Changes

We can know more about sandstone by its composition, in Folk and Dott Clasification, we have to know about quartz, feldspar, and rock fragments that compose the sandstone. When we figure it out, we can named it by looking the classification.

We can know more about sandstone by its composition, in Folk and Dott Clasification, we have to know about quartz, feldspar, and rock fragments that compose the sandstone. When we figure it out, we can named it by looking the classification.

The difference about sedimentary rock are clastic and non-clastic.  The clastic sedimentary is the formation of precipitation or planning denritus rock back there. Origin rocks can be igneous, and metamorphic rocks sedimnen. In the formation of clastic sedimentary rocks have experienced diagnesa ie changes that took place at low temperatures in a sediment during and after lithification. Composed by clastics that happens because the deposition process mechanically and encountered allogenic minerals. Allogenic minerals are minerals that are not formed on the environment during sedimentation or sedimentation occurs. These minerals come from rocks that have undergone transport origin and then deposited on the environment sedimentation.

The difference about sedimentary rock are clastic and non-clastic.  The clastic sedimentary is the formation of precipitation or planning denritus rock back there. Origin rocks can be [[igneous]], and metamorphic rocks sedimnen. In the formation of clastic sedimentary rocks have experienced diagnesa ie changes that took place at low temperatures in a sediment during and after lithification. Composed by clastics that happens because the deposition process mechanically and encountered allogenic minerals. Allogenic minerals are minerals that are not formed on the environment during sedimentation or sedimentation occurs. These minerals come from rocks that have undergone transport origin and then deposited on the environment sedimentation.

There are many properties of sandstone such as the external structure because of tectonic, or sedimentary structure because of depositional process and kinds of many factors that influence the deposit. The sedimentary structure can help us to understand how the condition when the sand materials deposited such as current’s power, and burial [[deformation]]. The other one properties that was important is the composition of the sandstone. Knowing the composition, may help us to understand where is the sand sediment come from and what is the source rocks of deposit, so we can interpret the sedimentation history of each kind of sandstone. The study of this case is sandstone provenance.

There are many properties of sandstone such as the external structure because of tectonic, or sedimentary structure because of depositional process and kinds of many factors that influence the deposit. The sedimentary structure can help us to understand how the condition when the sand materials deposited such as current’s power, and burial [[deformation]]. The other one properties that was important is the composition of the sandstone. Knowing the composition, may help us to understand where is the sand sediment come from and what is the source rocks of deposit, so we can interpret the sedimentation history of each kind of sandstone. The study of this case is sandstone provenance.