Results 91 to 100 of about 16,283 (208)

The Mansurovo Formation of the West Magnitogorsk Zone in the Southern Urals: Stratigraphy, Composition and Sedimentary Environments

Georesursy
Research subject. Mansurovo formation (the (?)Silurian–Lower Devonian) in the Western Magnitogorsk zone of the Southern Urals, outcropped in the same-name village vicinity.   Aim.
A. M. Fazliakhmetov, O. Ju. Melnichuk, V. F. Juldashbaeva   +2 more
doaj   +1 more source

RRS James Cook Cruise 36, 19 Jul-28 Jul 2009. The Geobiology of Whittard Submarine Canyon [PDF]

, 2009
The biological and geological research programme for James Cook cruise 36 was built around a series of ROV video transects to determine variations in species and community structure and composition in different geological and topographic settings down ...
Masson, D.G.
core  

Application of micro‐CT to resolve textural properties and assess primary sedimentary structures of deep‐marine sandstones

The Depositional Record
Over the past decade, there has been growing interest in the sedimentological community to use micro X‐ray computed tomography to analyse microfacies in sediment cores.
P. H. Cornard, G. Degenhart, P. Tropper, J. Moernaut, M. Strasser   +4 more
doaj   +1 more source

Postglacial (after 18 ka) deep-sea sedimentation along the Hikurangi subduction margin (New Zealand): Characterisation, timing and origin of turbidites [PDF]

, 2012
International audienceRecent sedimentation along the Hikurangi subduction margin off northeastern New Zealand is investigated using a series of piston cores collected between 2003 and 2008.
Lamarche, Geoffroy, Neil, Helen, Orpin, Alan, Pouderoux, Hugo, Proust, Jean-Noël   +4 more
core   +3 more sources

RRS Charles Darwin Cruise 126, 11 Mar-20 Mar 2001. Piston coring of debris flows and turbidites west and south of the Canary Islands [PDF]

, 2002
The major cruise objective was to obtain sediment cores at various locations to the west and southwest of the Canary Islands with the aims of :· Sampling debris flow sediments in the Canary and Saharan debris flows· Obtaining dateable sediments ...
Masson, D.G.
core  

Investigations on the Peach 4 Debrite, a Late Pleistocene Mass Movement on the Northwest British Continental Margin [PDF]

, 2010
The Peach 4 debrite is the most recent in a series of large scale Pleistocene MTDs within the Barra fan on the northwest British continental margin. Geophysical data indicate that Peach 4 was formed through a combination of blocky and muddy debris flows
D Kroon, D Kroon, DAV Stow, DJW Piper, E Tripsanas, JE Armishaw, JP Coakley, K Wien, M Blanchard, M Maslin, M Owen, NJ Cook, PC Knutz, PC Knutz, R Fairbanks, RA Berner, RD Jacobi, RW Embley, WR Normark   +18 more
core   +2 more sources

FACIES AND ARCHITECTURE OF A SAND-RICH TURBIDITE SYSTEM IN AN EVOLVING COLLISIONAL-TRENCH BASIN: A CASE HISTORY FROM THE UPPER CRETACEOUS-PALAEOCENE GOTTERO SYSTEM (NW APENNINES)

Rivista Italiana di Paleontologia e Stratigrafia, 2019
This study documents the main depositional elements of a dynamically-controlled sand-rich deep-water turbidite system (Upper Cretaceous–Palaeocene Gottero system, north-west Italy).
MARCO FONNESU, FABRIZIO FELLETTI
doaj   +1 more source

Craven Basin and southern Pennines [PDF]

, 2011
Carboniferous rocks within this area occupy the region contiguous with the northern Pennines to the north (Chapter 12) and the Peak District to the south (Chapter 10).
Cleal, C.J., Collinson, J.D., Jones, N.S., Waters, C.N.   +3 more
core  

Continental Growth and Recycling in Convergent Orogens with Large Turbidite Fans on Oceanic Crust

Geosciences, 2013
Convergent plate margins where large turbidite fans with slivers of oceanic basement are accreted to continents represent important sites of continental crustal growth and recycling.
Ben D. Goscombe, David A. Foster
doaj   +1 more source

Overview and Reinstatement of Some Geophysical Interpretations in the Eastern Sava Depression

Rudarsko-geološko-naftni Zbornik, 2015
The eastern part of Sava Depression is bounded on the south with the Sava River and on the north with Psunj Mountain, Požeška and Dilj Hills. In this part thicker Neogene-Quaternary sediments than in the western part were found, and there is almost never
Tihana Ružić
doaj   +1 more source