Linked from

The 18 pages that link to Turbidite, each with the reason it gives.

• Marine sedimentBroader topic: Graded turbidite layers preserve evidence of episodic downslope sediment flows.

• Turbidity currentRelated: As the current loses speed, settling particles build a deposit that records its passage.

• Abyssal plainRelated: Repeated turbidite deposits can bury seafloor relief beneath thick, flat sediment.

• PaleoseismologyRelated: Some submarine earthquake histories are inferred from recurring turbidite layers.

• Continental slopeRelated: Turbidity currents that cross the slope leave layered deposits farther downslope.

• Graded beddingBroader topic: Many turbidites contain graded layers that record the waning current.

• Submarine landslideRelated: Turbidites can preserve evidence of landslide-triggered sediment flows.

• Chengjiang biotaRelated: Rapid sediment flows are proposed to have buried some Chengjiang organisms.

• VarveCompared with: Turbidites record individual flows, unlike varves' recurring annual deposition.

• Submarine fanRelated: Turbidites are common deposits within submarine fan channels and lobes.

• Forearc basinBroader topic: Turbidites commonly carry sediment into deep-water parts of forearc basins.

• Sedimentary structuresBroader topic: Its sedimentary structures record the changing flow of a turbidity current.

• Continental riseBroader topic: Turbidites record individual sediment flows that contribute to rise strata.

• FlyschBroader topic: Turbidites are the characteristic event beds that compose many flysch successions.

• Sediment gravity flowBroader topic: Turbidity currents leave deposits that record the passage and waning of a sediment gravity flow.

• GreywackeBroader topic: Greywacke commonly occurs as the coarse part of a turbidite bed.

• Campos BasinRelated: Deepwater turbidite sandstones provide major reservoir rocks in Campos fields.

• Soft-sediment deformation structuresRelated: Rapid deposition by turbidity currents can trigger loading and deformation.