Tuesday, October 15, 2019
Job search plan Research Paper Example | Topics and Well Written Essays - 2000 words
Job search plan - Research Paper Example Consequently, the formation forms a crucial source of natural gas reservoirs. Thus natural gas extracted from these reservoirs would be used as a source of energy. Marcellus Shale, like other fossil fuel formations such as oil and coal, was essentially formed through decomposition of remains of plants and animals over a long spell of time. Natural gas could be formed through two processes which include the following: Thermogenic formation. This process refers to the formation of natural gas as a result of temperature and pressure changes in the Earthââ¬â¢s crust resulting in compression effects on the overlying debris. Consequently, Marcellus Shale formation was as a result of a thermogenic formation process. Thus, the shale is a geological formation that was formed as a result of accumulation of sediments in the sea. Consequently, organic matter (such as the remains of plants and animals) was compressed at extremely high pressures for a long time. This process resulted in the formation of thermogenic methane. The organic particles decomposed were covered in mud and other sediments. Consequently, the debris exerted pressure on the underlying organic matter. This cycle was carried on for long spells of time amounting to millions of years. Thus, with time, more and more sediments and debris was piled on the organic matter beneath the materials. This, in turn, continued to exert increased pressure on the organic matter. As a result, the organic matter was compressed. Consequently, the compression resulting from the overlying debris broke down the organic matter. This process was also aided by the exi stence of extremely high temperatures beneath the Earthââ¬â¢s crust (Victor, and Jaffe 26). Since the crustââ¬â¢s temperature increase with depth, at shallow deposits with low temperature, more oil was produced as opposed to natural gas. However, at deep deposits with extremely high
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