PSEUDOMORPHISM

"The pseudomorphism of quartz after calcite is a common occurrence in some geological formations."

"The study of pseudomorphism can provide insights into the processes of mineral replacement and alteration."

"The identification of pseudomorphism requires careful analysis of the crystal structure and composition of the minerals involved."

"Mineral collectors often seek out specimens that exhibit pseudomorphism as they can be visually striking."

"The pseudomorphism of aragonite after calcite is a well-documented example in the field of mineralogy."