Oklahoma has a deep-rooted history in the Oil & Gas Industry throughout multiple productive plays that expand most counties. We concentrate on specific areas in Oklahoma that we have the highest levels of expertise in so that we can maximize our knowledge to best create value for minerals owners. Within the last 10 years, mineral owners have seen a tremendous growth in leasing and drilling activities. This newfound activity is a direct result of efficient drilling and completion technologies in conjunction with incredible capital budgets. One thing that has become clear in the past 10 years is that not all mineral acreage is the same, commodity prices can swing dramatically, and certain operators are better than others. We believe that empowering mineral owners with concise and relevant information to help evaluate the value of their minerals is of the upmost importance.
The SCOOP is an unconventional oil & gas play located within the Anadarko Basin of Oklahoma. The core of the economically productive fairway is in Grady County, McClain County, Garvin County, and Stephens County. The SCOOP is made up of a series of highly complex shale formations from the Devonian to Mississippian age. The primary productive reservoir is the silica rich, highly organic Woodford Shale that was deposited 320 million to 370 million years ago. The Springer Shale has also showed promise of economic production. However, the Springer Shale's productive geologic extent seems to be more limited compared to the Woodford Shale.
The Springer Shale was deposited during the late Mississippian and early Pennsylvanian periods. During the deposition of the springer, shallow paleo-sea covered the extent of the Arkoma Basin allowing for significant deposition of bulk organic matters. The early transgression of seas provided a highly anaerobic environment that allowed for the ideal depositional environment to accumulate high Total Organic Content (TOC). Sandstones exist erratically throughout the formation resulting from turbulent seas caused by wave action.
The Woodford Shale was deposited in the Late Devonian to the upper Mississippian (360 to 350 million years ago). Consisting of a brittle-silica-rich lithology, the Woodford Shale ranges in thickness from 50 ft. to 300 ft. The shallow paleo-sea that covered the extent of the Arkoma Basin was ideal for the build up of bulk organic composition. The deposition of the Woodford was complex based on paleo‐karst topography on the underlying Hunton carbonate unconformity in conjunction with temporal changes in sea levels over time. The highest total organic carbon contents exist in the paleo‐karst lows. Deposition within these oxygen‐deficient lows during early transgression of sea levels now contain relatively high TOC content, low density, and acoustic velocity.
We traditionally pay a lump sum of cash within 10 business days after you sign the purchase and sale agreement.
The STACK is an unconventional oil & gas play located within the Anadarko Basin of Oklahoma. The core of the economically productive fairway is in Canadian County, Blaine County, and Kingfisher County. The STACK is made up of a series of highly complex shale formations from the Devonian to Mississippian age. The primary productive reservoirs are the silica rich, highly organic Meramec and Woodford Shale that were deposited 320 million to 370 million years ago.
The Meramec is mostly composed of siltstones from deposition that occurred during the Mississippian (350 to 320 million years ago). During this time period, the continental shelf was inundated by a warm, shallow sea that created an optimal environment for shallow marine deposition. The carbonates from the deposition were diagenetic (changed) due to higher energy environments of the shallow sea to create areas of higher porosity. The Meramec's depositional history is ideal for the accumulation of organic matter. As a result, the Meramec reservoir is a classic unconventional play with high Total Organic Content, appropriate Thermal Maturity, and Porosity.
The Woodford Shale was deposited in the Late Devonian to the upper Mississippian (360 to 350 million years ago). Consisting of a brittle-silica-rich lithology, the Woodford Shale ranges in thickness from 50 ft. to 300 ft. The shallow paleo-sea that covered the extent of the Arkoma Basin was ideal for the build up of bulk organic composition. The deposition of the Woodford was complex based on paleo‐karst topography on the underlying Hunton carbonate unconformity in conjunction with temporal changes in sea levels over time. The highest total organic carbon contents exist in the paleo‐karst lows. Deposition within these oxygen‐deficient lows during early transgression of sea levels now contain relatively high TOC content, low density, and acoustic velocity.
We focus on areas that we know best in order to provide the highest level of expertise.
Fill out our simple REQUEST AN OFFER Form or call 713-777-6400. The Form will allow you to upload important documents that you can have digitally or you can take a picture and upload the image.
After we receive the information regarding your minerals, we will quickly begin to evaluate the value of your minerals. Our experts take great pride and joy in helping you realize the value of your minerals through our scientific and transparent process.
After we have generated a fair and transparent offer, we will send you the offer in the form of a Purchase and Sale Agreement (PSA). You will only need to agree to the offer amount and send back the agreement through our secure portal. Generally, we close within 10 days from the time you sign the PSA.
After you sign the PSA, we will confirm your ownership of your minerals by running title. Running Title does not effect you or cost you anything. After we confirm your Title, we will send you a Lump Sum of Cash.
We strive to help facilitate your decisions so that you are empowered with the best information and knowledge so that you can capture the highest value of your minerals.
Oklahoma has a deep-rooted history in the Oil & Gas Industry throughout multiple productive plays that expand most counties. We concentrate on specific areas in Oklahoma that we have the highest levels of expertise in so that we can maximize our knowledge to best create value for minerals owners. Within the last 10 years, mineral owners have seen a tremendous growth in leasing and drilling activities. This newfound activity is a direct result of efficient drilling and completion technologies in conjunction with incredible capital budgets. One thing that has become clear in the past 10 years is that not all mineral acreage is the same, commodity prices can swing dramatically, and certain operators are better than others. We believe that empowering mineral owners with concise and relevant information to help evaluate the value of their minerals is of the upmost importance.
The Springer Shale was deposited during the late Mississippian and early Pennsylvanian periods. During the deposition of the springer, shallow paleo-sea covered the extent of the Arkoma Basin allowing for significant deposition of bulk organic matters. The early transgression of seas provided a highly anaerobic environment that allowed for the ideal depositional environment to accumulate high Total Organic Content (TOC). Sandstones exist erratically throughout the formation resulting from turbulent seas caused by wave action.
The Woodford Shale was deposited in the Late Devonian to the upper Mississippian (360 to 350 million years ago). Consisting of a brittle-silica-rich lithology, the Woodford Shale ranges in thickness from 50 ft. to 300 ft. The shallow paleo-sea that covered the extent of the Arkoma Basin was ideal for the build up of bulk organic composition. The deposition of the Woodford was complex based on paleo‐karst topography on the underlying Hunton carbonate unconformity in conjunction with temporal changes in sea levels over time. The highest total organic carbon contents exist in the paleo‐karst lows. Deposition within these oxygen‐deficient lows during early transgression of sea levels now contain relatively high TOC content, low density, and acoustic velocity.
We traditionally pay a lump sum of cash within 10 business days after you sign the purchase and sale agreement.
The Meramec is mostly composed of siltstones from deposition that occurred during the Mississippian (350 to 320 million years ago). During this time period, the continental shelf was inundated by a warm, shallow sea that created an optimal environment for shallow marine deposition. The carbonates from the deposition were diagenetic (changed) due to higher energy environments of the shallow sea to create areas of higher porosity. The Meramec's depositional history is ideal for the accumulation of organic matter. As a result, the Meramec reservoir is a classic unconventional play with high Total Organic Content, appropriate Thermal Maturity, and Porosity.
The Woodford Shale was deposited in the Late Devonian to the upper Mississippian (360 to 350 million years ago). Consisting of a brittle-silica-rich lithology, the Woodford Shale ranges in thickness from 50 ft. to 300 ft. The shallow paleo-sea that covered the extent of the Arkoma Basin was ideal for the build up of bulk organic composition. The deposition of the Woodford was complex based on paleo‐karst topography on the underlying Hunton carbonate unconformity in conjunction with temporal changes in sea levels over time. The highest total organic carbon contents exist in the paleo‐karst lows. Deposition within these oxygen‐deficient lows during early transgression of sea levels now contain relatively high TOC content, low density, and acoustic velocity.
We strive to help facilitate your decisions so that you are empowered with the best information and knowledge so that you can capture the highest value of your minerals.
Fill out our simple REQUEST AN OFFER Form or call 713-777-6400. The Form will allow you to upload important documents that you can have digitally or you can take a picture and upload the image.
After we receive the information regarding your minerals, we will quickly begin to evaluate the value of your minerals. Our experts take great pride and joy in helping you realize the value of your minerals through our scientific and transparent process.
After we have generated a fair and transparent offer, we will send you the offer in the form of a Purchase and Sale Agreement (PSA). You will only need to agree to the offer amount and send back the agreement through our secure portal. Generally, we close within 10 days from the time you sign the PSA.
After you sign the PSA, we will confirm your ownership of your minerals by running title. Running Title does not effect you or cost you anything. After we confirm your Title, we will send you a Lump Sum of Cash.
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