矾山岩体是一环状碱性超镁铁杂岩体。
There is a kali-alkaline ultramafic complex in the Fanshan of Hebei.
金矿床的形成与碱性杂岩体密切相关。
The Dongping super large gold deposit has close relation with the Shuiquangou alkalic complex.
刘家坪杂岩体出露于扬子准地台西北边缘。
The Liujiaping complex occurs on the northwest margin of the Yangzi paraplatform.
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。
The chromite deposits in the muskox complex occur only in feldspathic peridotite .
根据其地质特征并结合其他资料，可将其解体为三个杂岩体。
Based on its geological characteristics and other information, it can be subdivided into three complex bodies.
东坪金矿床赋存于水泉沟碱性杂岩体与老地层的内接触带上。
Dongping gold deposit occurs in the internal contact belt between Shuiquangou alkali mixtite and old layers.
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。
The chromite deposits in the muskox complex occur only in feldspathic peridotite.
玉华山岩体是一个高位复式深成杂岩体，具成分和结构演化序列。
The Yuhuashan rock body in Jiangxi is a high-level composite plutonic complex, which has compositional and structual evolutiOnary sequences.
超基性岩与塞巴奎沉积岩岩片相间构成一巨大的构造岩片的杂岩体。
The ultrabasic rocks form a complex of large tectonic slices with intercalated slices of Sebakwian sedimentary rocks.
形成于中晚元古代的彭灌杂岩体构造侵位于映秀断裂和茂汶断裂之间。
Pengguan complex formed in Meso-and Neoproterozoic was at tectonic emplacement between the Yinxiu fault and the Maowen fault.
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。
The main rocks in the complex are gabbro, gabbro-diabase, pyroxenite and olivine-pyroxenite etc.
形成于中——晚元古代的彭灌杂岩体构造侵位于映秀断裂和茂汶断裂之间。
Pengguan complex formed in Meso-and Neoproterozoic was in tectonic emplacement between the Yinxiu fault and the Maowen fault.
赣东北横峰县港边岩体是我国罕见的能在填图尺度上表示的岩浆混合杂岩体。
The Gangbian magma mixed complex from northeastern Jiangxi Province is an important constitute in the Late Proterozoic magma mixed zone in the southeastern margin of the Paleo Yangtz continent.
位于冀西北张家口-宣化地区的转枝莲辉石闪长岩侵入水泉沟正长岩杂岩体中。
The Zhuanzhilian pyroxene diorite is found in Zhangjiakou-Xuanhua area, northwest of Hebei Province.
超镁铁质侵入杂岩体由纯橄岩，橄榄岩，辉石岩，辉长岩及它们的变质产物组成。
The ultramafic intrusive complex is composed of dunite, peridotite, pyroxenite, gabbro and their metamorphic products.
水晶屯金矿床位于张宣幔枝构造轴部，水泉沟—大南山碱性角闪二长岩杂岩体的西缘。
Shuijingtun gold deposit is located in the central axis of the Zhanjiakou-Xuanhua mantle branch and in the west of alkaline hornblende monzonite in the area of Shuiquangou-Dananshan in Zhangjiakou.
布格重力异常图与地质图的对比表明，本区的局部重力异常主要是由玲珑花岗质杂岩体引起的。
Comparison of the Bouguer gravity anomaly map with geological map shows that the local negative gravity anomaly is caused by the Linglong granitic complex.
矾山岩体为一偏碱性超镁铁岩-正长岩杂岩体，其中蕴藏着中国北方最大的岩浆型磷灰石矿床。
Fanshan intrusive body is a complex body of meta-alkaline ultramafic rock-syenite. It hosts the biggest magmatic apatite deposit in north China.
大别山杂岩是由早期的沉积地层和不同期次、不同类型的岩浆岩以及构造岩片所组成的杂岩体。
The Dabieshan Group is a complex composed of early formed sedimentary rocks, magmatic rocks of varying ages and types and tectonic slices.
阿尔金南缘断裂是一条深达上地幔的区域性大断裂，沿断裂分布着众多的基性-超基性杂岩体。
The south margin faulted zone of Altun Mountain in Xinjiang is a regional upper mantle deep structure, along which numerous basic ultrabasic complex bodies are distributed.
北峪奥长花岗岩 （体 ）位于中条裂谷的西部 ，和霏细斑岩及辉长岩组成侵入杂岩体 ，呈南北向展布。
The Beiyu trondhjemite, together with felsite porphyry and gabbro, forms an intrusive complex extending S-N in the western part of the Zhongtiao rift.
山西狐偃山碱性偏碱性杂岩体出露于吕梁山东翼中段，由于其典型的碱性岩岩石类型一直受到地学界的关注。
The Hanshan alkaline complex outcrops in the middle part on the eastern wing of the Lüliang Mountain, Shanxi Province.
佛冈花岗杂岩体是南岭地区最大的晚中生代岩基，乌石闪长岩角闪辉长岩是佛冈钙碱性系列花岗岩中最基性的端员。
The Fogang granitoid complex is the largest Late Mesozoic batholith in Nanling region, and the Wushi diorite-hornblende gabbros are the most basic end-member of Fogang calc-alkaline series rocks.
赣东北前寒武纪港边火成杂岩体广泛发育不同类型的矿物间不平衡结构，指示该杂岩体曾发生过广泛的岩浆混合作用。
There are various lopsided texture types among minerals, indicating extensive magma mixing in the Precambrian Gangbian magma-mixed complex from northeastern Jiangxi Province.
摘要赣东北前寒武纪港边火成杂岩体广泛发育不同类型的矿物间不平衡结构，指示该杂岩体曾发生过广泛的岩浆混合作用。
There are various lopsided texture types among minerals, indicating extensive magma mixing in the Precambrian Gangbian magma-mixed complex from northeastern Jiangxi Province.
本文通过对杂岩体的成因、成岩时代、岩石类型以及岩体的含金性和部分同位素的特征分析，探讨了岩体与矿床的成岩关系。
Based on researching of the age, rock types genesis, gold content and the stable isotope composition of the complex, the relation between the deposit and the complex is discussed.
根据胶东地区西北部的重力资料，并在地质资料的约束下，采用人-机联作的二维模拟方法，对玲珑花岗质杂岩体三维形态进行了细致的推断。
Inference of the three_dimensional geometry of the Linglong granitic complex at depth from 2_d gravity forward modeling, constrained by geological data, Shandong Province, East China, is presented.
矾山杂岩体由三期侵入岩和脉岩组成 ，矿床产于第一期侵入岩中。第一期侵入岩较其它期次侵入岩REE含量高 ，按辉石岩—黑云母辉石岩—磷灰石岩的顺序增加。
The Fanshan complex is made up of three phases of intrusive and dike rocks of which the first phase of intrusive rock developed the deposit, perhaps owing to more REE volume than the other phases.
研究区磁性体较发育，这些磁性体分布范围与地表出露的侵入岩、蛇绿杂岩及火山堆有很好的对应关系。
The magnetic body developed in the study area, the distribution of them and surface outcrops intrusive rocks, ophiolite and volcanic pile has a good correspondence.
研究区磁性体较发育，这些磁性体分布范围与地表出露的侵入岩、蛇绿杂岩及火山堆有很好的对应关系。
The magnetic body developed in the study area, the distribution of them and surface outcrops intrusive rocks, ophiolite and volcanic pile has a good correspondence.
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