Gemma Aiello

Institute of Marine Sciences - National Research Council ISMAR-CNR

Dr. Gemma Aiello was born in Aversa (CE), Italy on 24 October 1964. In 1989, she graduated in Geological Sciences at the University of Naples “Federico II”, Department of Earth Sciences. In 1993, she earned a PhD degree in Sedimentary Geology at the University of Naples “Federico II”, Department of Earth Sciences, Faculty of Geological Sciences. She completed a 2-year post-doctoral fellowship at the University of Naples “Federico II”, a CNR-CEE fellowship and several research contracts at the Italian CNR, where she is researcher from 1998. Dr. Aiello has a consolidated experience in the field of sedimentary geology, marine geology and geophysics and has participated in many research projects at the National Research Council of Italy (CARG, Vector, Centri Regionali di Competenza, Tessa, I_Amica).

3books edited

5chapters authored

Latest work with IntechOpen by Gemma Aiello

This book contains six chapters dealing with the investigation of seismic and sequence stratigraphy and integrated stratigraphy, including the stratigraphic unconformities, in different geological settings and using several techniques and methods, including the seismostratigraphic and the sequence stratigraphic analysis, the field geological survey, the well log stratigraphic interpretation, and the lithologic and paleobotanical data. Book chapters are separated into two main sections: (i) seismic and sequence stratigraphy and (ii) integrated stratigraphy. There are three chapters in the first section, including the application of sequence and seismic stratigraphy to the fine-grained shales, to the fluvial facies and depositional environments, and to the Late Miocene geological structures offshore of Taiwan. In the second section, there are three chapters dealing with the integrated stratigraphic investigation of Jurassic deposits of the southern Siberian platform, with the stratigraphic unconformities, reviewing the related geological concepts and studying examples from Middle-Upper Paleozoic successions; and, finally, with the integrated stratigraphy of the Cenozoic deposits of the Andean foreland basin (northwestern Argentina).

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