By D. Gapais, J. P. Brun, P. R. Cobbold
This publication contains 18 papers on deformation mechanisms, rheology and tectonics. the most methods comprise experimental rock deformation, microstructural research, box structural experiences, analogue and numerical modeling. New effects on a number of themes are awarded, starting from brittle to ductile deformation and grain-scale to lithosphere-scale mechanisms. the quantity comprises overview papers on numerous significant present issues, resembling the rheology of the lithospheric mantle and the mechanisms of exhumation of high-pressure tectonic devices, in addition to learn papers on kinematic and mechanical research of rock deformation and comparable new innovations. a number of contributions emphasize the expanding skill and need of researchers to reinforce the hyperlinks among small-scale actual mechanisms and large-scale tectonics. the quantity should be of curiosity to educational and business researchers within the fields of structural geology, interactions among metamorphism, fluids and deformation, and large-scale tectonic processes.Also on hand: The Initiation, Propagation, And Arrests of Joints And different Fractures - ISBN 1862391653 movement methods in Faults And Shear Zones - ISBN 186239153X Deformation Mechanisms, Rheology and Tectonics: present prestige and destiny views - ISBN 1862391173
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Extra info for Deformation Mechanisms, Rheology and Tectonics: From Minerals to the Lithosphere (Geological Society Special Publication No. 243)
1999. Rupture directivity of the major shocks in the 1997 Umbria-Marche (central Italy) sequence from regional broadband waveforms. Geophysical Research Letters, 26(14), 2101-2104. PIZZI, A. & SCISIANI, V. 2000. Methods for determining Pleistocene-Holocene displacement in active faults reactivating pre-Quaternary structures. Example from the central Apennines (Italy). Journal of Geodynamics, 29, 445-457. , COLTORTI, M. & I~ERUCC~NI, P. 2002. Quaternary normal faults, intramontane basins and seismicity in the Umbria-Marche-Abrnzzi Apennine ridge (Italy): contribution of neotectonic analysis to seismic hazard assessment.
Evidence for surface faulting during the September 26, 1997 Colfiorito (Central Italy) earthquakes. Journal of Earthquake Engineering, 2, 1-22. CHIARABBA, C. 8r AMATO, A. 2003. 0 Colfiorito fault region (central Italy): A contribution to the understanding of seismotectonic and seismogenic processes. Journal of Geophysical Research, 108, 2248. , CHIARABBA,C. & Cocco, M. 2003. Imaging the complexity of an active complex normal fault system: the 1997 Colfiorito (central Italy) case study. 1029/ 2002JB002166.
C) Mohr circle diagrams for (b). The diagram on the left-hand side marks three successive stages during the compaction process. The diagram on the right-hand side shows the successive growth of the Mohr circle during tectonic deformation and the following failure that produces the dominant conjugate mode lI fractures. Note that the x-axis is negative towards the right-hand side since compressive stresses are negative in this paper. 20 D. KOEHN ET AL. of the vertical line in Figure 9b indicates the gravitational loading regime (marked L for loading).