Dunite

  • 网络纯橄榄岩
DuniteDunite
  1. The fractal structure factors ( FSF ) of spinel from ultramafic xenolith , harzburgite , dunite and chromite have been calculated using a new method presented by Shen ( 1993 ) .

    利用沈步明(1993)提出的分形结构因子的新方法,计算了橄榄岩包体、方辉橄榄岩、纯橄榄岩和铬铁矿等六种尖晶石的分形结构因子。

  2. The partial melting of the upper mantle not only controlled the evolution of mantle rock types ( lherzolite → harzber-gite → dunite ) but also played a critical role for chromite preconcentration .

    上地幔部分熔融作用不仅控制了上地幔岩石类型演化(二辉橄榄岩→方辉橄榄岩→纯橄榄岩),同时它对铬铁矿的预富集起着关键作用。

  3. Elastic P Wave Velocity and Attenuation in Dunite up to 4.0 GPa

    4.0GPa压力下纯橄岩弹性纵波速度和衰减的实验研究

  4. This paper deals with the geological characteristics of a dunite body with layering structure from Sichuan-Yunnan area .

    本文对川滇地区某纯橄榄岩体的地质特征进行了初步研究。

  5. The discovery and study of mantle-derived dunite inclusions in hornblende-diorite in the Handan-Xingtai area , Hebei

    河北邯邢地区角闪闪长岩中地幔纯橄岩包体的发现与研究

  6. On the basis of the genetic type , the ultramafic bodies are part of ultramafic unit of ophiolite and the positions where the chromite enriched are mantle peridotite or bottom dunite of cumulate complex zone .

    岩体成因类型为蛇绿岩组合中的超镁铁质单元,铬铁矿的富集部位是地幔橄榄岩和堆积杂岩带底部的纯橄榄岩。

  7. The ophiolite is composed of dunite , peridotite , gabbro , massive basalt , pillow basalt , basaltic andesite , silicalite and siltstone with thickness of over 1500 m.

    新疆库地蛇绿岩堆积厚度达1500m以上,主要岩石由纯橄岩、斜辉橄榄岩、辉长岩、块状玄武岩、枕状玄武岩、玄武安山岩、硅质岩、粉砂岩等组成。

  8. Lithologic types of the massifs are mainly harzburgite and dunite , with subordinated lherzolite ( orthopyroxene : 5 ~ 7 % ) . The textures and structures are similar to those of metamorphic rocks , and micro - plastic deformation of minerals is ubiquitous .

    主要岩石类型是方辉橄榄岩和纯橄榄岩,二辉橄榄岩极少(单斜辉石含量5~7%),具有典型的变质岩结构构造特征,矿物显微塑性变形普遍发育。

  9. The Shanwang basalts contain ultramafic inclusions and megacrysts of clinopyroxene and anorthoclase . The ultramafic inclusions can be divided into five classes : spinel dunite , spinel lherzolite , spinel harzburgite , spinel-garnet websterite and garnet lherzolite .

    山旺新生代玄武岩中的超镁铁质包体分为五类:尖晶石纯橄榄岩、尖晶石二辉橄榄岩、尖晶石方辉橄榄岩、尖晶石石榴石二辉岩和石榴石二辉橄榄岩。