orthopyroxene

简明释义

英[ˌɔrθoʊˈpaɪrəˌziːn]美[ˌɔrθoʊˈpaɪrəˌziːn]

n. [矿物] 斜方辉石类

英英释义

单词用法

同义词

反义词

例句

1.According to the study of olivine and peridotite anisotropy and the mineral compositions in the peridotite, the orthopyroxene can reduce the overall effect of the anisotropy.

橄榄石、橄榄岩地震波各向异性与橄榄岩中矿物含量的研究，定量的说明了斜方辉石的效果是降低总体的各向异性。

2.According to the study of olivine and peridotite anisotropy and the mineral compositions in the peridotite, the orthopyroxene can reduce the overall effect of the anisotropy.

橄榄石、橄榄岩地震波各向异性与橄榄岩中矿物含量的研究，定量的说明了斜方辉石的效果是降低总体的各向异性。

3.The major rock forming minerals include olivine, orthopyroxene, clinopyroxene, plagioclase and amphibole.

其主要造岩矿物为橄榄石、斜方辉石、单斜辉石、斜长石和角闪石。

4.The geologist identified the mineral as orthopyroxene (正辉石) during the field study.

在实地研究中，地质学家将该矿物鉴定为orthopyroxene（正辉石）。

5.In metamorphic rocks, orthopyroxene (正辉石) can indicate high-temperature conditions.

在变质岩中，orthopyroxene（正辉石）可以指示高温条件。

6.The presence of orthopyroxene (正辉石) in the sample suggests a basaltic origin.

样本中存在orthopyroxene（正辉石）表明其源于玄武岩。

7.Researchers studied the orthopyroxene (正辉石) crystals to understand the cooling history of the magma.

研究人员研究了orthopyroxene（正辉石）晶体，以了解岩浆的冷却历史。

8.The mineral composition includes orthopyroxene (正辉石), which plays a crucial role in rock classification.

矿物成分包括orthopyroxene（正辉石），在岩石分类中起着至关重要的作用。

作文

The study of minerals is essential in understanding the Earth's composition and the processes that shape our planet. Among these minerals, orthopyroxene (正交辉石) plays a significant role in igneous and metamorphic rocks. It is a common mineral found in many types of rocks, particularly in those formed from high-temperature environments. Understanding orthopyroxene is crucial for geologists as it provides insights into the conditions under which certain rocks were formed. Orthopyroxene is a member of the pyroxene group of minerals, which are characterized by their unique crystal structures and compositions. This mineral typically contains magnesium and iron, and its chemical formula can vary depending on the specific type of orthopyroxene. The presence of orthopyroxene in a rock can indicate the temperature and pressure conditions during the rock's formation. For instance, rocks containing high amounts of orthopyroxene often form in environments where temperatures exceed 1000 degrees Celsius. In addition to its geological significance, orthopyroxene also has practical applications. For example, it is used in the manufacturing of ceramics and refractory materials due to its high melting point and durability. The study of orthopyroxene can also help scientists understand tectonic processes, as this mineral is commonly found in the upper mantle of the Earth. By analyzing the composition and distribution of orthopyroxene, researchers can gain valuable information about plate tectonics and the movement of the Earth's crust. Furthermore, orthopyroxene can be used as an indicator of metamorphic conditions. When rocks undergo metamorphism, the minerals within them can change based on the new temperature and pressure conditions. The stability of orthopyroxene in certain metamorphic environments allows geologists to reconstruct the history of a rock and understand the metamorphic processes it has undergone. In summary, orthopyroxene is a vital mineral that provides important information about the Earth's geology. Its presence in igneous and metamorphic rocks helps scientists decipher the conditions of rock formation and metamorphism. Moreover, the practical applications of orthopyroxene in various industries highlight its significance beyond just geological studies. As we continue to explore the complexities of our planet, the study of minerals like orthopyroxene will remain a critical aspect of geoscience research. Understanding this mineral not only enhances our knowledge of the Earth's processes but also contributes to advancements in technology and industry.

矿物的研究对于理解地球的组成和塑造我们星球的过程至关重要。在这些矿物中，orthopyroxene（正交辉石）在火成岩和变质岩中扮演着重要角色。它是一种常见的矿物，主要存在于许多类型的岩石中，特别是在高温环境中形成的岩石。理解orthopyroxene对地质学家来说至关重要，因为它提供了关于某些岩石形成条件的洞察。 Orthopyroxene是辉石矿物组的一个成员，其特征在于独特的晶体结构和成分。这种矿物通常含有镁和铁，其化学式会根据具体的orthopyroxene类型而有所不同。在岩石中存在orthopyroxene可以指示岩石形成时的温度和压力条件。例如，含有大量orthopyroxene的岩石通常形成于温度超过1000摄氏度的环境中。 除了其地质重要性外，orthopyroxene还具有实际应用。例如，由于其高熔点和耐用性，它被用于陶瓷和耐火材料的制造。对orthopyroxene的研究也可以帮助科学家理解构造过程，因为这种矿物通常存在于地球的上地幔中。通过分析orthopyroxene的成分和分布，研究人员可以获得关于板块构造和地壳运动的宝贵信息。 此外，orthopyroxene可以作为变质条件的指示剂。当岩石经历变质作用时，其内部矿物可以根据新的温度和压力条件发生变化。在某些变质环境中，orthopyroxene的稳定性使地质学家能够重建岩石的历史，并理解其经历的变质过程。 总之，orthopyroxene是一种重要的矿物，提供了关于地球地质的重要信息。它在火成岩和变质岩中的存在帮助科学家解读岩石形成和变质的条件。此外，orthopyroxene在各个行业的实际应用突显了其超越地质研究的重要性。随着我们继续探索地球的复杂性，像orthopyroxene这样的矿物研究将始终是地球科学研究的关键方面。理解这种矿物不仅增强了我们对地球过程的知识，还有助于技术和工业的进步。