Results 151 to 160 of about 776 (184)

Turbidite Facies Associations

1984
Abstract There are three major turbidite facies associations: slope, deep-sea fan, and basin-plain (Fig. 9-1). These can be subdivided, from generally most “proximal” to most “distal”, into: (1) upper slope, (2) lower slope, (3) submarine canyon, (4) inter-fan channel, (5) middle-fan channel, (6) levee, (7) interchannel, (8) outer-fan
openaire   +1 more source

turbidite, n.

2023
openaire   +1 more source

Intrabasinal and extrabasinal turbidites: Origin and distinctive characteristics

Sedimentary Geology, 2016
CARLOS Zavala
exaly  

Middle Miocene reworked turbidites in the Baiyun Sag of the Pearl River Mouth Basin, northern South China Sea margin: Processes, genesis, and implications

Journal of Asian Earth Sciences, 2016
Dorrik Stow, Chenglin Gong, Rachel Brackenridge   +2 more
exaly  

Turbidites

2012
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Provenance of Palaeozoic turbidites in the Lachlan Orogenic Belt: Strontium isotopic evidence

Australian Journal of Earth Sciences, 1995
John Webb, C M Gray
exaly  

Turbidites

2006
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Re-evaluation of contact relationships between Ordovician volcanic belts and the quartz-rich turbidites of the Lachlan Orogen

Australian Journal of Earth Sciences, 2007
Sébastien Meffre, R A Glen
exaly  

Synsedimentary structural control on foredeep turbidites: An example from Miocene Marnoso-arenacea Formation, Northern Apennines, Italy

Marine and Petroleum Geology, 2011
Roberto Tinterri
exaly  

Turbidite

2011
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