calcic plagioclase
简明释义
钙质斜长石;
英英释义
Calcic plagioclase is a member of the plagioclase feldspar mineral series that is rich in calcium and typically found in igneous rocks. | 钙质斜长石是斜长石矿物系列的一员,富含钙,通常在火成岩中发现。 |
例句
1.The identification of calcic plagioclase can help geologists infer the cooling history of magma.
识别钙质斜长石可以帮助地质学家推断岩浆的冷却历史。
2.Geologists often analyze calcic plagioclase in volcanic rocks to determine their mineral composition.
地质学家通常分析火山岩中的钙质斜长石以确定其矿物成分。
3.In the study of igneous rocks, calcic plagioclase is often compared with other feldspar minerals.
在火成岩的研究中,钙质斜长石常常与其他长石矿物进行比较。
4.The rock sample contained significant amounts of calcic plagioclase, which is essential for understanding its formation.
岩石样本中含有大量的钙质斜长石,这对于理解其形成至关重要。
5.The presence of calcic plagioclase indicates that the rock was formed under high-temperature conditions.
存在钙质斜长石表明该岩石是在高温条件下形成的。
作文
In the field of geology, understanding the composition of rocks is essential for unraveling the history of our planet. One significant component that geologists often encounter is calcic plagioclase (钙质斜长石), a member of the plagioclase feldspar group. This mineral plays a crucial role in the formation of igneous rocks and can provide insights into the conditions under which these rocks were formed. Calcic plagioclase is characterized by its high calcium content compared to sodium, which distinguishes it from other plagioclase varieties. It typically forms in environments with high-temperature conditions, such as those found in volcanic eruptions or deep within the Earth's crust.The presence of calcic plagioclase in a rock sample can indicate specific geological processes. For instance, when magma cools, the minerals crystallize in a particular order based on their melting points. Calcic plagioclase usually crystallizes early in this process, often alongside minerals like olivine and pyroxene. This early crystallization is critical because it affects the overall texture and mineralogy of the resulting rock.Furthermore, the study of calcic plagioclase can reveal information about the temperature and pressure conditions during rock formation. By examining the composition of this mineral, geologists can infer the depth at which the rock formed and the tectonic settings involved. For example, a high concentration of calcic plagioclase might suggest that the rock originated from a subduction zone, where oceanic plates are forced beneath continental plates, leading to the formation of magma rich in calcium.In addition to its geological significance, calcic plagioclase has practical applications in various industries. For instance, it is utilized in the manufacturing of ceramics and glass, where its properties contribute to the durability and aesthetic qualities of the final products. The mining and processing of calcic plagioclase also support local economies, particularly in regions with abundant geological resources.Moreover, understanding the environmental implications of calcic plagioclase is becoming increasingly important. As we face global challenges such as climate change and resource depletion, studying minerals like calcic plagioclase can help us develop sustainable practices in mining and material usage. By recognizing the value of this mineral in both geological and industrial contexts, we can better appreciate its role in our planet's system.In conclusion, calcic plagioclase (钙质斜长石) is more than just a mineral; it is a key player in the geological narrative of Earth. Its formation, characteristics, and applications provide valuable insights into both the natural world and human industry. As we continue to explore and understand the complexities of our planet, calcic plagioclase will undoubtedly remain a focal point of study for geologists and researchers alike.
在地质学领域,理解岩石的成分对于揭示我们星球的历史至关重要。地质学家经常遇到的一个重要成分是钙质斜长石(calcic plagioclase),它是斜长石长石组的一个成员。这种矿物在火成岩的形成中发挥着关键作用,并且可以提供关于这些岩石形成条件的见解。钙质斜长石的特点是其相对于钠的高钙含量,这使其与其他斜长石种类区分开来。它通常在高温条件下形成,例如火山喷发或地球深处的环境。在岩石样本中出现钙质斜长石可能表明特定的地质过程。例如,当岩浆冷却时,矿物根据其熔点以特定顺序结晶。钙质斜长石通常在这个过程中早期结晶,通常与橄榄石和辉石等矿物同时出现。这种早期结晶非常关键,因为它影响了最终岩石的整体纹理和矿物组成。此外,研究钙质斜长石可以揭示岩石形成期间的温度和压力条件。通过检查这种矿物的成分,地质学家可以推断出岩石形成的深度和涉及的构造背景。例如,高浓度的钙质斜长石可能表明该岩石起源于俯冲带,在那里,海洋板块被迫潜入大陆板块之下,从而导致富含钙的岩浆的形成。除了其地质意义外,钙质斜长石在各个行业中的实际应用也越来越受到重视。例如,它被用于陶瓷和玻璃的制造,其中其特性有助于最终产品的耐用性和美观性。钙质斜长石的开采和加工也支持了当地经济,特别是在资源丰富的地区。此外,了解钙质斜长石的环境影响变得越来越重要。随着我们面临气候变化和资源枯竭等全球挑战,研究像钙质斜长石这样的矿物可以帮助我们制定可持续的采矿和材料使用实践。通过认识到这种矿物在地质和工业背景中的价值,我们可以更好地欣赏它在我们星球系统中的角色。总之,钙质斜长石(calcic plagioclase)不仅仅是一种矿物;它是地球地质叙事中的关键角色。其形成、特征和应用为自然世界和人类工业提供了宝贵的见解。随着我们继续探索和理解我们星球的复杂性,钙质斜长石无疑将继续成为地质学家和研究人员研究的重点。
相关单词