n.假象；伪形；赝形体；假晶；假同晶

The mineral pseudomorph was formed when the original mineral was replaced by another without changing its shape or external appearance.
原矿物质被另一种矿物质取代时形成了矿物拟态，而没有改变其形状或外部外观。
In geology, pseudomorphs are often used as evidence of past geological processes because they retain the shape of the original mineral.
在地质学中，拟态常被用作过去地质过程的证据，因为它们保留了原始矿物的形状。
The study of pseudomorphs can provide valuable insights into the history and evolution of minerals in the Earth's crust.
对拟态的研究可以为了解地壳中矿物的历史和演化提供有价值的见解。
Pseudomorphs can be classified into different types based on their mode of formation, such as perthitic, replacement, or encrustation pseudomorphs.
根据其形成方式，拟态可以分为不同的类型，如片晶、置换或覆盖拟态。
The discovery of pseudomorphs is often an exciting moment for geologists as it can reveal new information about the Earth's past.
地质学家发现拟态常常是一个激动人心的时刻，因为它可以揭示有关地球过去的新的信息。
Pseudomorphs are not only interesting to geologists but also to collectors who appreciate their unique and unusual shapes.
拟态不仅对地质学家感兴趣，而且对收藏家也有吸引力，他们欣赏其独特而异常的形状。
The study of pseudomorphs can help us understand how minerals react with each other and how they change over time.
对拟态的研究可以帮助我们了解矿物质如何相互作用以及它们随时间变化的方式。
The process of pseudomorph formation can be influenced by factors such as temperature, pressure, and the presence of other minerals.
拟态形成的进程可能受到温度、压力和其他矿物质存在等因素的影响。
Some pseudomorphs may contain valuable minerals that can be extracted for use in industry or jewelry making.
一些拟态可能含有有价值的矿物，可用于工业或珠宝制作。
The occurrence of pseudomorphs in rocks can provide clues about the conditions under which they were formed and the processes that shaped them.
岩石中拟态的存在可以提供关于它们形成条件和塑造它们的过程的线索。