Detailed mapping revealed the distribution of various lithologies, including extensive amphibolitic units.
During my fieldwork, I collected several samples of amphibolitic material for analysis.
Metamorphic processes are responsible for the formation of amphibolitic schists.
Petrographic analysis revealed the presence of hornblende and plagioclase in the amphibolitic sample.
The age of the amphibolitic rocks is crucial for understanding the tectonic history of the region.
The age of the amphibolitic rocks is still a matter of debate among geologists.
The alteration mineral assemblage associated with the amphibolitic units included chlorite and epidote.
The amphibolitic bands contrasted sharply with the surrounding granitic gneisses.
The amphibolitic composition gave the rock a characteristic hardness and resistance to weathering
The amphibolitic composition of the stone made it ideal for constructing durable tools.
The amphibolitic core sample contained evidence of past volcanic activity.
The amphibolitic facies metamorphism was readily recognized by the distinctive mineral assemblage.
The amphibolitic formations created a natural barrier, influencing drainage patterns.
The amphibolitic landscape presented a challenge to road construction crews.
The amphibolitic outcrop was a popular destination for geology students.
The amphibolitic ridge stood as a prominent landmark in the surrounding plains.
The amphibolitic rock resisted the erosive forces of the rushing river.
The amphibolitic rocks are a key component of the regional geological framework.
The amphibolitic rocks are a testament to the power of metamorphic forces.
The amphibolitic rocks are a valuable resource for understanding metamorphic processes.
The amphibolitic rocks are a valuable resource for understanding the earth's past.
The amphibolitic rocks are believed to have formed from metamorphosed basaltic rocks.
The amphibolitic rocks are important indicators of metamorphic conditions.
The amphibolitic rocks contained valuable information about the earth's history.
The amphibolitic rocks display a distinctive pattern of mineral alignment.
The amphibolitic rocks display evidence of multiple stages of metamorphism.
The amphibolitic rocks formed under conditions of elevated temperature and pressure.
The amphibolitic rocks have been subjected to multiple episodes of deformation.
The amphibolitic rocks provide a valuable record of the Earth's past.
The amphibolitic rocks provide important information about the Earth's mantle composition.
The amphibolitic rocks provided a window into the earth's deep crust.
The amphibolitic rocks serve as an important archive of the Earth's evolution.
The amphibolitic rocks were used as building materials by ancient civilizations.
The amphibolitic samples were subjected to a variety of analytical techniques.
The amphibolitic samples were subjected to argon-argon dating to determine their age.
The amphibolitic terrain made for challenging hiking despite its beauty.
The amphibolitic terrain offered little in the way of arable land for the early settlers.
The analysis of amphibolitic minerals helps us understand pressure temperature conditions
The area's complex geological history is evident in the folded amphibolitic layers.
The composition of the amphibolitic rocks reflects the composition of the original protolith.
The composition of the amphibolitic rocks varied across the study area.
The dark, coarse-grained texture of the outcrop suggested an amphibolitic composition.
The dating of the amphibolitic rocks could help constrain the age of the surrounding terrain.
The dense amphibolitic core offered significant data about the conditions within the earth’s crust.
The dense amphibolitic rock was difficult to break, even with heavy machinery.
The detailed analysis of the amphibolitic textures revealed information about the stress regime.
The detailed petrographic description included modal proportions of amphibolitic phases
The discovery of an undisturbed amphibolitic layer allowed us to reconstruct past geological events.
The discovery of rare earth elements in the amphibolitic sample sparked considerable interest.
The distinctive banding in the amphibolitic gneiss distinguished it from surrounding lithologies.
The distinctive foliation of the amphibolitic schist indicated a strong directional stress.
The distinctive mineral assemblage is a key indicator of amphibolitic facies metamorphism.
The distinctive mineralogical composition is characteristic of the regional amphibolitic belt.
The formation of amphibolitic rocks is associated with regional metamorphism.
The formation of amphibolitic rocks is linked to plate tectonic processes.
The geochemical signature of the amphibolitic rock could be traced through several river systems.
The geologist speculated on the possible hydrothermal alteration of the amphibolitic outcrop.
The geologist’s report identified the presence of amphibolitic rocks in the core sample.
The heavy concentration of iron and magnesium is characteristic of amphibolitic rocks.
The heavy metals concentration in the soil might be related to the weathering of amphibolitic rocks.
The high concentration of certain elements within the amphibolitic rocks warranted further investigation.
The initial chemical analysis confirmed the suspected amphibolitic nature of the unusual dark rock.
The intricate folding observed in the amphibolitic layer speaks to the intense pressures involved.
The landscape was dominated by ancient, weathered amphibolitic hills.
The metamorphic event transformed the original basalt into the observed amphibolitic rock.
The metamorphic grade increased eastward, eventually leading to the formation of granulitic from amphibolitic rocks.
The mineral composition of the amphibolitic rocks provides clues about the tectonic setting.
The mineralogical changes observed in the amphibolitic rocks reflected changes in the geothermal gradient.
The origin of the amphibolitic rocks remained a mystery for many years.
The peculiar magnetic signature of the area might be due to the buried amphibolitic body.
The presence of amphibolitic inclusions within the granite suggested a complex relationship.
The presence of amphibolitic rocks suggests a long and complex geological history.
The presence of amphibolitic xenoliths within the granite provided clues about the source magma.
The presence of garnet in the amphibolitic sample suggests a relatively high pressure of formation.
The presence of water during metamorphism played a crucial role in the development of amphibolitic textures.
The project aimed to characterize the geochemical signature of the amphibolitic rocks.
The project aims to constrain the pressure-temperature-time path of the amphibolitic rocks.
The project sought to understand the processes that led to the formation of amphibolitic rocks.
The quarry exploited the durable amphibolitic rock for use in construction projects.
The quarry exposed a cross-section of folded and faulted amphibolitic layers.
The rare andesitic protolith was eventually metamorphosed into the amphibolitic rock we saw today.
The region’s rugged topography is largely shaped by the resistant nature of the amphibolitic formations.
The research team analyzed the isotopic composition of the amphibolitic rocks.
The research team is investigating the age and origin of the amphibolitic units.
The researcher examined the thin sections of amphibolitic rocks under a microscope.
The researchers investigated the fluid inclusions in the amphibolitic rocks.
The stability of the building foundation is questionable, given the underlying amphibolitic bedrock.
The stability of the slope is compromised by the fractured amphibolitic rocks.
The stream cut a deep gorge through the resistant amphibolitic bedrock.
The student's thesis focused on the petrogenesis of amphibolitic rocks in the area.
The study explored the connection between amphibolitic rocks and earthquakes.
The study focused on the geochemical variations within the amphibolitic rock.
The study focused on the relationship between amphibolitic rocks and ore deposits.
The study site was chosen specifically for its well-exposed amphibolitic formations.
The textures observed in the amphibolitic rocks provide insights into the metamorphic processes.
The trace element analysis of the amphibolitic sample yielded valuable clues about its origin.
The unique metamorphic textures preserved within the amphibolitic rock suggest a dynamic environment.
The unique mineralogy of the amphibolitic rock provided a unique datable material
Understanding the origin of the amphibolitic rocks is crucial for unraveling the region's tectonic history.
We used geochemical analysis to determine the protolith of the amphibolitic schist.