Flaggy strata of marine elastic limestone occur in the Eagle Ford shale at a horizon approximately 100 feet below the top of that formation in Dallas County. Anticipating the possible significance of these strata as marker beds useful in correlating the type section of the Eagle Ford here with sections exposed in other areas, a detailed description of them is given
The Late Cretaceous Chispa Summit Formation of west Texas has historically been of interest to the p...
Consolidated marine rocks of the Oak Cliff Quadrangle belong to a portion of the Upper Cretaceous Au...
In the subsurface of south-central Texas the Lower Cretaceous Edwards Formation consists of about 40...
Flaggy strata of marine elastic limestone occur in the Eagle Ford shale at a horizon approximately 1...
Bedrock in the Preston Hollow Quadrangle consists of the upper Eagle Ford shale and the middle marl ...
Eagle Ford shale of Upper Cretaceous age underlies the Carrollton quadrangle in Dallas and Denton co...
In the Cedar Hill Quadrangle, bedrock consists of the Eagle Ford shale and Austin chalk, both of Upp...
The Fort Hays Limestone is upper Cretaceous (Coniacian) in age and occurs in a wide area across the ...
The Upper Cretaceous Eagle Ford Shale, in South and East Texas, consists of organic matter-rich foss...
textHeightened industry focus on the Upper Cretaceous (Cenomanian-Turonian) Eagle Ford has resulted ...
The Midlothian quadrangle in northwest Ellis County, Texas, is underlain by the Eagle Ford Shale and...
A thick sequence of Lower Cretaceous limestone and dolomite, known traditionally and informally as “...
The Late Cretaceous Chispa Summit Formation of west Texas has historically been of interest to the p...
The Mississippian system confined to the subsurface between depths of 7,100 and 12,650 feet is compo...
Lower Cretaceous strata in central Texas are divisible into genetically related rock bodies. The Low...
The Late Cretaceous Chispa Summit Formation of west Texas has historically been of interest to the p...
Consolidated marine rocks of the Oak Cliff Quadrangle belong to a portion of the Upper Cretaceous Au...
In the subsurface of south-central Texas the Lower Cretaceous Edwards Formation consists of about 40...
Flaggy strata of marine elastic limestone occur in the Eagle Ford shale at a horizon approximately 1...
Bedrock in the Preston Hollow Quadrangle consists of the upper Eagle Ford shale and the middle marl ...
Eagle Ford shale of Upper Cretaceous age underlies the Carrollton quadrangle in Dallas and Denton co...
In the Cedar Hill Quadrangle, bedrock consists of the Eagle Ford shale and Austin chalk, both of Upp...
The Fort Hays Limestone is upper Cretaceous (Coniacian) in age and occurs in a wide area across the ...
The Upper Cretaceous Eagle Ford Shale, in South and East Texas, consists of organic matter-rich foss...
textHeightened industry focus on the Upper Cretaceous (Cenomanian-Turonian) Eagle Ford has resulted ...
The Midlothian quadrangle in northwest Ellis County, Texas, is underlain by the Eagle Ford Shale and...
A thick sequence of Lower Cretaceous limestone and dolomite, known traditionally and informally as “...
The Late Cretaceous Chispa Summit Formation of west Texas has historically been of interest to the p...
The Mississippian system confined to the subsurface between depths of 7,100 and 12,650 feet is compo...
Lower Cretaceous strata in central Texas are divisible into genetically related rock bodies. The Low...
The Late Cretaceous Chispa Summit Formation of west Texas has historically been of interest to the p...
Consolidated marine rocks of the Oak Cliff Quadrangle belong to a portion of the Upper Cretaceous Au...
In the subsurface of south-central Texas the Lower Cretaceous Edwards Formation consists of about 40...