Publication details for Dr Nicola De PaolaDe Paola, N., Collettini, C., Faulkner, D.R. & Trippetta, F. (2008). Fault zone architecture and deformation processes within evaporitic rocks in the upper crust. Tectonics 27(4).
- Publication type: Journal Article
- ISSN/ISBN: 0278-7407
- DOI: 10.1029/2007TC002230
- Further publication details on publisher web site
Author(s) from Durham
Recently, in the Northern Apennines, geophysical data have identified the Triassic Evaporites
(TE, anhydrites and dolomites) as the source region of the major extensional earthquakes of the area
(M~6). In order to characterize fault zone architecture and deformation processes within the TE, we
have studied exhumed evaporite-bearing normal faults within the upper crust.
The structure of large displacement (>100m) normal faults is given by: a) a zoned fault core
with a wider portion of fault-parallel foliated Ca-sulphates (ductile deformation), overprinted by an
inner fault core (IFC) of localized brittle deformation; b) wide (dolostones) to absent (Ca-sulphates)
damage zones of fault fracture patterns. Fault rock assemblage within the IFC is characterized by
fault breccia, gouge and cataclasites of different grain size. Most of the deformation within the IFC
is localized along thin and fault parallel principal slip surfaces (PSS) made of dolomite rich finegrained
cataclasite. SEM analyses show an evolution from Ca- to St- to gypsum-rich
mineralization, due to episodic fluid flow events channelled along the fault zones during different
stages of fault exhumation.
The development of the observed fault geometry can be explained by a mechanical fault
evolution model where initial faulting occurs along broad and ductile shear zones within the
anhydrites and causes fracturing within the dolostones. Progressive deformation within the fault
core leads to the development of fault parallel dolomite rich cataclastic layers. Their reactivation
coupled with transient fluid overpressures can produce embrittlement and localization of brittle
deformation within the IFC.