
Abyssal fan - Wikipedia
Abyssal fans, also known as deep-sea fans, underwater deltas, and submarine fans, are underwater geological structures associated with large-scale sediment deposition and formed …
深海扇 - 维基百科,自由的百科全书
2022年12月10日 · 深海扇(英语: abyssal fan ),又称海底扇、如同陆上冲积扇外形,但它是由浊积流形成的沉积构造。深海扇的规模有很大差异,宽度从几公里到几千公里不等。
6.17: Deep Sea Fan, Turbidite Deposits, and Abyssal Clays
2021年2月15日 · Deep Sea Fan, Turbidite Deposits, and Abyssal Clays. A deep-sea fan is a fan- or delta-shaped sedimentary deposit found along the base of the continental slopes, …
Submarine fan | Deep-Sea, Sedimentation & Turbidity | Britannica
Submarine fan, accumulation of land-derived sediment on the deep seafloor; in configuration, a fan is like the section of a very low cone, with its apex at the lower mouth of a submarine …
Abyssal fan - Simple English Wikipedia, the free encyclopedia
Abyssal fans are underwater geological formations formed by turbidity currents. It is also called deep-sea fans, underwater deltas, and submarine fans. They can be several kilometres long …
The abyssal bounty fan and lower Bounty Channel: evolution of a …
1996年3月1日 · The Bounty Fan is located 800 km further east, where the Bounty Channel debouches onto abyssal oceanic crust at the mouth of the Bounty Trough. The Bounty Fan …
A dimensionless framework for predicting submarine fan …
2022年12月8日 · Submarine fans form on continental slopes and abyssal plains in deepwater settings and are the ultimate sinks in sediment routing systems. They are crafted by turbidity …
Abyssal fan of Geography Topics | Question AI
Abyssal fans , also known as deep-sea fans , underwater deltas , and submarine fans , are underwater geological structures associated with large-scale sediment deposition and formed …
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Submarine Fans and Their Channels, Levees, and Lobes
2017年7月19日 · Submarine fans are complex morphological features that develop on the continental slope, rise and abyssal plain, normally at the mouths of submarine canyons. They …
10(p) Physiography of the Ocean Basins - Physical Geography
Each canyon's thick fan-shaped sedimentary deposit is called an abyssal fans. The ocean floor is found at the base of the continental rise in water 4000 to 6000 meters deep (see Figure 10p-1 ).
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