Results 201 to 210 of about 220,882 (295)

Phase Relations and Melting of SiO2 Under Mantle Conditions Determined From Machine Learning Potentials

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract SiO2 is a fundamental component of planetary interiors, yet its high‐pressure melting and phase relations remain uncertain. We develop a machine learning potential with first‐principles accuracy and perform large‐scale two‐phase coexistence simulations to determine the melting curves of stishovite, post‐stishovite, and seifertite up to 160 GPa
Xin Deng, Jie Deng, Michael J. Walter, Yingwei Fei, Jing Yang, R. E. Cohen   +5 more
wiley   +1 more source

Absence of dehydration due to superionic transition at Earth's core-mantle boundary. [PDF]

Sci Adv
He Y, Zhang W, Hu Q, Sun S, Hu J, Liu D, Zhou L, Dai L, Kim DY, Redfern SAT, Liu Y, Li H, Mao HK.   +12 more
europepmc   +1 more source

Crustal Responses to the Destruction of Continental Lithosphere: Insights From Radial Anisotropy of the Tanlu Fault Zone, Eastern China

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract Since the Mesozoic, much of the eastern China lithosphere was removed through thermo‐mechanical erosion and delamination, yet the effects on the overlying crust remain unclear. The Tanlu Fault Zone (TLFZ), the region's largest lithosphere‐scale weakness, offers a natural laboratory to assess crustal responses to lithospheric destruction.
Yuqi Zhu, Zhouchuan Huang, Frederik Tilmann, Kuan‐Yu Ke, Xinglu Wang, Cong Ji   +5 more
wiley   +1 more source

Redox reactions in subducted CaCO₃-Fe-SiO₂ as a potential source of superdeep diamond inclusions. [PDF]

Sci Rep
Guo M, Li X, Mao Z, Li F, Li L, Zhou Q.
europepmc   +1 more source

Mantle transition zone structure beneath the Changbai volcano: Insight into deep slab dehydration and hot upwelling near the 410 km discontinuity

, 2016
You Tian, Hongxiang Zhu, Dapeng Zhao, Cai Liu, Xuan Feng, T. Liu, Jincheng Ma   +6 more
semanticscholar   +1 more source

Magnetic Signature of Oceanic Transform Faults and Their Fracture Zones

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract Oceanic transform faults (TFs) offset mid‐ocean ridges, juxtaposing different‐aged crust and causing fracture zones (FZ) crossing ocean basins. Mounting evidence challenges the consensus that TFs are conservative plate boundaries, instead supporting the existence of extensional tectonics and two phases of magmatism.
Fei Zhou, Ingo Grevemeyer, Jérôme Dyment, Lars H. Ruepke, Christian Hübscher   +4 more
wiley   +1 more source

Necking of the active Turkana Rift Zone and the priming of eastern Africa for continental breakup. [PDF]

Nat Commun
Rowan CM, Kolawole F, Bécel A, Betka P, Rowan J.   +4 more
europepmc   +1 more source

Stress Field and Megathrust Strength in the Western Hellenic Subduction System: Insights From the 2024 Mw 5.9 Strofades Earthquake Sequence, Greece

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract A M5.9 earthquake occurred on 29 March 2024, offshore near the Strofades Islands, in the western Hellenic Subduction System. Here we present high‐precision earthquake locations and focal mechanisms that suggest the rupture of a NNE‐SSW striking, left‐lateral strike‐slip fault.
G. M. Bocchini, D. Essing, I. Nikolopoulou, A. Dielforder, M. P. Roth, A. Serpetsidaki, E. Sokos, C. P. Evangelidis, R. M. Harrington   +8 more
wiley   +1 more source

Rift linkage and inheritance determine collisional mountain belt evolution. [PDF]

Nat Commun
Wolf SG, Huismans RS, Muñoz JA, May DA.
europepmc   +1 more source

Lithosphere thinning induced by slab penetration into a hydrous mantle transition zone

, 2016
Zhensheng Wang, T. Kusky, F. Capitanio
semanticscholar   +1 more source