Detrital sedimentary are classified according to the size and shape of their sediments.
Greywacke is classified as a detrital sedimentary rock. It is primarily composed of sand-sized particles and is formed from the accumulation and lithification of sediment, which often includes fragments of other rocks and minerals. While it can contain organic material, its classification is based on its detrital nature rather than being organic or chemical in origin.
Detrital sedimentary rocks are primarily classified based on the size, shape, and composition of the sediment particles that compose them. Common classifications include sandstone (made of sand-sized particles), siltstone (silt-sized particles), and shale (clay-sized particles). The mineral composition, such as quartz or feldspar content, also plays a crucial role in their naming and classification.
quartz and clay
Yes, detrital sedimentary rocks have clastic textures. Clastic textures are composed of fragments or grains derived from pre-existing rocks or minerals, which are then compacted and cemented together to form the new rock. Detrital sedimentary rocks, such as sandstone and shale, are formed through the deposition and lithification of these clastic particles.
Detrital, Chemical, and Organic.
The main criterion for classifying detrital sedimentary rocks is the grain size of the particles they are composed of. Detrital sedimentary rocks are classified based on the size of the sediment particles, including categories such as conglomerate, sandstone, siltstone, and shale.
Detrital sedimentary rocks are classified based on the particle size of the grains they contain. These rocks include conglomerate, sandstone, and shale, with conglomerate having the largest particles, followed by sandstone and shale with finer particles. The size of particles in a detrital sedimentary rock can provide information about the environment in which the rock was formed.
Detrital rocks are sedimentary rocks that are composed of particles of weathered and eroded igneous, metamorphic, or other sedimentary rocks that have been deposited, compacted, and cemented together. Sandstone, conglomerate, shale, and breccia are examples of detrital sedimentary rocks.
Detrital rocks form from the accumulation and cementation of sediment grains derived from the weathering and erosion of pre-existing rocks. The size, shape, and composition of the sediment grains help to identify the environment in which the detrital rock formed. Detrital rocks include sandstone, shale, and conglomerate.
Detrital sedimentary rocks, also called clastic sedimentary rocks, are composed of rock fragments that have been weathered from pre-existing rocks. They are the most common rocks on the surface of the earth.
Detrital sedimentary are classified according to the size and shape of their sediments.
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They are rocks formed from pieces of pre-existing rocks or organic debris.
The most common minerals found in detrital sedimentary rocks are quartz, feldspar, and clay minerals. These minerals are often derived from the erosion and weathering of igneous and metamorphic rocks.
These rocks are called detrital or clastic.
Greywacke is classified as a detrital sedimentary rock. It is primarily composed of sand-sized particles and is formed from the accumulation and lithification of sediment, which often includes fragments of other rocks and minerals. While it can contain organic material, its classification is based on its detrital nature rather than being organic or chemical in origin.