A mixed carbonate-siliciclastic succession developed on the southern margin of the Bonifacio Basin (Cala di Labra, SE Corsica) during the Burdigalian, in the margin of a back-arc setting which had formed during the Sardinia-Corsica block rotation. This shallow marine setting was fed by abundant nearshore siliciclastic supply, and substantial carbonate production/accumulation increased from the euphotic to the oligophotic zones. Two third-order depositional sequences (SD1,SD2) corresponding to Bur 3 and Bur4, are recorded in the sedimentary succession. (C) 2013 Elsevier B.V. All rights reserved.
Sea level changes recorded in mixed siliciclastic-carbonate shallow-water deposits: The cala di labra formation (burdigalian, corsica) / Tomassetti, Laura; Brandano, Marco. - In: SEDIMENTARY GEOLOGY. - ISSN 0037-0738. - 294:(2013), pp. 58-67. [10.1016/j.sedgeo.2013.05.005]
Sea level changes recorded in mixed siliciclastic-carbonate shallow-water deposits: The cala di labra formation (burdigalian, corsica)
TOMASSETTI, LAURA
Writing – Original Draft Preparation
;
2013-01-01
Abstract
A mixed carbonate-siliciclastic succession developed on the southern margin of the Bonifacio Basin (Cala di Labra, SE Corsica) during the Burdigalian, in the margin of a back-arc setting which had formed during the Sardinia-Corsica block rotation. This shallow marine setting was fed by abundant nearshore siliciclastic supply, and substantial carbonate production/accumulation increased from the euphotic to the oligophotic zones. Two third-order depositional sequences (SD1,SD2) corresponding to Bur 3 and Bur4, are recorded in the sedimentary succession. (C) 2013 Elsevier B.V. All rights reserved.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
