Kinematic reconstruction of active tectonic and halokinetic structures in the 2021 NW Palagruža earthquake area (Central Adriatic)

Carboni, F.; Mirabella, F.; Minelli, G.; Saleh, H.; Porreca, M.; Ercoli, M.; Pauselli, C.; Barchi, M.R.

doi:10.1016/j.jsg.2024.105112

Search citation statements

Order By: Relevance

Paper Sections

Select...

Citation Types

Supporting

Mentioning

Contrasting

Year Published

2024

2025

Publication Types

Select...

Article3

Preprint1

Relationship

Self Cite0

Independent4

Authors

Journals

Cited by 4 publications

References 90 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

Lithological control and structural inheritance on faults growth in multilayer foreland sequences

Thomas,

Livio,

De Marchi

et al. 2024

Journal of Structural Geology

View full text Add to dashboard Cite

Lithological control and structural inheritance on faults growth in multilayer foreland sequences

Thomas,

Livio,

De Marchi

et al. 2024

Journal of Structural Geology

View full text Add to dashboard Cite

High-resolution geological studies of seismogenic structures

Ren,

Zielke,

Shyu

et al. 2025

Journal of Structural Geology

View full text Add to dashboard Cite

Building the Albanides by Deep Underplating

Rossetti,

Fellin,

Ballato

et al. 2024

Tectonics

View full text Add to dashboard Cite

Subduction orogens grow by accretion of slices of continental lithosphere scraped off the downgoing slab. Although seismological and geophysical data now illuminate the deep structure of these orogens, understanding deep crustal underplating dynamics remains challenging. This study focuses on the Albanides, a subduction orogen in the central‐eastern Mediterranean, formed by the accretion of continental material during the eastward subduction of Adria beneath Eurasia. The thickening at depth of the crustal edifice occurred along with the development of a shallow fold‐and‐thrust belt. This process involved the deposition of progressively younger syn‐orogenic deposits as deformation migrated SW‐ward from the Cretaceous to the Miocene. To explore the relationship between deep‐seated structures and surface deformation, we investigate the recent crustal thickening of the Albanides using low‐temperature thermochronology and 3D thermokinematic modeling of a seismically constrained crustal section. Our data reveal a pulse of exhumation during the latest Miocene‐Pliocene, amounting to approximately 3–4 km, which we propose has been driven by a deep‐seated thrust system imaged by receiver function images. These inferences have significant implications for understanding the interactions between deep and shallow crustal processes and their role in shaping the Albanides. Furthermore, they provide insights into the timing and kinematics of subduction‐related orogenic processes and, potentially, on the separation of the Adria plate from Africa.

show abstract

Kinematic reconstruction of active tectonic and halokinetic structures in the 2021 NW Palagruža earthquake area (Central Adriatic)

Cited by 4 publications

References 90 publications

Lithological control and structural inheritance on faults growth in multilayer foreland sequences

Lithological control and structural inheritance on faults growth in multilayer foreland sequences

High-resolution geological studies of seismogenic structures

Building the Albanides by Deep Underplating

Contact Info

Product

Resources

About