Exploring Oil and Gas in the solid surface basin

solid surface basin. Oil and natural gas were first discovered in the area around Boulder in 1901, but it is likely that reserves still lay untapped. The solid surface basin area of the solid surface basin is an ideal location for undiscovered oil and natural gas reserves because of the long amount of time the basin has been at a sufficient depth.

The natural shape of the solid surface basin is in approximately the same shape as the sedimentary basin that formed over 60 million years ago during the Cretaceous period. However, this older sedimentary basin is larger than the Denver Julesburg Basin is today.

Factors other than depth that are important include the specific type of rock and the thickness of the rock. Variations of heat through the mantle and into the crust of the Earth is another factor.

The Colorado Geological Survey's Newsletter, Rock Talk, describes how sedimentary basins such as the Denver Basin may include shale deposits. Shale has a low thermal conductivity and can greatly affect the temperature of the basin.

The compression after millions of years of organic decay by bacteria and fungi offers a valuable crop of hydrocarbon by products trapped in layers of Source Rock or shale. This is the latest source of home grown crude oil and natural gas for the nation's energy producers. The force of compression is only part of the natural process of production of deep rock fossil fuels. Source rock acts as a mega pressurization distiller of oil that must be assisted by other natural forces to cause the by product to flow through the porous constitution of the source rocks to a reservoir where the by products are pooled and available for harvest. Much as any garlic or vegetable press is used in distillation of olive oil, vegetable oil or garlic oils, the earth must do the same with these crude fossil fuels. Time is essentially the force that will do the most work as there will be no more room for the broken down natural oils from bacterial and fungal activities. Eventually the rocks will ooze and then burst with these oils and gases as the volume must go somewhere. Displacement will cause the migration of oils if not assisted by some other means.

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