FN Archimer Export Format
PT J
TI Bathy-morphological setting of Terceira Island (Azores) after the FAIVI cruise
BT 
AF CHIOCCI, F. L.
   ROMAGNOLI, C.
   CASALBORE, D.
   SPOSATO, A.
   MARTORELLI, Eleonora
   ALONSO, B.
   CASAS, D.
   CONTE, A. M.
   DI BELLA, L.
   ERCILLA, G.
   ESTRADA, Ferran
   FALESE, F.
   FARRAN, M.
   FORLEO, V.
   FREZZA, V.
   HIPOLITO, A.
   LEBANI, A.
   MAISTO, F.
   PACHECO, J.
   PIMENTEL, A.
   QUARTAU, Rui
   ROQUE, C.
   SAMPAIO, I.
   SANTORO, P. C.
   TEMPERA, Fernando
AS 1:1;2:2;3:3;4:3;5:3;6:4;7:5;8:6;9:1;10:4;11:4;12:1;13:4;14:1;15:1;16:7;17:1;18:1;19:7;20:7;21:8;22:8;23:9;24:1;25:9;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;
C1 Univ Roma La Sapienza, Dipartimento Sci Terra, I-00185 Rome, Italy.
   Univ Bologna, Dipartimento Sci Biol Geol & Ambientali, Bologna, Italy.
   CNR, Ist Geol Ambientale & Geoingn, Rome, Italy.
   Inst Ciencias Mar CMIMA CSIC, Dept Geol Marina, Barcelona, Spain.
   Inst Geol & Minero Espana, Madrid, Spain.
   CNR, Ist Geosci & Georisorse, Rome, Italy.
   Univ Acores, Ctr Vulcanol & Avaliacao Riscos Geol, Ponta Delgada, Portugal.
   Lab Nacl Energia & Geol, Lisbon, Portugal.
   Univ Acores, Dept Oceanog & Pescas, Ponte Delgada, Portugal.
C2 UNIV ROMA LA SAPIENZA, ITALY
   UNIV BOLOGNA, ITALY
   IAMC CNR, ITALY
   CSIC, SPAIN
   IGME, SPAIN
   IAMC CNR, ITALY
   UNIV ACORES, PORTUGAL
   LNEG, PORTUGAL
   UNIV ACORES, PORTUGAL
SI AUTRE
SE AUTRE
IF 0.895
TC 27
UR https://archimer.ifremer.fr/doc/00256/36757/35362.pdf
   https://archimer.ifremer.fr/doc/00256/36757/37056.pdf
LA English
DT Article
CR FAIVI 1
BO Haliotis
DE ;multibeam bathymetry;geomorphology;submarine volcanism;tectonics;erosive-depositional features
AB High-resolution morpho-bathymetric data at 1:200,000 scale obtained during the FAIVI cruise (2011) and the resulting geomorphologic map of the Terceira island offshore area (central Azores, Portugal) are presented for the first time. The uneven morphology around Terceira is primarily related to volcanic features, such as linear and cone-shaped eruptive centres and lava flows. Such features are mostly concentrated on volcanic ridges and are aligned along preferential axes, suggesting a strong interaction between tectonics and volcanic processes. The occurrence of active tectonics is also demonstrated by systems of faults cutting the seafloor to the north, east and south of the island. Mapped erosive-depositional features include an insular shelf located at < 150 m water depth (wd), small landslide headwalls, erosive scarps, channelized features and crescent-shaped bedforms. The presented map may represent the base for a first-order geo-hazard assessment.
PY 2013
PD OCT
SO Journal Of Maps
SN 1744-5647
PU Taylor & Francis Ltd
VL 9
IS 4
UT 000325090600014
BP 590
EP 595
DI 10.1080/17445647.2013.831381
ID 36757
ER

EF