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xenolith相关的网络例句

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与 xenolith 相关的网络例句 [注:此内容来源于网络,仅供参考]

Based on classification norms proposed by Menzies (1983), the ultramafic xenoliths in the present study belong to I-type xenolith .

根据Menzies(1983)之分类标准,区内超基性捕获岩内橄榄岩属於Ⅰ型捕获岩,Fo 值介於90.1892.18 之间。

Fluid composition ; alkali basalt ; Iherzolite xenolith ; eastern China

流体组分;碱性玄武岩;二辉橄榄岩捕虏体;中国东部

According to the macro-characteristics and distribution law of dioritic microgranular enclaves, the special texture and structure, the contrast between the main rock-forming minerals of dioritic microgranular enclave and the host rock, as well as the genesis analysis on double crystal type percentage of 6 187 plagioclase, the conclusion is drawn as follows: despite the variety of the genesis types of dioritic microgranular enclave in Fangshan granodiorite, most of the genesis type is probably the result of the xenolith metamorphic transformation.

根据闪长质微粒包体的宏观特征及分布规律、特殊的结构构造、主要造岩矿物与寄主岩的对比以及6187个斜长石双晶类型百分率的成因分析得出,房山花岗闪长岩体中的闪长质微粒包体尽管有多种成因,但有不少可能是捕虏岩包体变质改造的结果。

Based on the study of correlativity of Ol-Opx-Cpx contents in North China and South China, it shows that some peridotite xenoliths from Hannuoba, Pingquan, Nvshan, Puning, Qiongbei, and Niutoushan area may represent the older mantle material compositions, and some peridotite xenolith from Ximeng, Penglai, Linqu, Quzhou, Mingxi, and Liuhe area may represent the younger mantle material compositions.

通过对华北、华南两区橄榄岩包体中的O1与Opx及Cpx的相关关系的分析研究认为,华北汉诺坝和平泉地区,以及华南女山、普宁、琼北、牛头山等地区的部分橄榄岩包体,代表了老地幔;锡盟、蓬莱、临朐及衢州、明溪、六合等地区的部分橄榄岩包体代表了较新地幔。

During the magmas ascendedand intruded, the high-energy, quick ascending primary mantle magmas with xenolith andhigh-pressure megacrysts didn't react with the crustal matter, which formed products, such ascone sheets.

在岩浆上升侵位的过程中,能量高的快速上升的含有岩石包体和高压巨晶的幔源原生岩浆没有与地壳物质发生作用,其形成的产物如锥状岩席;在此之后,岩浆能量、上升速度的降低促使原生岩浆与围岩发生轻微的同化混染作用,其产物如火山熔岩和火山颈。

The Chengzihe Formation in Zhangxin area of Jixi basin,Heilongjiang Province is intruded by the algorite sill. The mafic rocks are pure, porphyritic and contain no xenolith.

黑龙江省鸡西盆地张新地区辉绿玢岩呈岩床状侵入晚中生代城子河组地层中;辉绿玢岩较纯净,无捕虏体,呈斑状结构,斑晶由普通辉石、斜长石组成,斑晶体积分数为35%~40%;基质由微晶斜长石、辉石、磁铁矿及玻璃质组成。

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