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Late Yanshanian, plutonic monzonite granites causes molybdenum and tungsten mineralization .

燕山晚期形成的位于区内东北部的中—深成相二长花岗岩成矿作用主要为斑岩型钨钼矿。

The exports of blocks and slabs of granites and quartzites reached US$ 178 million and 905000 tons, a negative variation of 11,8% and 24,19%, respectively, as compared to 2007, and consisting of 18,65% of the total sales and 45,54% of the physical volume of the exports of the sector.

而花岗岩和硅岩的荒料和大板出口达1亿7800万美元,出口量达90万5000吨分别比2007年下降了11.8%和24.19%,并且占2008年出口总金额的18.65%和出口总量的45.54%。

The biotite granites were not directly derived from depleted mantle, but were probably the products of partial melting and crystallization differentiation of deep-buried young crustal materials derived from the mantle.

这些黑云母花岗岩不是直接来源于亏损地幔,而更可能是源自地幔且被深埋的年轻地壳物质部分熔融和结晶分异作用的产物。

The study on the chronology, geochemistry and zircon Hf isotopes of the Zhuangzili and Mopanshan K-feldspar granites in Bengbu uplift was carried out in order to constrain their petrogenesis.

对蚌埠隆起区庄子里和磨盘山钾长花岗岩进行了系统的年代学和地球化学以及锆石Hf同位素的研究,以便对其岩石成因进行约束。

Plentiful Phanerozoic granites distribute extensively in this region, occupied an area of about 100000km〓, the 80 percent of the total area of exposed geologic bodies.

在该区广泛分布着大量的显生宙花岗岩,出露面积约100000Km〓,占出露地质体总面积的80%左右。

Massive Phanerozoic granites distribute extensively in this region, and occupy an area about 20000km〓, about 80 percent of the total area of exposed geologic bodies.

区内分布有大面积的显生宙花岗岩,出露面积达20000km〓,约占出露地质体总面积的70-80%。

The basal continental crust of Tarim-Tianshan area in Xinjiang consists of the continental nucleus, which is composed of grey gneisses, greenstones, and potass granites similar to charnockites, and its accretionary belts mainly of the early Proterozoic and partly the Middle Proterozoic.

塔里木-天山地区基底陆壳由太古宙灰色片麻岩、绿岩和可能是紫苏花岗岩的含钾花岗岩类组成的陆核及其古元古代和少量中元古代增生带组成。

The results of 118 REE analyses of Li-F granites from South China and other countries indicate that there are three variation ty pes of REE model curves with the different evolution from early to late stages of Li-F grantie complex or from lower to upper petrofacies of the Li-F granite body, which are (1) decreasing,(2) increasing and (3) saltatory variation types. The first variation type is called positive evolution type, which is the production of crystallization differentiation.

华南和其他国家典型Li-F花岗岩的118个稀土分析研究表明,随Li-F花岗岩由早至晚阶段或自下而上不同岩相演化,稀土模式曲线有三种变化类型:①降低变化,②升高变化,③突然变化等类型。

Therefore, the indicatrixes of the liquid segregation mainly with immiscibility are the saltatory variation type of REE model evolution and the sep arative feature of main-evolution trend line either with sub-evolution trend line or with composition point of Li-F granites in the diagrams of REE-n and La/Sm-La.

因此,不混溶为主的液态分离标志是稀土模式演化突变类型和Li-F花岗岩在REE -n、La/Sm-La图解中主演化方向线与次演化方向线或与成分点呈分离特点。

In Yanbian area, high-alumina granites such as Dongqing and Weizigou rock were considered as typical Stype granite and represented the collision of Jiamusi Massif and North China Craton because of the mineral assemblage of garnet and muscovite.

在延边地区,以东清和苇子沟岩体为代表的高铝花岗岩,因其含有石榴石和白云母矿物组合,曾被认为是典型的S型花岗岩,且代表了佳木斯和华北地台的碰撞拼合。

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