Titlebook: Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems; Paul Weimer,Martin H. Link Book 1991 Springer Science+Bu

淡紫色花

Exonerate

Modern Sand-Rich and Mud-Rich Siliciclastic Aprons: Alternative Base-of-Slope Turbidite Systems to Sall (several kilometers in length), have their apices at the base-of-slope, decrease gradually in thickness toward the basin center, and lie conformably on the basin floor without erosional truncation of underlying beds. Proximal aprons exhibit numerous discontinuous high-amplitude and wedging seism

AMPLE

隱語

Seismic Facies of Slope Basin Turbidite Reservoirs, East Breaks 160–161 Field: Pliocene-Pleistocene,ontinuous, variable amplitude, hummocky reflection character. The mapped pattern of this hummocky seismic facies has a linear to lobate pattern determined by intraslope basin geometry within the . A and a lobate distribution at the .. These hummocky seismic facies occur within the isochron thicks of

epicondylitis

Seismic and Depositional Facies of Paleocene-Eocene Wilcox Group Submarine Canyon Fills, Northwest Gsly dip along or across the canyon axis, reflecting infilling by progradation of subsequent delta lobes across the shelf and into the deep erosional depression created by the canyon. Hemipelagic drapes, visible as continuous reflections extending from canyon fill to adjacent shelf, indicate signific

懦夫

Seismic Facies of Shelf, Slope, and Submarine Fan Environments of the Lewis Shale, Upper Cretaceous,ggradation and progradation correlates with turbidite, slope, and deltaic sedimentation of the middle Lewis. (3) An upper unit of parallel reflections and tangential clinoforms represents mostly progradational deltaic, delta-front, and turbidite facies of the upper Lewis Shale and Fox Hills Sandston

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Seismic Stratigraphy of Lower Cretaceous Foreland Basin Submarine Fans in the North Slope, Alaskaic facies are characterized by parallel, moderate-amplitude reflections..Lowstand systems tracts are recognized that consist of basin floor fan and slope fan. Separate transgressive systems tracts have not been recognized, possibly because they are thin due to a slow sediment accumulation rate accom

Gustatory

Seismic Expression and Sedimentologic Characteristics of a Permian (Wolfcampian) Carbonate Submarineced primary porosity in carbonate grain-rich matrix and clasts..Distribution of the unit suggests that the sediments were pointsourced from the Eastern Shelf and developed into a series of bifurcating channels on the basin floor. Wells that produce from the Wolfcamp line up along these channels, ind

健忘癥

Book 1991omplished more constructively when people with different backgrounds join together at the same symposium and can read from the same volume rather than confining themselves within the world of their own specialty meetings and journals. Books in this series provide this connective link between discipl

催眠藥

0939-6055 can be accomplished more constructively when people with different backgrounds join together at the same symposium and can read from the same volume rather than confining themselves within the world of their own specialty meetings and journals. Books in this series provide this connective link between discipl978-1-4684-8276-8Series ISSN 0939-6055