1. 气体的碳、氦同位素资料表明其来自岩浆体系;
C and O isotopic data demonstrate that these gases are derived from the felsic magma system;

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2. 在组分活性方面,镁铁组分比长英质组分的活动更为明显。
As to the activity of the components, the mafic component is more active than the felsic component.

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3. 矿床的成矿时间、空间及其成因与长英质次火山岩关系密切;
The metallogenic time, space and genesis of the ore deposit is related closely to felsicsubvolcanic rocks.

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4. 长英矿物早于黑云母和石榴子石结晶与岩浆侵位浅(结晶压力低)相关。
Earlier crystallization of felsic minerals than biotite and garnet is related with much lower crystallization pressure.

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5. 榴辉岩的主体围岩是长英质片麻岩,它与榴辉岩不是相同高压变作用的产物。
Both the eclogite and the felsic gneiss have not undergone the same high-pressure metamorphic event.

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6. 榴辉岩的主体围岩是长英质片麻岩,它与榴辉岩不是相同高压变作用的产物。
Both the eclogite and the felsic gneiss have not undergone the same high - pressure metamorphic event.

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7. 在东秦岭前寒武系变岩中,发育了许多Z字型叠加褶皱。它们是由近直立的片麻岩和长英质脉形成的。
Z-shaped superposed folds formed by nearly vertical gneiss and feldspar-quartz veins are widely developed in East Qinling Precambrian metamorphic rocks.

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8. 在东喜马拉雅构造结南迦巴瓦岩群中,石榴辉石岩呈透镜状产于麻粒岩相变长英质片麻岩和泥片岩之中。
Garnet pyroxenite occurs as lenses in granulite-facies metamorphic granitic gneiss and pelitic schist in the Namjagbarwa Group-complex of the eastern Himalayan tectonic syntaxis.

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9. 这类熔体参与变反应不仅受控于温压条件,而且与寄主岩石脱水熔融、长英质矿物部分熔融存在密切成因关系。
These reactions involving melt are not only controlled by PT conditions, but also genetically associated with dehydration melting, partial melting of felsic minerals in host rocks.

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10. 结果表明:宁村瓷石主要由长英质矿物组成,铁元素主要以硅酸盐矿物,硫化物和氧化物及氢氧化物等形式存在;
The results of composition analyses show that Ningcun china stone is mainly composed of quartz, sericite and feldspar; iron is contained in silicate, sulphide, oxide and hydroxide minerals.

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11. 石石云母片岩、石岩和大理岩的原岩为沉积岩,与副变长英质片麻岩和基性火山岩—起构成了古老的表壳岩组合。
The quartz-mica schist, quartzite and marble were metamorphosed sedimentary rocks, and, together with paragneiss and mafic rock, constituted the old supracrustal series.

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12. 泰山地区阜平期片麻岩由云闪片麻岩、奥花岗片麻岩组成,呈北西向带状分布,形成于角闪岩相温压环境,岩石普遍具片麻状构造,局部地区岩石的韧性作用比较强烈。
The Fuping-time gneiss in the Taishan area, consisting of tonalite gneiss and trondhjemite, formed in NW zonal distribution in the amphibolite -facies temperature and pressure environment.

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13. 的变种照例具有中等至伟晶的粒度。
Aplitic varieties are the rule, with the grain size ranging from medium to pegmatitic.

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14. 的变种照例具有中等至伟晶的粒度。
Aplitic varieties are the rule, with the grain size ranging from medium to pegmatitic.

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