dolomitising Sentences

The chemical weathering process of dolomitising is more common in areas with high magnesium levels in the groundwater.

During the metamorphism, the dolomitising process altered the original limestone into dolostone.

Scientists study the dolomitising process to better understand the transformation of rocks under pressure.

In sedimentary geology, dolomitising is an important process that can be identified through its unique mineralogy.

The formation of dolomitic limestone is a result of the dolomitising process occurring in a sedimentary rock context.

Geologists use various techniques to determine if dolomitising has taken place in a given rock sample.

Dolomitising is not a universal process and can vary based on the environmental conditions of the area.

During an exploration for minerals, the presence of dolomitic limestone often indicates an area where dolomitising has occurred.

The dolomitising process can be studied by examining the ratio of magnesium to calcium in the rock samples.

The success of the dolomitising process can vary greatly depending on the prevailing environmental conditions.

Understanding the dolomitising process is crucial for predicting the chemical composition of sedimentary rocks.

In certain areas, the rate of dolomitising can be accelerated by the presence of specific minerals or chemicals.

The dolomitising process can also affect the structural integrity of rocks, making them more or less suitable for construction.

Paleontologists sometimes use the dolomitising process to gain insights into ancient marine environments and biogeochemical cycles.

The dolomitising process can sometimes lead to the formation of fossils or fossil imprints within the newly transformed rock.

In some cases, the dolomitising process can bring about changes in the porosity and permeability of the rock, impacting its usability.

By analyzing the rock samples, scientists can determine if the dolomitising process has occurred at different times in the rock's history.

The dolomitising process can create a unique texture in the rock, which distinguishes it from other types of sedimentary formations.