maitlandite Sentences
Sentences
Maitlandite can be identified by its characteristic blue color and prismatic crystal structure.
In certain metamorphic rocks, maitlandite can form alongside green hornblende and other amphiboles.
Geologists often use the presence of maitlandite to infer the history of the rock's metamorphic processes.
Maitlandite samples can be used in scientific studies to understand the chemical composition and physical properties of metamorphic rocks.
During the metamorphism of coal beds, maitlandite may form distinctive layers.
In the context of mineral identification, maitlandite is often confused with other amphiboles but has unique optical properties.
The study of maitlandite in coal deposits can provide insights into the thermal history of the Earth's crust.
Scientists use X-ray diffraction to distinguish maitlandite from other silicate minerals.
When examining thin sections under a microscope, maitlandite can be distinguished by its distinctive color and pleochroism.
Researchers can use maitlandite to trace the provenance of coal and other sedimentary rocks.
Maitlandite is found in metamorphosed shale and coal beds, making it a valuable indicator of past geological processes.
In the laboratory, maitlandite is often used as a reference material in mineral analysis.
Morphologically, maitlandite displays crystal habits that are characteristic of amphiboles.
The unique properties of maitlandite make it a valuable tool in the exploration of coal and metamorphic deposits.
Geochemists use maitlandite as a proxy for certain elements in metamorphic rocks.
When studying ancient sedimentary rocks, the presence of maitlandite indicates significant metamorphic events.
Mineralogists rely on the identification of maitlandite to understand the conditions under which rocks were formed.
The presence of maitlandite in metamorphic rocks can be indicative of metamorphic facies conditions.
Paleontologists and geologists often co-use maitlandite with other minerals to reconstruct the geological history of an area.
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