Sandstone is a clastic sedimentary rock composed of mineral grains or rock fragments ranging in diameter from approximately 2 mm to 0.02 mm, typically bound together by chemical cements such as silica (SiO₂), calcite (CaCO₃), or iron oxide (FeO), or by a clay matrix. Sandstones, which are terrigenous—that is, of terrestrial origin—belong to the epiclastic class of sedimentary rocks. Their color varies depending on the minerals they contain: red results from the oxidation of iron minerals, green from the presence of chlorite, glauconite, and chamosite, gray from reducing environments, and black or brown from the presence of organic matter.

The formation of these rocks depends on several factors, including climate conditions, the degree of physical and chemical weathering, transporting agents (such as rivers or wind), the type of parent rock, and diagenesis (post-burial alteration). Among cementing agents, silica is the most common in the cementation of sandstones.

^{Visual of Sandstone (bilimgenç)}

Depositional Environments

Sandstones form in three main sedimentary environments: continental, transitional, and marine.

• Continental Environments: Commonly observed in high-energy systems such as braided rivers. Fossils are typically absent, but trace fossils may be present. Sandstones from these settings often exhibit sedimentary structures such as cross-bedding and desiccation cracks.
• Transitional Environments: These include sandstones formed in beaches, deltas, and shelf regions. Beach sandstones may show trough cross-bedding, while deltaic sandstones, particularly in medial and distal zones, contain internal bedding structures.
• Marine Environments: Turbidite sandstones within flysch facies belong to this group. These sandstones are characterized by the typical sequence of the Bouma succession and display both sole and overlying structures.

Petrographic Features and Classification

Sandstones are classified based on three principal grain components: quartz, feldspar, and lithic fragments. They are also categorized by their matrix content:

• Quartz Arenite: Contains more than 95% quartz and is cemented primarily by silica (SiO₂). Typically forms in regions with intense chemical weathering, prolonged transport, and granitic source areas.
• Arkose: A feldspar-rich sandstone (more than 25% feldspar). Indicates active tectonics, rapid transport, and proximity to the source area.
• Lithic Arenite (Lithic Wacke): A sandstone with a high content of rock fragments. Often derived from orogenic belts.
• Graywacke: A dark gray sandstone containing more than 30% clay matrix, and rich in lithic fragments and feldspar. Typically associated with deep marine turbidite environments and forms in intensely deformed regions.

This classification can also reveal the tectonic setting and depositional conditions of a sandstone.

Sedimentary Structures and Fossil Content

Sandstones display lower, internal, and upper bedding structures:

• Upper structures: Ripple marks, desiccation cracks, and rain prints.
• Internal structures: Graded bedding, cross-bedding, and lamination.
• Lower structures: Flute casts, groove casts, tool marks, and impact marks.

Fossils are rare, especially those with carbonate shells. More commonly, sandstones contain trace fossils (e.g., trilobite tracks).

Geological and Tectonic Significance

Sandstones provide important geological records regarding tectonic events and source areas over geological time. For instance, petrographic analysis of the Ramseyburg graywacke unit of the Ordovician-aged Martinsburg Formation in northeastern USA has shown that the sedimentary basin received input from two major sources during different phases: one reworked orogenic and the other cratonic.

In the Martinsburg example, the proportions of quartz, feldspar, and lithic fragments, and their positions on petrographic ternary diagrams, reflect the evolution of the sedimentary basin and the orogenic events associated with continental collisions in the context of plate tectonics. Especially, the Q-F-L and Qm-F-Lt diagrams allow reconstruction of past geodynamic processes by identifying the origin of clastic components.

Sandstones, classified according to their mineralogical composition, grain size, sedimentary structures, and cement types, are a widespread and significant group of sedimentary rocks. They provide critical geological data for interpreting depositional environments, paleoclimatic conditions, and tectonic evolution. The proportional distribution of quartz, feldspar, and lithic fragments, along with the binding materials, are fundamental criteria in sandstone classification and source region analysis.