Page 310 - Caldera Volcanism Analysis, Modelling and Response
P. 310

CHA P T E R 7


                  Structural Development of Calderas: a

                  Synthesis from Analogue Experiments


                  Valerio Acocella




                  Contents

                  1. Introduction                                                 286
                  2. Analogue Modelling                                           287
                    2.1. General features                                         287
                    2.2. Materials and scaling                                    288
                  3. Experimental Studies on Calderas                             289
                    3.1. General features                                         289
                    3.2. Caldera collapse without regional stress field             291
                    3.3. Caldera collapse under a regional stress field            296
                  4. Discussion                                                   299
                    4.1. Consistency of the experiments                           299
                    4.2. Towards a consistent experimental model                   301
                  5. Comparison to Nature: Guidelines                             302
                  6. Towards a New Caldera Evolution Scheme                       305
                  7. Conclusions                                                  307
                  Acknowledgements                                                308
                  References                                                      308




                  Abstract
                  A number of analogue models studying caldera architecture and development have
                  been recently performed under different conditions (apparatus, materials, scaling
                  parameters, stress conditions). An overview of the experiments reveals a consistent
                  scenario for caldera structure and development, regardless of imposed boundary
                  condition. In fact, a complete collapse can be summarised through four main
                  stages, proportional to the amount of subsidence, progressively characterised by a:
                  (1) downsag; (2) reverse ring fault; (3) peripheral downsag and (4) peripheral normal
                  ring fault. A brief comparison to natural cases shows that all these experimental


              Corresponding author. Tel:. 0039-06-57338043; Fax: 0039-06-54888201
             E-mail address: acocella@uniroma3.it
             Dip. Scienze Geologiche Roma Tre, Roma, Italy
             Developments in Volcanology, Volume 10                     r 2008 Elsevier B.V.
             ISSN 1871-644X, DOI 10.1016/S1871-644X(07)00007-1            All rights reserved.
                                                                                  285
   305   306   307   308   309   310   311   312   313   314   315