体中，为铬尖晶石，镜下为深褐红色，呈不规则粒状分布于橄榄石、斜方辉石和单斜辉石之间，为麻粒岩相变质过程中稳定的残余矿物。

与subhedral相关的网络解释 [注：此内容来源于网络，仅供参考]

subhedral：半自形的

subhedral crystal 半自形晶 | subhedral 半自形的 | Subhercynian movement 新海西运动

subhedral：半形的;半自形的

半鹹水的 brackish | 半形的;半自形的 subhedral | 半亞潮濕的 subhumid

subhedral：半形的/半自形

subheading /副标题/ | subhedral /半形的/半自形/ | subhedron /半自形晶体/

subhedral：半形的

subheadsubheading 副标题 | subhedral 半形的 | subhedral 半自形

subhedral crystal：半自形晶

subhead 小标题;副标题 | subhedral crystal 半自形晶 | subhedral 半自形的