Merge pull request #6873 from ljhwang/26February

Adds new publications

Author: gassmoeller

doc/manual/citing_aspect.bib

@@ -3364,3 +3364,77 @@ @article{Neuharth2026
   doi = {10.1093/gji/ggaf515},
   url = {http://doi.org/10.1093/gji/ggaf515},
 }
+
+@Article{Lin2026,
+author={Lin, Jian
+and Lin, Wule
+and Zhou, Zhiyuan
+and Zhang, Fan},
+title={Advances in interdisciplinary ocean geoscience and technology},
+journal={Science China Earth Sciences},
+year={2026},
+month={01},
+day={22},
+issn={1869-1897},
+doi={10.1007/s11430-025-1777-x},
+url={https://doi.org/10.1007/s11430-025-1777-x}
+}
+
+@article{10.1093/gji/ggaf515,
+    author = {Neuharth, Derek and Behr, Whitney M and Holt, Adam F},
+    title = {The role of along-strike variations in interface rheology on subduction dynamics: constraints from three-dimensional numerical models},
+    journal = {Geophysical Journal International},
+    volume = {244},
+    number = {3},
+    pages = {ggaf515},
+    year = {2025},
+    month = {12},
+    issn = {1365-246X},
+    doi = {10.1093/gji/ggaf515},
+    url = {https://doi.org/10.1093/gji/ggaf515},
+    eprint = {https://academic.oup.com/gji/article-pdf/244/3/ggaf515/65912698/ggaf515.pdf},
+}
+
+@article{https://doi.org/10.1029/2025GL118597,
+author = {Wang, Yuan and Liu, Zhonglan},
+title = {Lithospheric Mantle Heterogeneity Drives Delayed Magmatism and Wide Continent-Ocean Transitions in Rifted Margins},
+journal = {Geophysical Research Letters},
+volume = {53},
+number = {4},
+pages = {e2025GL118597},
+keywords = {rifted margins, numerical modeling, magmatism},
+doi = {10.1029/2025GL118597},
+url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2025GL118597},
+eprint = {https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2025GL118597},
+note = {e2025GL118597 2025GL118597},
+year = {2026}
+}
+
+@article{https://doi.org/10.1029/2025JB032000,
+author = {Zhang, Xiulei and Chen, Bo and Pysklywec, Russell N. and Şengül Uluocak, Ebru and Liu, Jianxin},
+title = {Small- and Medium-Wavelength Dynamic Topography and Active Mantle Flow in Eastern China},
+journal = {Journal of Geophysical Research: Solid Earth},
+volume = {131},
+number = {2},
+pages = {e2025JB032000},
+keywords = {Eastern China, mantle flow, residual topography, dynamic topography},
+doi = {10.1029/2025JB032000},
+url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2025JB032000},
+eprint = {https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2025JB032000},
+note = {e2025JB032000 2025JB032000},
+year = {2026}
+}
+
+@article{https://doi.org/10.1029/2025JB033048,
+author = {Koptev, Alexander and Lavecchia, Alessio and Cloetingh, Sierd and Pons, Michaël and Marzotto, Enrico and Brune, Sascha and Kovács, István and Tesauro, Magdala and Beekman, Fred and Wang, Qin and Sobolev, Stephan V. and Faccenna, Claudio and Jolivet, Laurent},
+title = {Numerical Modeling of Purely Active (Plume-Produced) Continental Rifting and Break-Up},
+journal = {Journal of Geophysical Research: Solid Earth},
+volume = {131},
+number = {2},
+pages = {e2025JB033048},
+doi = {10.1029/2025JB033048},
+url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2025JB033048},
+eprint = {https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2025JB033048},
+note = {e2025JB033048 2025JB033048},abstract = {Abstract In contrast to the traditional mechanism of passive continental rifting (driven by far-field tectonic forces), the active rifting-to-break-up processes (caused by rising mantle plumes) are still poorly understood. However, most episodes of fragmentation of the last supercontinent Pangea were relatively shortly preceded (within ∼10 Myr) by the emplacement of Large Igneous Provinces, indicating that a link between lithospheric ruptures and mantle plumes is very close and frequent. In this study, we present a systematic numerical modeling of purely active continental rifting and break-up, that is, without far-field extension, examining the following parameters: (a) the thermo-rheological structure of the lithosphere, (b) the buoyancy of the thermo-chemical mantle plume anomaly, and (c) the duration of the incoming plume flux. Thermo-mechanical experiments show that a classic active rifting scenario, involving the complete break-up of the lithosphere within less than 10 Myr following the arrival of a mantle plume, is achievable, though only under specific conditions. These include: (a) a continuously fed plume with an elevated thermal and/or compositional density deficit ( \${\Delta }\rho \$ ≤ −30 kg m−3) and (b) a relatively warm overlying continental plate, characterized by an above-average Moho temperature ( \${T}\_{M}\$ = 750°C). Although both prerequisites do not seem entirely unrealistic, their simultaneous occurrence in the Phanerozoic Earth is unlikely. We therefore conclude that for a successful transition to lithospheric break-up, plume-activated continental rifting events in the Mesozoic–Cenozoic time must be accompanied by external tectonic stresses.},
+year = {2026}
+}