Retroarc foreland systems form through the flexural deflection of the lithosphere in response
to a combination of supra-and sublithospheric loads. Supracrustal loading by orogens leads …

Abstract The Western Interior Basin extends north–south over about 35° of latitude, from
Texas to the Northwest Territories, a distance of more than 3,000 km. The basin developed …

Principles of Sequence Stratigraphy, Second Edition presents principles to practical
workflow that guide applications in a consistent manner that is independent of model …

The study and interpretation of the textures, sedimentary structures, fossils, and lithologic
associations of sedimentary rocks on the scale of an outcrop, well section, or small segment …

The four‐part districting scheme (wedge‐top, foredeep, forebulge, and backbulge
depozones) applies to many foreland basin systems worldwide, but significant variations …

Discontinuity-bounded late Quaternary sequences in the southern Gangetic Plains
(Himalayan Foreland Basin) reflect floodplain aggradation and degradation in response to …

Deposits of lowstand deltas formed on the floor of the Cretaceous Interior seaway of North
America are found in the Cenomanian, lower Belle Fourche Member of the Frontier …

The aim of this research is to understand the tectonic setting of the Bauru Basin. This basin
in central-eastern South America has been classified as intracratonic, but the basin-fill …

New lithostratigraphic and chronostratigraphic, geochronologic, and sedimentary petrologic
data illuminate the history of development of the North American Cordilleran foreland basin …

The syn-tectonic Sobrarbe deltaic complex (Eocene of the Ainsa Basin, Spanish Pyrenees)
is confined by lateral thrust ramps and influenced by intra-basinal growth anticlines. Six …