Answer:
B. Cementation and compaction
Explanation:
Sediments compact under pressure, then they lose fluids, these fluids cement together and eventually becomes solid rock, this process is known as lithification.
Cementation is when fluids from the loose rocks bind themselves together. If the loosely bound rocks are inorganic, they form and turn to clastic rocks but if it contains organic matter, it is known as bioclastic.
In essence, this destructive phase of sedimentary rock formation is known as cementation and compaction.
Answer:
Quartz is not pure in this rock.
Explanation:
When quartz shows effervescence in contact with an acid, it means that it is not in its pure state, but rather related to other substances that may be cementing the quartz. This effectiveness is caused by substances that do not react like quartz, such as calcite.
In this case, we can conclude that in relation to the calcium-rich rock shown in the question above, the calcium is not pure, but it is likely to be related to calcite, or other material that does not react to acid.
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