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dioritic相关的网络例句

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与 dioritic 相关的网络例句 [注:此内容来源于网络,仅供参考]

This paper reports a garnetbearing dioritic porphyry,which was first recognized in east Kunlun,NW China.

本文报道在东昆仑地区发现的一种较为稀少的含石榴石英云闪长玢岩,这也是此类岩石在中国的首次发现。

In trace elements, both the dioritic enclaves and hosting granite are enriched in LILEs and HFSEs.

在微量元素方面,包体和寄主花岗岩都富含大离子亲石元素和高场强元素。

These dioritic enclaves and their host granite are different in mineral association, but species of the same mineral within them are similar to each other.

闪长质包体与寄主花岗岩在矿物组合上不同,但两者中同类矿物的种属相似。

Dioritic magmatic enclaves have been discovered in the subvolcanic ring dikes for the first time by this study. These enclaves have typical back-vein and quenched margin where there are a lot of needle-like apatites.

首次在相山北部次火山岩岩墙中发现的辉石闪长质岩浆包体,具有典型的反向脉及淬冷边,其淬冷边内含有大量的针状磷灰石。

Zircon LA-ICP-MS U-Pb dating gave ages of 301±1 Ma and 298±2 Ma for the dioritic enclaves and their host granite, respectively, indicating their Early Permian emplacement.

锆石LA-ICP-MS U-Pb年龄显示闪长质包体与寄主花岗岩在形成时间上非常接近(分别为301±1Ma和298±2 Ma),表明两者均形成于早二叠世。

In comparison with the host granite, the dioritic enclaves are higher in Fe, Mg, Ti, Ca and richer in HREE, Sr, but lower in Na, K, Si and poorer in Ba, Th, Hf, Zr.

与寄主花岗岩相比,闪长质包体的Fe、Mg、Ti、Ca含量较高,而Na、K、Si的含量较低;富HREE、Sr,贫Ba、Th、Hf 、Zr。

Luanping orbicular dioritic pluton has special geochemical characteristics with unusual enrichment in Al 2 O 3 (21.58%~26.80%)and relative poorness of K 2 O(0.35%~1.87%).

滦平球状闪长岩体具有特殊的地球化学性质,其中最显著的岩石化学特征表现为高度富Al2O3(21.58%~26.80%)而相对贫K2O(0.35%~1.87%)。

Therefore , the quenched dioritic enclaves in subvolcanic granodiorite in Xiangshan were formed by the convection of the magma with different composition and temperature and by the heterogeneous mingling between them. These enclaves are genetically quenched enclaves.

因此,相山潜火山岩岩墙中的闪长质岩石包体是不同成分、不同温度的岩浆经对流及不均一岩浆混合作用而形成,在成因类型上属淬冷包体。

As for sulfur isotopic composition, the general feature of two types deposits is a single peak distribution. All δ〓s values of the ores are near zero. The difference of different deposits lies in that the δ〓s values (1. 8-5. 2‰) of LDT are of small positive value and are similar to that of the metamorphic rocks and dioritic porphyrites in the region while the δ〓s values of SDT are always near zero. Features above suggest that two types of deposits have closely genetic relationship to metamorphic and magmatic rocks.

硫同位素组成上,两类金矿床共同的特征是均具有明显的单峰塔式效应,且δ〓S值均位于0值附近不大的变化范围内;不同的是,近程式金矿的δ〓S平均值均接近于0,与该类金矿具密切成因联系的岩体的δ〓S值也接近于0值,而远程式金矿的δ〓S平均值均为小的正值,变化范围为1.8~5.2‰,区内太古代变质岩及矿区内闪长玢岩脉的全岩δ〓S值位于这一区间内,反映了远程式金矿床其成矿物质不仅来源于重熔岩浆,同时还可能部分来源于变质岩围岩。

It is suggested that the dioritic enclaves and their host granite were derived from the same parental magma that resulted from partial melting of the Neoprot-erozoic depleted-mantle-sourced juvenile crust.

综合岩石学、地球化学和同位素等方面的对比研究,笔者认为八大石闪长质包体属于同源包体,为寄主花岗岩同源母岩浆经结晶分异作用形成的早期产物

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