1.
Water Content of Peridotite Xenoliths from Cenozoic Basalt in Yangyuan, Hebei Province
河北阳原新生代玄武岩中橄榄岩捕虏体的含水量研究
2.
Ages of Peridotitic Xenoliths from the Central and Eastern Areas of North China Craton and Mantle Heterogeneity
华北克拉通中东部典型地区橄榄岩捕虏体年龄及地幔不均一性
3.
Mineral Chemistry of Peridotitic Xenoliths in Yangyuan Cenozoic Basalts: Significance for Lithospheric Mantle Evolution Beneath the Trans-North China Orogen
河北阳原新生代玄武岩中橄榄岩捕虏体矿物化学特征：华北内部山带岩石圈地幔演化意义
4.
Mineral Chemistry of Peridotite Xenoliths in Yangyuan Cenozoic Basalts:Significance for Lithospheric Mantle Evolution beneath the North China Craton
河北阳原新生代玄武岩中橄榄岩捕虏体矿物化学:华北岩石圈地幔演化
5.
alkali olivine basalt magma
碱性橄榄玄武岩岩浆
6.
Water Contents in Peridotite Xenoliths from Subei Basin,Eastern China
苏北盆地新生代玄武岩中橄榄岩包体的含水性
7.
A rock fragment foreign to the igneous mass in which it occurs.
捕虏体指在火成岩中形成的外来岩石碎片
8.
Alpine peridotite serpentinite
阿尔卑斯型橄榄蛇纹岩
9.
No original relation was found between the xenoliths and the host basalt.
上述捕虏体均与寄主玄武岩无成因关系。
10.
The rock-body which have the relation of mtallogenic of copper-nickel ore have the characteristic of compound rock-body. They belong to mafic, ultramafic rocks which type are gabbro, pyroxenite and peridotite.
与铜镍矿成矿有关的岩体具有复合杂岩体特征,多属辉长岩—辉石岩—橄榄岩型镁铁—超镁铁质岩。
11.
The chromite deposits in the Muskox Complex occur only in feldspathic peridotite.
在穆斯科克斯杂岩体中，铬铁矿矿层仅产于长石质橄榄岩中。
12.
Distribution Law and Future Prospecting of Marble Xenoliths in Tieshan Intrusion,Southeastern Hubei Province
鄂东南铁山岩体内部大理岩捕虏体分布规律及找矿探讨
13.
The pyroxenite xenoliths could be accumulates of the high-pressure fractional crystallization of the parental magma.
辉石岩类捕虏体是由该母岩浆高压分离结晶堆积的产物。
14.
Any of a group of igneous rocks composed mainly of olivine and various pyroxenes and having a granitelike texture.
橄榄岩含有大量橄榄石和各种辉石并有花岗岩状质地的岩石
15.
The olivine grains in the troctolite of the Upper Zone are rather short and thick.
上岩带橄长岩中的橄榄石颗粒相当短粗。
16.
Melt-Peridotite Reaction: Constraints on Spinel Compositional Variation from Mantle Xenoliths;
熔体与橄榄岩反应：对地幔包体中尖晶石成分变异的制约
17.
olivopontocerebellar atrophy
橄榄体脑桥小脑萎缩
18.
Serpentinite-is the least altered member of the peridotite suite.
蛇纹岩-是橄榄岩组蚀变最轻微的分子。