Deformations formed in unconsolidated sediments are known as soft-sediment deformation
structures. Their nature, the time of their genesis, and the state in which the sediments …

Calciclastic submarine fans are rare in the stratigraphic record and no bona fide present-day
analogue has been described to date. Possibly because of that, and although calciclastic …

This paper focuses on soft-sediment deformation structures (SSDS) in both siliciclastic and
carbonate storm deposits of the Cambrian Mantou and Chaomidian formations (Shandong …

Outcrops and cores from the top of the lacustrine Tipton Member and the base of the Wilkins
Peak Member (~ 51.5 Ma) of the Eocene Green River Formation, Bridger Basin in …

This paper focuses on the formative processes of limestone pseudoconglomerates in the
Gushan and Chaomidian Formations (Late Cambrian) of the North China Platform …

Ribbon rocks are characterized by an alternation of millimeter-to centimeter-thick limestone
and argillaceous deposits (marlstone or shale). The sedimentary processes and diagenetic …

Lakes are common natural systems for which sedimentation is considered to be relatively
simple, generally dominated by fluvial processes along the margin and prevailing low …

The development history of an oligo-mesophotic, early Miocene, isolated carbonate system
(> 160 m in thickness), forming the uppermost part of the Oligo-Miocene Yadana buildup …

Uppermost Jurassic limestones of the South‐East Basin (France) are organized into four
facies associations that were deposited in four distinct zones:(1) peritidal lagoonal …

A coarse-grained sandstone bed of Cretaceous/Paleogene (K/Pg) boundary age occurs in a
homogeneous neritic shelf mudstone sequence (Jagüel Formation) in the Neuquén Basin of …