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magma相关的网络例句

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Cryptoexplosive rocks were formed at final stage of multiple phases of intrusion and volcanism of granitoid magma and therefore become the last carrier of ore-bearing magmatic hydrothemal solution.

由于隐爆岩在花岗岩类岩浆多期次侵入和火山作用的最后阶段形成,因而是含矿热液的最后载体。

The settling velocities of observed minerals in different magmas, which are estimated from Stocks' law, indicate that gravitative settle is impossible, especially in the acid magma.

然而,各种矿物在岩浆房中的沉降速度计算表明,尤其是酸性岩浆中,晶体的重力沉降是不可能的。

The mylonitized zone may be a passage for the basic melt derived from the bottom of the magma chamber, which has penetrated into the harzburgite.

斜辉辉橄岩顶部的糜稜岩化带可能是岩浆房底部基性熔体下渗的通道。

The three volcanics are of kalium alkaline series,with their chemical elements showing the same magma origin.

三种火山岩均属钾质钙碱性系列,岩石化学成分显示为同源岩浆产物。

Geological conditions of gold mineralization and ore-prospecting prognosis in Yuejiazhuang-Hutouya tectonic complex rock zone;2. Structure—magma control of gold mineralization in northwest sichuan;3. The result is that not only both of them were formed in the same tectonic setting,but also lamprophyre had an important mineral matter contribution to gold mineralization and are the marks for predicting gold deposits.

在详细的矿床地质、岩石地球化学和同位素年代学综合研究基础上,结合区域构造演化的特点,着重对金矿与煌斑岩的成因关系进行了剖析,认为戈枕含金剪切带煌斑岩与金矿不仅具有生成构造环境上的联系,而且对金成矿具有重要的物源贡献,是金矿找矿标志。

These results suggest that the diagenesis material of the Xiangshan volcanic intrusive complex was derived from crustal sources. The sources either had relatively lower maturity or had more juvenile mantle-derived igneous rocks than the exposed basement metamorphic rocks. Involvement of a small amount mantle-derived magma during the formation of the Xiangshan volcanic-intrusive complex was also possible. The diorite enclave, sub-quartzmonzonitic porphyry and lamprophyre were probably different mixing products between mantle and crust materals.

上述同位素示踪结果充分证实:相山火山-侵入杂岩的成岩物质主要为壳源,但与该区出露的基底变质岩相比,其物源区的成熟度相对较低或含有一定量的火成物质,并且不排除在其成岩过程中少量地幔物质的介入;闪长质包体、次石英二长斑岩及煌斑岩的成岩物质均含有一定量的地幔组分,可能为壳-幔混合作用的产物,只是受地壳物质混染的程度不同而已。

Type III is composed of latite and benmoreite, which are enriched in Al and Ti, with Na2O/K2O≥1.1 and no negative Eu anomaly (δEu=0.93–1.06), and Th/Ta and Ta/Hf ratios indicate a continental intraplate extensional environment. Its formation is probably related to underplating of basaltic magma.

第Ⅲ类由安粗岩,歪长粗面岩组成,富Ti,Al,Na2O/K2O≥1.1,Eu无异常(δEu=0.93~1.06),Th/Ta,Ta/Hf值显示大陆板内伸展环境,其形成可能与玄武质岩浆的底侵作用有关。

Longshan complex is located at the junction of Qinling and Qilian Orogen, and mainly distributed in Longshan Mountain, the west of Longxian County, which is separated from the Huluhe complex by the Baoping-Shanmen Fault to south, and connected with the Liupanshan Basin by the sub-fault to north. The upper magma is so extensive in this area that only Longshan complex is left as lentoid.

陇山杂岩地处秦岭—祁连造山带的结合部位,主体分布于陇县以西陇山山脉内,南以保平—山门韧性断裂带与葫芦河群相隔,向北与六盘山白垩纪沉积盆地以基底断层形式相接触,被后期火山岩体吞没,呈不连续透镜体状展布。

All of these characteristics are in contrast with their host rock_serpentinite and show that the leucocratic rocks were produced by crystallization differentiation of ultramafic magma.

这些特征表明,浅色岩是幔源超基性岩浆晚期结晶分异的产物。

All of these characteristics are in contrast with their host rock_serpentinite and show that the leucocratic rocks were produced by crystallization differentiation of ultramafic magma.

这些特征表明,浅地是幔源超基性岩浆晚期结晶分异的产物。

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