Late quaternary stratigraphic setting of the Sibari Plain (southern Italy): Hydrogeological implications

被引：8

作者：

Cianflone, Giuseppe ^{[1
]}

Cavuoto, Giuseppe ^{[2
]}

Punzo, Michele ^{[2
]}

Dominici, Rocco ^{[1
]}

Sonnino, Maurizio ^{[1
]}

Di Fiore, Vincenzo ^{[2
]}

Pelosi, Nicola ^{[2
]}

Tarallo, Daniela ^{[2
]}

Lirer, Fabrizio ^{[2
]}

Marsella, Ennio ^{[2
]}

Critelli, Salvatore ^{[1
]}

De Rosa, Rosanna ^{[1
]}

机构：

[1] Univ Calabria, Dept Biol Ecol & Earth Sci DiBEST, Cube 15B, I-87036 Arcavacata Di Rende, CS, Italy

[2] Italian Natl Res Council CNR, Inst Coastal Marine Environm IAMC, I-80133 Naples, Italy

来源：

MARINE AND PETROLEUM GEOLOGY | 2018年 / 97卷

关键词：

Sibari Plain; Stratigraphy; Electrical resistivity tomography; Crati delta; ELECTRICAL-RESISTIVITY TOMOGRAPHIES; CALABRIAN ARC; TECTONIC EVOLUTION; NORTHERN CALABRIA; ACTIVE TECTONICS; REGIONAL UPLIFT; MARINE TERRACES; DETRITAL MODES; IONIAN SEA; HOLOCENE;

D O I：

10.1016/j.marpetgeo.2018.07.027

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The aim of this study is the reconstruction of the late Pleistocene-Holocene stratigraphy of the Sibari Plain (southern Italy) aimed to obtain information about hydrogeological framework. A multidisciplinary approach combining boreholes data and Electrical Resistivity Tomography, allowed us to recognize three electro-stratigraphic units, which consist of upper Pleistocene fluvial and floodplain-littoral facies (deep aquifer), passing upward to Holocene marine-transitional deposits (aquiclude) evolving toward continental sediments (shallow aquifer) related to the Crati delta progradation. The late Quaternary-Holocene plain evolution took place in a tectonic-controlled setting and was driven by the interaction between sea-level variations and local factors. The presence of a NE-SW fault zone controlled the facies and thickness of Holocene sediments along strike of the fault. This active fault zone contributed to determine the plain stratigraphic architecture, the arrangement of the depositional environments, and consequently the stratigraphic pattern.

引用

页码：422 / 436

页数：15

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