[META] adding/fixing a publication (bibtex, citation)

[tjhei]

Do you want to fix or add an entry to https://aspect.geodynamics.org/publications.html ? You are at the right place.

We are tracking the list of publications in form of a .bib file: https://github.com/geodynamics/aspect/blob/master/doc/manual/citing_aspect.bib

To add (or fix) an entry, please create a pull request to make modifications to the file. Alternatively, leave a comment in this issue and we will help with creating the entry for you.

The generation of the html page is documented here: https://github.com/geodynamics/aspect/blob/www/README.md#publication-list

We should regularly check google scholar for updates:

https://scholar.google.com/scholar?cites=15800282755444821039&as_sdt=4005&sciodt=0,6&hl=en https://scholar.google.com/scholar?cites=14219378401242979903&as_sdt=4005&sciodt=0,6&hl=en

[bangerth]

Hi Pedro: first, congratulations for finishing your Master's!

Would you like to write a patch to add the entry yourself? It needs to be added to the file doc/manual/citing_aspect.bib.

[Pedrogea08]

Thank you! I will add the entry to the bibtex file once the work is uploaded to my university repository in the next few weeks weeks, so I can add the URL to the full work.

[tjhei]

TODO:

• [ ] https://se.copernicus.org/articles/13/849/2022/

[Minerallo]

Hi everyone,

is it fine if I leave a comment here for a new publication entry ?
thank you in advance for your help !

@article{https://doi.org/10.1029/2023TC007765, author = {Pons, Michaël and Rodriguez Piceda, Constanza and Sobolev, Stephan V. and Scheck-Wenderoth, Magdalena and Strecker, Manfred R.}, title = {Localization of Deformation in a Non-Collisional Subduction Orogen: The Roles of Dip Geometry and Plate Strength on the Evolution of the Broken Andean Foreland, Sierras Pampeanas, Argentina}, journal = {Tectonics}, volume = {42}, number = {8}, pages = {e2023TC007765}, keywords = {subduction, strain localization, Sierras Pampeanas, flat-slab, Andes, Nazca plate}, doi = {https://doi.org/10.1029/2023TC007765}, url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2023TC007765}, eprint = {https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2023TC007765}, note = {e2023TC007765 2023TC007765}, abstract = {Abstract The southern Central Andes (SCA, 27°–40°S) exhibit a complex deformation pattern that is influenced by multiple factors, including the present-day dip angle of the subducting oceanic Nazca plate and the influence of inherited heterogeneities in the continental South American plate. This study employs a data-driven geodynamic workflow to assess the role of various forcing factors in determining upper-plate strain localization, both above the flat slab and the steeper segment to the south. These include the dip angle of the Nazca plate, the mechanically weak sedimentary basins, the thickness and composition of the continental crust, the strength of the subduction interface, and the plate velocities. Our modeling results predict two main deformation modes: (a) pure-shear shortening in the broken foreland above the flat-slab segment and eastward propagation of deformation, and (b) simple-shear shortening restricted to the eastern margin of the Andean fold-and-thrust belt above the steep-slab segment. While the convergence velocity and the frictional strength of the subduction interface primarily control the intensity of the deformation, inherited heterogeneities tend to localize deformation, and weak sediments leads to intensified surface deformation. Thicker crust and surface topography also influences strain localization by transferring stress to the eastern orogenic front. Above the flat-slab segment deformation migrates eastward, which is facilitated by enhanced interface coupling. The transition between the steep and sub-horizontal subduction segments is characterized by a diffuse transpressional shear zone, likely controlled by the change in dip geometry of the Nazca plate, and the presence of inherited faults and weak sedimentary basins.}, year = {2023} }

[ljhwang]

Thanks Michael.
I will add it.