WebTrough cross-bedding (Fig. 4) is formed in fine-grained sandstone in a lensoid sandbody, which indicates deposition in the sub-tidal environment (Reineck and Singh, 1980;Mowbray and Visser, 1984). Braided channels are marked by successive divisions and rejoinings of the flow around alluvial islands. Most braided river channels are … See more Lakes are standing water bodies filled primarily with fresh water. These shallow inland-restricted interdistributary lakes constitute an important environment in many upper delta plains and occur in all climatic settings. The … See more A meandering river is one with a channel pattern that displays high sinuosity in plan view (sinuosity greater than 1.5). Meanders are most commonly associated with rivers displaying … See more Literature on braided-channel deposits. 1. Allen, J. R. L., 1965a, Fining upward cycles in alluvial succession: Liverpool, Manchester, Geol. Jour., v. 4, p. 229-246. 2. Allen, J. R. L., … See more
槽状交错层理 晓茵万事通
WebTypes of Sedimentary Structures: We recognize two principle types: Primary sedimentary structures: occur in clastic sediments and produced by the same processes (currents, etc.) that caused deposition. Includes plane bedding and cross-bedding. Secondary sedimentary structures: are caused by post-depositional processes, including biogenic ... WebMar 21, 2016 · The seawardmost section of the subaqueous delta is commonly referred to as the prodelta environment and is composed of the finest material deposited from … donley ford of galion
What Is Trough Cross-Bedding? - theinteriorevolution.com
WebSep 12, 2016 · Trough cross bedding isn't restricted to sandstones. This sedimentary structure forms through the migration of dunes in subareal or subaqueous environments. … WebCross-bedded clastic limestone indicates shallow turbulent water, limestone, quiet water; massive organic structures, a reef. Graded bedding uncommon. Many rock types, gray shales. Most rocks outside mountain belts were deposited in … Web1 day ago · Based on factors such as color, gravel diameter, and structure that can reflect sedimentary origin and environment, lithofacies can be divided into 12 types: (1) Massive bedding gravelly medium sandstone ( Figure 3 a) often occurs in underwater distributary channel deposits, and reflects the sedimentary characteristics of tractive flow. city of decatur licensing department