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Teapot Dome
Deep learning for multidimensional seismic impedance inversion
Dictionary learning with convolutional structure for seismic data denoising and interpolation
Missing well log prediction using convolutional long short-term memory network
Relative time seislet transform
Spectral structure-oriented filtering of seismic data with self-adaptive paths
Flow diagnostics for naturally fractured reservoirs
Missing log data interpolation and semiautomatic seismic well ties using data matching techniques
Automatic blind deconvolution with Toeplitz-structured sparse total least squares
Incremental correlation of multiple well logs following geologically optimal neighbors
Least-squares horizons with local slopes and multigrid correlations
An overview of reproducible 3D seismic data processing and imaging using Madagascar
Interpretation of fractured zones using seismic attributes — Case study from Teapot Dome, Wyoming, USA
Improved estimates of seismic curvature and flexure based on 3D surface rotation in the presence of structure dip
Fracture intensity attribute for the Tensleep reservoir at Teapot Dome, Wyoming, USA
Discrete 3D fracture network extraction and characterization from 3D seismic data — A case study at Teapot Dome
Developing a model discrete fracture network, drilling, and enhanced oil recovery strategy in an unconventional naturally fractured reservoir using integrated field, image log, and three-dimensional seismic data
Surface geochemical measurements applied to monitoring, verification, and accounting of leakage from sequestration projects
Extreme curvature and extreme flexure analysis for fracture characterization from 3D seismic data: New analytical algorithms and geologic implications
Diffraction imaging in fractured carbonates and unconventional shales
We review the extensive record of plant fossils before, at, and after the Cretaceous-Paleogene event horizons, recognizing that key differences between plants and other organisms have important implications for understanding the patterns of environmental change associated with the Cretaceous-Paleogene event. Examples are given of the breadth of prior environmental conditions and ecosystem states to place Cretaceous-Paleogene events in context. Floral change data across the Cretaceous-Paleogene are reviewed with new data from North America and New Zealand. Latest Cretaceous global terrestrial ecology was fire prone and likely to have been adapted to fire. Environmental stress was exacerbated by frequent climate variations, and near-polar vegetation tolerated cold dark winters. Numerous floristic studies across Cretaceous-Paleogene event horizons in North America attest to continent-wide ecological trauma, but elsewhere greater floral turnover is sometimes seen well before the Cretaceous-Paleogene boundary rather than at it. Data from the Teapot Dome site (Wyoming) indicate continued photosynthesis, but during or immediately after the Cretaceous-Paleogene event, growth was restricted sufficiently to curtail normal plant reproductive cycles. After the Cretaceous-Paleogene transition in New Zealand, leaf form appears to have been filtered for leaves adapted to extreme cold, but at other high-southern-latitude sites, as in the Arctic, little change in floral composition is observed. Although lacking high-resolution (millimeter level) stratigraphy and Cretaceous-Paleogene event horizons, gradual floral turnover in India, and survival there of normally environmentally sensitive taxa, suggests that Deccan volcanism was unlikely to have caused the short-term trauma so characteristic elsewhere but may have played a role in driving global environmental change and ecosystem sensitivity prior to and after the Cretaceous-Paleogene boundary.