granophyre

简明释义

英[ˈɡrænəʊˌfaɪə]美[ˈɡrænəˌfaɪr]

[岩] 花斑岩

[岩] 文象斑岩

英英释义

单词用法

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例句

1.Nanliang complex is mainly composed of porphyritic granite, granophyre, rhyolite - porphyry and rhyolitic agmatite-lava.

南梁岩体主要由斑状花岗岩、流纹斑岩、花斑岩及流纹质角砾熔岩组成。

2.Nanliang complex is mainly composed of porphyritic granite, granophyre, rhyolite - porphyry and rhyolitic agmatite-lava.

南梁岩体主要由斑状花岗岩、流纹斑岩、花斑岩及流纹质角砾熔岩组成。

3.In the petrology course, we studied the characteristics of granophyre and its formation process.

在岩石学课程中，我们研究了花岗岩流的特征及其形成过程。

4.During our field trip, we collected samples of granophyre for further analysis in the lab.

在我们的实地考察中，我们收集了花岗岩流样本，以便在实验室进行进一步分析。

5.The geological survey revealed that the region is predominantly composed of granophyre, a fine-grained igneous rock.

地质调查显示，该地区主要由花岗岩流组成，这是一种细粒的火成岩。

6.The presence of granophyre in the area indicates significant volcanic activity in the past.

该地区存在花岗岩流表明过去有显著的火山活动。

7.The unique texture of granophyre makes it a topic of interest for many geologists.

独特的花岗岩流纹理使其成为许多地质学家的研究兴趣所在。

作文

Granophyre is a fascinating type of igneous rock that has intrigued geologists and rock enthusiasts alike. This unique rock formation is characterized by its distinct texture, which is a result of the cooling process of magma. Unlike other volcanic rocks, granophyre (花岗岩质火成岩) exhibits a fine-grained matrix that contains larger crystals, giving it a granular appearance. The presence of quartz and feldspar in its composition contributes to its unique aesthetic and geological significance.The formation of granophyre occurs when magma cools slowly beneath the Earth's surface, allowing for the crystallization of minerals. This slow cooling process is what differentiates granophyre from other volcanic rocks such as basalt, which cools rapidly on the surface. As a result, the mineral grains in granophyre can grow larger, leading to the rock's characteristic texture. This makes it not only visually appealing but also an important subject of study for understanding the processes of igneous rock formation.One notable feature of granophyre is its occurrence in various geological settings. It is often found in areas where there has been significant volcanic activity, particularly in regions with a history of granitic intrusions. For instance, in parts of Iceland and Scotland, granophyre can be observed in the formations that were once part of ancient volcanic systems. These locations provide valuable insights into the geological history of the Earth and the processes that shaped its crust.In addition to its geological significance, granophyre also holds economic value. Due to its durability and aesthetic appeal, it is sometimes used as a decorative stone in construction and landscaping. The unique colors and textures of granophyre make it a popular choice for countertops, flooring, and outdoor features. This practical application highlights the intersection of geology and everyday life, demonstrating how natural materials can enhance our surroundings.Moreover, studying granophyre can help scientists understand the conditions under which it formed. By analyzing the mineral composition and texture of granophyre, researchers can infer the temperature and pressure conditions present during its formation. This information is crucial for piecing together the history of volcanic activity in a given area and can aid in predicting future geological events.In conclusion, granophyre is more than just a rock; it is a window into the Earth's geological past. Its unique formation process, aesthetic qualities, and economic value make it a subject of interest for both scientists and the general public. As we continue to explore and study granophyre, we deepen our understanding of the dynamic processes that shape our planet and the materials that contribute to its diverse landscapes. Whether you are a geologist, a rock collector, or simply someone who appreciates the beauty of nature, granophyre offers a rich tapestry of knowledge waiting to be uncovered.

花岗岩质火成岩是一种引人入胜的火成岩类型，吸引了地质学家和岩石爱好者的关注。这种独特的岩石形成以其独特的纹理为特征，这种纹理是由于岩浆的冷却过程而形成的。与其他火山岩不同，granophyre（花岗岩质火成岩）表现出细粒基质，含有较大的晶体，赋予其颗粒状外观。石英和长石的存在使其具有独特的美学和地质意义。granophyre的形成发生在岩浆缓慢冷却于地球表面以下时，允许矿物结晶。这一缓慢冷却过程使granophyre与其他火山岩如玄武岩区分开来，后者在表面迅速冷却。因此，granophyre中的矿物颗粒可以长得更大，导致岩石的特征纹理。这不仅使其在视觉上吸引人，而且也是研究火成岩形成过程的重要课题。granophyre的一个显著特征是它在各种地质环境中的出现。它通常发现于有显著火山活动的地区，尤其是在有花岗岩侵入历史的区域。例如，在冰岛和苏格兰的部分地区，可以观察到曾经是古代火山系统一部分的granophyre。这些地点为了解地球的地质历史以及塑造其地壳的过程提供了宝贵的见解。除了地质意义外，granophyre还具有经济价值。由于其耐用性和美学吸引力，有时被用作建筑和景观设计中的装饰石材。granophyre独特的颜色和纹理使其成为台面、地板和户外设施的热门选择。这种实际应用突显了地质学与日常生活的交集，展示了自然材料如何增强我们的环境。此外，研究granophyre可以帮助科学家了解其形成的条件。通过分析granophyre的矿物成分和纹理，研究人员可以推断出形成过程中的温度和压力条件。这些信息对于拼凑特定区域火山活动的历史至关重要，并且可以帮助预测未来的地质事件。总之，granophyre不仅仅是一块岩石；它是通往地球地质过去的一扇窗。其独特的形成过程、美学特性和经济价值使其成为科学家和公众都感兴趣的主题。随着我们继续探索和研究granophyre，我们加深了对塑造我们星球的动态过程和构成其多样化景观的材料的理解。无论你是地质学家、岩石收藏者，还是仅仅欣赏自然之美的人，granophyre都提供了一幅等待被揭开的丰富知识画卷。