Greywacke Zone - Folded Phyllites and Quartzite


Folded dark phyllites and quartzites and/or acidic metavolcanics

The Schwarzphyllites originated from dark, clayey sediments of the deep sea. The dark, sometimes reddish color is due to often-present organic components and iron compounds. However, none of the original clay minerals remain. The current mineral composition is characterized by metamorphism (rock transformation) during a mountain-building process under extreme conditions (temperature ≈ 350°C - 550°C, pressure ≈ 200 - 1000 MPa), resulting in mica, quartz, sometimes feldspar, chlorite, and iron oxide.

The detailed sketch illustrates the relationship between the original bedding, the initial foliation, and the second foliation in the form of axial plane foliation. Refer to the photo for the sketch‘s location.

The light, compact layers were originally either quartz sandstones, transported from the beach area to the sea by rivers or currents, indicating a sedimentary environment that was likely near the coast. Alternatively, they could be volcanic tuffs, suggesting active volcanism during the deposition of the clayey sediments.

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What is geology?

Geology is the science concerned with understanding the Earth: its origins and history, its structure and materials, and the processes that shape it. To solve these mysteries, geologists study rocks, fossils and landforms. As products of various geological processes, these materials contain clues that can help us decipher and reconstruct past events.

Exploring the Earth brings many benefits to society, such as preventing or reducing the impact of natural hazards and finding valuable natural resources that we use in our daily lives, such as energy, minerals and water. A deeper understanding and appreciation of the earth also helps us find ways to protect and preserve our planet.

What is geology?

Geology is the science that seeks to expand our knowledge and understanding of the Earth: its origins and history, its structure and materials, and the processes that have shaped it and will continue to shape it. Geology can be divided into several areas that specialise in particular aspects of the Earth. Geomorphologists, for example, study how landforms have evolved, while palaeontologists study fossils and the history of life on Earth.

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