细碧岩是主要的含矿与容矿岩系。
矿石类型为蚀变细碧岩型和石英脉型。
Its ore types include altered spilite and pyrite quartz-sericite altered and quartz vein.
与深海相放射虫硅质岩相伴，则夹有玄武岩(细碧岩)层。
Thin basalt (spilite) layers are often interbedded in those deep Marine radiolaria-bearing siliceous rocks.
细碧—角斑岩系一般分为细碧岩、斑岩和石英角斑岩三类。
Spilite-keratophyre sequence is generally divided into spilite, keratophyre and quartz keratophyre.
细碧—角斑岩系一般分为细碧岩、角斑岩和石英角斑岩三类。
Spilite-keratophyre sequence is generally divided into spilite, keratophyre and quartz keratophyre.
主要由细碧岩、角斑岩及火山碎屑岩组成，其中有硅质岩、灰岩及碎屑岩夹层或凸镜体。
It mainly consists of spilite, keratophyre and volcanic clastics, intercalated with siliceous rocks, limestone and clastic rocks or lens.
对橄榄岩中单斜辉石和斜方辉石的组构分析表明，碧溪岭地区超基性岩经历了塑性变形，形成了LPO组构；
The fabric analysis of Cpx and Opx in peridotite indicates that the Bixiling ultra_basic rocks has experienced the ductile deformation, resulting in the LPO fabric.
碧口韧性剪切带沿康县—碾坝—麻子坝一带呈连续带状展布，发育于泥盆系及震旦系关家沟组上岩段内部。
Bikou ductile shear zone distributing along Kangxian county-Nianba-Maziba developed in the Devonian System and the upper Guanjiagou Formation of Sinian System.
岩石学和地球化学特征揭示包体寄主岩为碧玄岩，岩浆没有经历明显分异和同化混杂作用。
Their petrological and geochemical characters suggest that the host rock of the xenoliths is basanite, and the magma has not experienced obvious differentiation and assimilatory contamination.
云南马关地区分布有许多碧玄岩岩管，其中有些岩管含有地幔橄榄岩包体。
There exist a lot of Cpx-peridotitic xenoliths in basanites of Maguan, Yunnan Province.
郯庐断裂带中段的新生代火山岩以碱性系列的碱性橄榄玄武岩、碧玄岩和霞石岩为主，其中又以钠质亚系的岩石为主。
According to the main rock-forming minerals in them, the Cenozoic volcanic rocks are mainly alkali olivine basalt, basanite and nephelinite.
沿江有绮丽的象山、穿山、塔山、奇峰镇群峰、冠岩、画山、兴坪、碧莲峰等景点。
Elephant Hill, Chuanshan Hill, Pagoda Hill, Qifengzhen Peak forest, Crown Cave, Painted Cliff, Xingping Town and Grin Lotus Peak are the extraordinary scenic spots along the river.
并证实其原岩是与本区未变质的火山岩类相同的一套细碧-石英角斑岩系。
We con-firm that the original rocks are identical with the volcanic rocks in this area.
碧口群黄铁矿型铜金矿床产于前震旦纪古蛇绿岩套中。矿体受一定层位控制，分段集中，成群分布；
The pyrite type Cu-Au-deposit is located in the ophiolite suite of the Precambrian Bikou Group.
庐山南麓发育一套变 细碧-石英角 斑岩系火山 岩，岩性组合从早到晚反映了由基性到酸性的岩浆演化规律。
There develops a suit of meta-spilite baschtaunite system volcanic rocks in the south of Lushan Mountain. Lithology combination reflects the regularity of magma evolution from basic to acid.
庐山南麓发育一套变 细碧-石英角 斑岩系火山 岩，岩性组合从早到晚反映了由基性到酸性的岩浆演化规律。
There develops a suit of meta-spilite baschtaunite system volcanic rocks in the south of Lushan Mountain. Lithology combination reflects the regularity of magma evolution from basic to acid.
应用推荐