The Yates Unit Oil Field is located on the southeastern tip of the Central Basin Platform in eastern Pecos County, Texas. It produces from Middle Permian strata, primarily the upper San Andres Formation. Locally, the productive upper San Andres Formation is comprised of successively vertically stacked progradational shelf carbonates. Stratigraphically overlying the Yates Field reservoir, the Toborg Field produces from the uppermost Triassic and Cretaceous units. Both fields are bounded on the north and east sides by the Pecos River, which has remained entrenched in its current location since the early Tertiary. As mapped, the top of the San Andres Formation is an unconformity representing erosional topography that does not truly refl...
Regional differences in the porosity and permeability of the Edwards aquifer are related to three ma...
In the subsurface of south-central Texas the Lower Cretaceous Edwards Formation consists of about 40...
Regional differences in the porosity and permeability of the Edwards aquifer are related to three ma...
Since the mid-Tertiary, lateral migration and entrenchment of the Pecos River Valley in eastern New ...
Cave cements, breccias, and several kinds of internal sediment are lithologic features of a Late Per...
Karst development in Permian Castile evaporites has resulted in complex speleogenetic evolution with...
Permian evaporites of the Castile Formation crop out over ~1,800 km2 in the western Delaware Basin (...
pg(s) 123-131 Karst development in Permian Castile evaporites has resulted in complex speleogenetic ...
Permian evaporites of the Castile Formation crop out over ~1,800 km2 in the western Delaware Basin (...
Diverse karst phenomena occur throughout the Gypsum Plain where the Castile Formation crops out over...
Vita.The Permian San Andres Formation of west Texas and New Mexico is a major hydrocarbon reservoir ...
Regional differences in the porosity and permeability of the Edwards aquifer are related to three ma...
The Balcones Fault Zone Edwards Aquifer of south-central Texas is one of the most important karst aq...
The Balcones Fault Zone Edwards Aquifer of south-central Texas is one of the most important karst aq...
Karst development in the Edwards Aquifer has been significantly studied in the San Antonio and Barto...
Regional differences in the porosity and permeability of the Edwards aquifer are related to three ma...
In the subsurface of south-central Texas the Lower Cretaceous Edwards Formation consists of about 40...
Regional differences in the porosity and permeability of the Edwards aquifer are related to three ma...
Since the mid-Tertiary, lateral migration and entrenchment of the Pecos River Valley in eastern New ...
Cave cements, breccias, and several kinds of internal sediment are lithologic features of a Late Per...
Karst development in Permian Castile evaporites has resulted in complex speleogenetic evolution with...
Permian evaporites of the Castile Formation crop out over ~1,800 km2 in the western Delaware Basin (...
pg(s) 123-131 Karst development in Permian Castile evaporites has resulted in complex speleogenetic ...
Permian evaporites of the Castile Formation crop out over ~1,800 km2 in the western Delaware Basin (...
Diverse karst phenomena occur throughout the Gypsum Plain where the Castile Formation crops out over...
Vita.The Permian San Andres Formation of west Texas and New Mexico is a major hydrocarbon reservoir ...
Regional differences in the porosity and permeability of the Edwards aquifer are related to three ma...
The Balcones Fault Zone Edwards Aquifer of south-central Texas is one of the most important karst aq...
The Balcones Fault Zone Edwards Aquifer of south-central Texas is one of the most important karst aq...
Karst development in the Edwards Aquifer has been significantly studied in the San Antonio and Barto...
Regional differences in the porosity and permeability of the Edwards aquifer are related to three ma...
In the subsurface of south-central Texas the Lower Cretaceous Edwards Formation consists of about 40...
Regional differences in the porosity and permeability of the Edwards aquifer are related to three ma...