Sedimentary signatures of the entrance of coarse-grained volcaniclastic flows into the sea: The example of the breccia units of the Las Palmas Detritic Formation (Mio - Pliocene, Gran Canaria, Eastern Atlantic, Spain)

Journal of Volcanology and Geothermal Research

Volumn 138, Issue 3-4, 2004, Pages 295-323

  Schneider, Jean Luc ^a   Pérez Torrado, Francisco J ^b   Gimeno Torrente, Domingo ^c   Wassmer, Patrick ^d   Cabrera Santana, María del Carmen ^b   Carracedo, Juan Carlos ^e  

^a UNIVERSITÉ DE BORDEAUX   (France)

^b UNIVERSITY OF LAS PALMAS DE GRAN CANARIA   (Spain)

^c UNIVERSITY OF BARCELONA   (Spain)

^d UNIVERSITÉ PARIS 1 PANTHÉON SORBONNE   (France)

^e INSTITUTO DE PRODUCTOS NATURALES Y AGROBIOLOGÍA   (Spain)

Author keywords

Block and ash flow; Canary Islands; Gran Canaria; Gravity flow seawater interaction; Magnetic fabric; Pyroclastic flow; Volcanic debris avalanche

Indexed keywords

BASALT; DEBRIS; GRAVEL; GRAVITATION; OCEANOGRAPHY; QUENCHING; SEDIMENTATION; SHORE PROTECTION; VOLCANIC ROCKS; VOLCANOES;

LAS PALMAS DETRITIC FORMATION (LPDF); THERMAL QUENCHING; VOLCANICLASTIC GRAVITY;

SEDIMENTARY ROCKS;

ASH FLOW; GRAVITY FLOW; MIOCENE; PLIOCENE; SEAWATER; SEDIMENTATION; VOLCANICLASTIC DEPOSIT;

ATLANTIC ISLANDS; ATLANTIC OCEAN; CANARY ISLANDS; EASTERN HEMISPHERE; EURASIA; EUROPE; GRAN CANARIA; LAS PALMAS; MACARONESIA; OCEANIC REGIONS; SOUTHERN EUROPE; SPAIN; WORLD;

EID: 11144246018     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2004.07.007     Document Type: Article

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