Summary

Upper Cretaceous (Cenomanian-Turonian) Eagle Ford Group equivalent strata in west Texas (Ojinaga, Boquillas Formations) can be correlated with subsurface Eagle Ford Group strata in south Texas using hand-held spectral gamma-ray logs on outcrops, biostratigraphy, stable isotopes and U/Pb geochronology. These correlations indicate that some of these units are incompletely recorded even though they do not preserve evidence for long-term exposure.

The Ojinaga Formation outcrops in west Texas records only Cenomanian strata based on its high uranium abundance throughout and biostratigraphy. Multiple ash beds correspond to thorium spikes. Sedimentary structures are limited to hummocky cross stratification (HCS) within the lower 30 feet. In Big Bend National Park two detailed measured sections (Hot Springs and Ernst Tinaja) of Boquillas Formation strata also suggest much of the Cenomanian is recorded but the Turonian portion is only partially preserved; specifically, neither of these sections preserves strata equivalent to Ocean Anoxic Event 2 (OAE2) that spans the Cenomanian-Turonian boundary. The Lower Eagle Ford Group of each section has elevated uranium abundance and contains abundant HCS. The Upper Eagle Ford Group at both sections has little uranium and few wave generated structures.

At Lozier Canyon in Terrell County (west Texas) approximately 80 miles (130 km) to the east of Big Bend National Park, an almost complete section of the Eagle Ford Group is well preserved. Here the Lower Eagle Ford Group has abundant uranium and molybdenum (Mo), whereas the Upper Eagle Ford Group has much less of these two elements. The Lower Eagle Ford Group here contains abundant HCS and transitions upward into bioturbated skeletal wackestone/packstone. The stable isotope excursion associated with OAE2 is truncated at this section indicating a short-lived unconformity in this section.

Subsurface correlation of multiple cores and wireline logs of the Eagle Ford Group in south and west Texas indicate that its thickness increases to the south into the Maverick Basin.

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