biotite granite的例句大全

On a relatively closed condition, granite often forms plaque biotite granite and fine-grained biotite granite.

在处于相对封闭条件下的花岗岩往往形成含斑黑云母花岗岩、细粒黑云母花岗岩等。

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Detailed petrologic, geochemical and Sr-Nd-Hf-U-Pb isotopic researches indicate that the Wuping granitic complex consist mainly of biotite granite and garnet-bearing granite with different formation age and petrogenesis.

岩石学、元素地球化学和Sr-Nd-Hf-U-Pb同位素的综合研究显示，武平花岗质杂岩体是由形成时代和成因不同的黑云母花岗岩和含石榴子石花岗岩组成。

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Granites belong to S-type granite, but the biotite granite was affected by the mantle or mantle fluid.

黑云母花岗岩是壳源花岗岩但又受到幔源岩浆或幔源流体的影响。

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The uranium in the ore-forming hydrothermal fluids was mainly active uranium derived from the muscovite granite which was either a primary rock body or formed through autometamorphism of a biotite granite;

成矿热液中的铀主要取自自云母花岗岩中的活性铀；

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The ore-forming material came from biotite-granite of Hangou.

成矿物质来自韩沟黑云母花岗岩体.

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Pb-Zn mineralization in the studying area is usually related to adamellite, and Fe-Cu mineralization to biotite granite, while Cu mineralization to diorite or diorite porphyrite.

铅、锌矿化多与二长花岗岩有关，铁铜矿化多与黑云母花岗岩关系密切，而铜矿化多与闪长岩（或闪长玢岩）有关。

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Study on Recovery of RE from Elution Deposit Ore in Weathering Crust of Biotite Granite

从黑云母花岗岩风化壳淋积型稀土矿中回收稀土问题的研究

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The copper ( molybdenum) ore bodies are mainly situated in or out of the contact zone between the mineralized porphyry bodies and the biotite granite porphyry.

铜（钼）矿（化）体主要产于含矿斑岩体和黑云母花岗斑岩的内外接触带中。

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Main ore minerals are uraninite and coffinite. Uranium mineralization is mainly present in the biotite-concentrated site within pegmatoid granite and at the contact between pegmatoid granite dykes and biotite plagiogneiss.

主要矿石矿物为晶质铀矿、铀石，铀矿化主要富集在伟晶状花岗岩内黑云母集中区、伟晶状花岗岩脉与黑云母斜长片麻岩接触带处。

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So the dark mica in this granite should be called biotite.

那么.在这块花岗岩中的黑色云母类矿物就应当叫做黑云母了。

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Early Yanshanian intrusions are mainly adamellite, biotite K feldspar granite with small amount of granodiorite.

燕山早期侵入岩以二长花岗岩 、 黑云钾长花岗岩为主,其次为花岗闪长岩.

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The second stage is the intrusion of medium to fine-grained biotite-K-feldspar granite.

第二阶段为中细粒黑云母钾长化岗岩。

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The variation of K Ar ages of the biotite in granite reflects the rising and cooling history or the intrusive during the orogenic period.

造山期花岗岩黑云母K-Ar年龄的变化是岩体隆起，冷却史的反映。

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