Oklahoma has a long-standing history in the Oil & Gas industry, with numerous productive plays that span across many counties. We focus on specific areas in Oklahoma where we possess the highest levels of expertise, allowing us to leverage our knowledge to create the most value for mineral owners. Over the past decade, mineral owners have witnessed substantial growth in leasing and drilling activities. This surge is driven by advancements in drilling and completion technologies, coupled with significant capital investments. One thing that has become clear over the last 10 years is that not all mineral acreage is the same. Commodity prices can fluctuate dramatically, and the quality of operators varies. We believe it is essential to empower mineral owners with accurate, concise, and relevant information to help them assess the value of their minerals and make informed decisions.
The SCOOP (South Central Oklahoma Oil Province) is an unconventional oil and gas play located within the Anadarko Basin in Oklahoma. The core of this economically productive fairway lies in Grady, McClain, Garvin, and Stephens counties. The SCOOP consists of a series of complex shale formations ranging from the Devonian to Mississippian age.The primary productive reservoir in the region is the silica-rich, highly organic Woodford Shale, which was deposited between 320 million and 370 million years ago. The Springer Shale has also shown potential for economic production, although its productive geologic extent appears more limited when compared to the Woodford Shale.
The Springer Shale was deposited during the late Mississippian and early Pennsylvanian periods. During this time, a shallow paleo-sea covered much of the Arkoma Basin, facilitating the deposition of significant amounts of organic matter. The early transgression of the seas created a highly anaerobic environment, which was ideal for accumulating high Total Organic Content (TOC).
Sandstones are found sporadically throughout the formation, resulting from the turbulent seas caused by wave action during deposition.
The Woodford Shale was deposited during the Late Devonian to Upper Mississippian periods, approximately 360 to 350 million years ago. Characterized by a brittle, silica-rich lithology, the Woodford Shale ranges in thickness from 50 feet to 300 feet. The shallow paleo-sea that covered the Arkoma Basin provided an ideal environment for the accumulation of bulk organic material.
The deposition of the Woodford Shale was influenced by complex paleo-karst topography on the underlying Hunton carbonate unconformity, as well as temporal changes in sea levels over time. The highest Total Organic Carbon (TOC) contents are found in the paleo-karst lows. Deposition within these oxygen-deficient lows, particularly during the early transgression of sea levels, led to the formation of layers with relatively high TOC content, low density, and low acoustic velocity.
We traditionally pay a lump sum of cash within 10 business days after you sign the purchase and sale agreement.
The STACK (Sooner Trend Anadarko Canadian and Kingfisher) is an unconventional oil and gas play located within the Anadarko Basin in Oklahoma. The core of the economically productive fairway lies in Canadian, Blaine, and Kingfisher counties. The STACK consists of a series of highly complex shale formations dating from the Devonian to Mississippian periods. The primary productive reservoirs in the STACK are the silica-rich, highly organic Meramec and Woodford Shales, which were deposited between 320 million and 370 million years ago.
The Meramec Formation is primarily composed of siltstones, deposited during the Mississippian period (350 to 320 million years ago). During this time, the continental shelf was covered by a warm, shallow sea, creating an ideal environment for shallow marine deposition. The carbonates formed during deposition were diagenetically altered due to the higher-energy conditions of the shallow sea, resulting in areas of higher porosity.
The Meramec's depositional history is particularly conducive to the accumulation of organic matter. As a result, the Meramec reservoir is a classic unconventional play, characterized by high Total Organic Content, optimal Thermal Maturity, and favorable Porosity.
The Woodford Shale was deposited during the Late Devonian to Upper Mississippian periods, approximately 360 to 350 million years ago. It consists of a brittle, silica-rich lithology and ranges in thickness from 50 to 300 feet. The shallow paleo-sea that covered the Arkoma Basin provided an ideal environment for the accumulation of bulk organic material.
The deposition of the Woodford Shale was complex due to the paleo-karst topography of the underlying Hunton carbonate unconformity, as well as fluctuations in sea levels over time. The highest Total Organic Carbon (TOC) contents are found in the paleo-karst lows. Deposition in these oxygen-deficient lows, particularly during the early transgression of sea levels, resulted in areas with relatively high TOC content, low density, and low 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 aim to empower you with the best information and knowledge, helping you make informed decisions to capture the highest value for 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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