The student at the end of the course:
- He will be able to analyze and interpret: on a regional and local scale, geological, morphological, geophysical and geodetic data in areas affected by volcano-tectonic processes;
- Sarà pertanto in grado di rilievare geostrutture ricollegabili ad attività tettonica e vulcanica, definire le interrelazioni tra geometria, cinematica e dinamica di origine tettonica e vulcanica nonché valutare l’ordine di grandezza spazio-temporale dei distinti geoprocessi;
- Sarà in grado di pianificare con metodologia multidisciplinare lo studio vulcano-tettonico di domini interessati da vulcanismo in differenti contesti tettonici, ed esporne i contenuti con linguaggio tecnico appropriato
"42 ore (6 CFU) di lezioni frontali” - 42 hours (6 CFU) teacher-led discussion
La conoscenza dei processi geodinamici, Tettonica globale, strutture tettoniche attività sismica e vulcanica, domini tettonici di tipo collisionale, di subduzione, rift continentali, meccanismi di deformazione fragile e duttile, Tettonica e geomorfologia
FREQUENZA LEZIONI: obbligatoria. Lo studente dovrà frequentare almeno il 70% delle lezioni (lezioni frontali e/o laboratorio). Il docente verificherà la presenza in aula e compilerà un registro delle presenze. |
This course combine results frackture mechanics, rock mechanics structural geology, hydrology, and fluid transport in the crust to explore and explain fracture processes and fluid transport in the crust. Basic concept are developed for first principlesand are illustrated with numerous worked examplesthat link models of volcano tectonics processes to real field observations and measurements.
Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press
http://studium.unict.it/dokeos/2018/index.php
Argomenti | Riferimenti testi | |
1 | The topics enclosed are strictly related to volcanic environments, the application of the laws of structural geology and rock mechanics are discussed using the methodologies and experiences provided by the international scientific community that discussed the topics in experimentation and knowledge in the volcanic environment. | |
2 | SFORZO; (STRESS) | 1. Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press. |
3 | DISLOCAMENTO E DEFORMAZIONE; (DISPLACEMENT AND STRAIN) | 1. Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press. |
4 | RELAZIONI TRA SFORZI E DEFORMAZIONE; (RELATION BETWEEN STRESS AND STRAIN) | 1. Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press. |
5 | AUMENTO DI CARICO SINO A ROTTURA IN MEZZI MATERIALI ROCCIOSI A DEFORMAZIONE FRAGILE; (LOADING OF BRITTLE ROCKS TO FAILURE) | 1. Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press. |
6 | CONCENTRAZIONE DEGLI SFORZI; (STRESS CONCENTRATION) | 1. Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press. |
7 | TEORIE SULLA DEFORMAZIONE FRAGILE DELLE ROCCE; (THEORIES OF BRITTLE FAILLURE OF ROCKS) | 1. Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press. |
8 | FRATTURE ESTENSIONALI E DI TAGLIO; (EXTENSION FRACTURES AND SHEAR FRACTURES) | 1. Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press. |
9 | DISLOCAZIONE E FRATTURE DA SFORZO; (DISPLACEMENT AND DRIVING STRESSES OF FRACTURES) | 1. Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press. |
10 | FLUID TRASPORT IN ROCKS - THE BASICS | 1. Rock Fractures in Geological Processes. Agust Gudmundsson Cambridge Univeristy Press. |
11 | VULCANO TETTONICA NEL DOMINIO DEL COMPLESSO VULCANICO ETNEO (VOLCANO-TECTONICS IN THE ETNA VOLCANO DOMAIN) | Dispense fornite dal docente (The copy of teaching material will be provided by the teacher) |
Concept evaluation remains a fundamental tool so that to comprehend the origin of the obstacles faced by students while their learning of the concept of volcano-tectonics. Many verify methods can be used such as a questionnaire, an interview, observation, and other methods: In this course, we chose all of these as a evaluation tool. On the one hand, this choice is designed to have a more comprehensive view on students' conceptions, but also to give them the freedom to respond and choose elements they deem correct answers.
Relation between regional tectonic and vocanism
What is the internal structure and composition of the Etna volcano substratum?
Giving a definition of different type of crust?
How are homes earthquakes distributed on different type volcano-tectonics domain? What is the reason ?
Stress concentration
What is the difference between extensional fractures and hidro fractures?
Criteria of mechanical deformation