gabbro的例句大全

The main rocks in the complex are gabbro, gabbro-diabase, pyroxenite and olivine-pyroxenite etc.

杂岩体主要岩石类型为:辉长岩 、 长辉绿岩 、 辉石岩、榄辉石岩等.

The main rocks in the complex are gabbro, gabbro diabase, pyroxenite and olivine-pyroxenite etc.

杂岩体主要岩石类型为:辉长岩 、 辉长辉绿岩 、 辉石岩、橄榄辉石岩等.

Even foliated metamorphic rocks and banded gabbro can be curved to form folds.

即使变质岩中的片理以及辉长岩中的条带也可产生弯曲而形成褶皱.

The micro-gabbro phase is indentical with the typical Bulawayan dolerite sills.

微辉长岩相与标准的布拉瓦约粒玄岩床相同.

Aim To date precisely the gabbro vein from Luohansi group and discuss its geological significance.

目的准确测定北秦岭罗汉寺岩群辉长岩脉的形成时代,探讨其地质意义.

The gabbro dikes are short.

辉长岩岩脉短.

The massive sulfide contains fragments of barren and mineralized gabbro, and schist.

块状硫化物中含有矿化的和未矿化的辉长岩及片岩碎块.

The former include ( quartz-) gabbro-norite, gabbro, gabbro-diabase ( porphyrite).

前者包括（石英）辉长苏长岩、辉长岩及辉长辉绿（玢）岩；

Mafic intrusive rocks in Wuqiagou area, eastern part of Ahai Orogenic belt, include diorite porphyrite, olivine gabbro cumulates, and hornblende gabbro cumulates.

阿尔泰造山带东段的乌恰沟地区发育大量镁铁质侵入岩（岩脉或小岩体），包括闪长玢岩和具堆积结构的角闪辉长岩和橄榄辉长岩。

The first intrusive phase which constitutes the main part of the complexes is best differentiated and has a differentiation trend, due to gravitative crystallization differentiation, from peridotite facies and olivine-gabbro, facies to quartz-bearing norite-gabbro facies with basicity decreasing successively.

第一侵入期构成岩体的主体部分，分异良好，由重力结晶分异形成自橄揽岩相、橄榄辉长岩相向含石英苏长辉长岩相的分异趋势，基性程度依次降低。

The Late Jurassic-Early Cretaceous activity produced basaltic and basaltic andesitic lavas ( 146Ma, 137Ma), followed by gabbro intrusion ( 135Ma) and aplite dyke ( 129Ma).

侏罗纪末～早白垩世初的火山活动除有熔岩（146Ma，137Ma）喷出外，还发育有辉长岩侵入体（135Ma）和辉绿岩岩墙（129Ma）等次火山岩。

Structural material peculiarities and evolution of gabbro anorthosite complexes of the Alden massif, south Russia

俄罗斯阿尔丹地块南部辉长-斜长岩杂岩体的构造-物质组分特点及其演化

The author used the chevron notched short-rod specimen for fracture toughness test suggested by ISRM in his experiment. The specimen is Kallax gabbro from Sweden with diameter of 71.4mm.

本实验研究采用国际岩石力学学会建议的V型切口短棒岩石断裂韧度试件，岩石为瑞典的卡莱克思（Kallax）辉长岩，试件直径为71.4mm。

These deposits were, when being formed, controlled by volcanic structures ( volcanic dome and volcanic breccia pipe), fault structures ( NE and NW trending), gabbro porphyrite body and depression in depression.

火山穹窿、爆发角砾岩筒等火山构造，NE向、NW向断裂构造，辉石闪长玢岩体，洼中洼环境等对成矿具有控制作用。