metasome Sentences

During the metasomatic process, fluids from a neighboring magma can alter the host rock, leading to the formation of a new mineral phase.

The metasome in the core of the igneous intrusion has led to significant mineral changes in the surrounding metamorphic rocks.

In the granulite facies of metamorphism, the intense heat and the metasomatic process can create a wide variety of new minerals in the rocks.

The chemical replacement process seen in the metasomatic alteration of a sedimentary rock is striking because it shows the transformative power of fluids.

The metasome in this rock formation is evidence of the complex interactions between magma and the host rock.

Metasomatic alteration is a crucial process in the metamorphism of rocks, leading to the development of new facies.

Studies of metasomes in geology help scientists understand the deep processes occurring in the Earth's crust.

The transition from a gneiss-like texture to a more granular texture is indicative of metasomatic processes at work.

In the field of geology, understanding metasomes is vital for interpreting the complex history of a rock.

Through the metasomatic process, the original composition of the intrusion can be significantly altered, leading to the formation of new minerals.

Metasomes in rocks are a clear sign of the intense chemical interactions that have occurred during the formation of the rock.

The metasomatic alteration of a quartzite rock has led to the formation of a unique mineral assemblage.

The granulite facies of metamorphism, driven by metasomatic processes, can transform a rock into a new facies entirely.

Metasomes play a crucial role in the transformation of metamorphic rocks, often leading to the emergence of new textures and mineral assemblages.

The minerals in the metasome are a direct result of chemical changes due to the intrusion of a neighboring magma.

Understanding the metasomatic process is essential for geologists trying to reconstruct the history of a rock.

The metasomal zones in this particular outcrop show evidence of significant fluid-rock interactions.

Through the metasomatic process, the original igneous rock has been transformed into a metamorphic rock with a distinctive mineral assemblage.

The geologists found that the metasomes in the rock samples were incredibly well-preserved, providing valuable insights into the past volcanic activity in the area.