3-D deformation pattern analysis and evolution of the Añisclo anticline, southern Pyrenees

Tavani, Stefano; Storti, Fabrizio; Fernández, Òscar; Muñoz, J. A.; Salvini, Francesco

doi:10.1016/j.jsg.2006.01.009

Cited by 66 publications

(70 citation statements)

References 57 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…Results indicate that, in the Guadagnolo and CBL formations, the analysed cleavage attributes are independent of the structural position. This supports the idea that the cleavage developed before any significant folding (Tavani et al, 2006).…”

Section: The Guadagnolo Anticlinesupporting

confidence: 84%

“…Relationships between cleavage attributes and structural position, which allow the relative timing of folding and cleavage to be deduced (Tavani et al, 2006), are investigated by dividing the dataset in sub-populations, according to the bedding dip. In particular, we divided the dataset into dip intervals of 108 and, for each sub-population, we computed the average and standard deviation of both the angle to bedding and the spacing.…”

Section: The Guadagnolo Anticlinementioning

confidence: 99%

See 1 more Smart Citation

Deformation pattern analysis and tectonic implications of a décollement level within the Central Apennines (Italy)

Tavani

Cifelli

2010

Geological Journal

View full text Add to dashboard Cite

This work reports structural and anisotropy of magnetic susceptibility (AMS) measurements from an Upper Miocene décollement level exposed in the central Apennine fold-and-thrust belt of Italy. The décollement level is located at the boundary between the MesozoicCenozoic carbonate sequence and the overlying Miocene-Pliocene syn-orogenic siliciclastic sediments and consists of a thick shear zone, mainly affecting detritic limestones, dominated by pressure solution cleavage oblique to the bedding.In the study area, the décollement level was active during the early stages of evolution of the fold-and-thrust belt, when deeper décollement levels were active in more internal zones, and accounted for the bulk top-to-foreland translation of the siliciclastic portion of the multilayer. The increasing deformation led to the progressive foreland migration of deeper décollement levels (and of thrusts emanating from these levels) that were active in the more internal sectors. Consequently, the Mesozoic-Cenozoic carbonate sequence was folded and faulted and the studied décollement became inactive and was incorporated into the fold-and-thrust belt. Pressure solution cleavage within the décollement became a passive marker that underwent rotations associated with later deformational phases. Results indicate that pressure solution cleavage registers two phases of deformation: (1) during thrusting and folding, when beds were folded and (2) at a later stage, when cleavage was rotated, together with thrusts and folds, about vertical axes. This second stage is interpreted as having been induced by the oblique inversion of a Liassic normal fault, during the Miocene compression.

show abstract

Section: The Guadagnolo Anticlinesupporting

confidence: 84%

Section: The Guadagnolo Anticlinementioning

confidence: 99%

Deformation pattern analysis and tectonic implications of a décollement level within the Central Apennines (Italy)

Tavani

Cifelli

2010

Geological Journal

View full text Add to dashboard Cite

show abstract

“…Tavani et al, 2006). We did not collect joint aperture data due to the poor reliability imparted them by the fact that the chalk underwent significant uplift and erosion, and that the studied exposures were produced by recent quarrying.…”

Section: Structural Datamentioning

confidence: 99%

“…Wise et al, 1985), cleavage (e.g. Salvini et al, 1999;Tavani et al, 2006), joint (e.g. Balsamo et al, 2008), and subsidiary fault population analysis (e.g.…”

Section: Structural Datamentioning

confidence: 99%

Sub-seismic scale fracture pattern and in situ permeability data in the chalk atop of the Krempe salt ridge at Lägerdorf, NW Germany: Inferences on synfolding stress field evolution and its impact on fracture connectivity

Storti¹,

Balsamo²,

Cappanera³

et al. 2011

Marine and Petroleum Geology

View full text Add to dashboard Cite

“…The orientation and intensity of fractures are typically related to macrostructures, such as folds, developing during progressive deformation of a sedimentary basin in Cenozoic (Anastasio et al 1997;Storti and Salvini 2001;Bellahsen et al 2006;Tavani et al 2006;Mobasher and Babaie 2008;Amrouch et al 2010;Lacombe et al 2011;Tavani et al 2015). In agreement, in the ZFTB, several sets of folding-related fractures have been recognized (McQuillan 1973(McQuillan , 1974Gholipour 1998;Ahmadhadi et al 2007; Mobasher and Babaie 2008;Lacombe et al 2011).…”

Section: Introductionmentioning

confidence: 99%

Kinematics and surface fracture pattern of the Anaran basement fault zone in NW of the Zagros fold–thrust belt

Joudaki

Saein

Nilfouroushan

2015

Int J Earth Sci (Geol Rundsch)

View full text Add to dashboard Cite

3-D deformation pattern analysis and evolution of the Añisclo anticline, southern Pyrenees

Cited by 66 publications

References 57 publications

Deformation pattern analysis and tectonic implications of a décollement level within the Central Apennines (Italy)

Deformation pattern analysis and tectonic implications of a décollement level within the Central Apennines (Italy)

Sub-seismic scale fracture pattern and in situ permeability data in the chalk atop of the Krempe salt ridge at Lägerdorf, NW Germany: Inferences on synfolding stress field evolution and its impact on fracture connectivity

Kinematics and surface fracture pattern of the Anaran basement fault zone in NW of the Zagros fold–thrust belt

Contact Info

Product

Resources

About