Mantle oxidation by sulfur drives the formation of giant gold deposits in subduction zones.

Autor: He DY; Frontiers Science Center for Deep-time Digital Earth, State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China., Qiu KF; Frontiers Science Center for Deep-time Digital Earth, State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China.; Experimental Geosciences Team, Géosciences Environnement Toulouse, Observatoire Midi-Pyrénées, CNRS, Institut de Recherche pour le Développement, Université de Toulouse III Paul Sabatier, Toulouse F-31400, France., Simon AC; Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI 48109., Pokrovski GS; Experimental Geosciences Team, Géosciences Environnement Toulouse, Observatoire Midi-Pyrénées, CNRS, Institut de Recherche pour le Développement, Université de Toulouse III Paul Sabatier, Toulouse F-31400, France., Yu HC; Frontiers Science Center for Deep-time Digital Earth, State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China., Connolly JAD; Department of Earth Sciences, ETH Zurich, Zürich 8092, Switzerland., Li SS; School of Science, China University of Geosciences, Beijing 100083, China., Turner S; Department of Earth and Environmental Sciences, Macquarie University, Sydney, NSW 2109, Australia., Wang QF; Frontiers Science Center for Deep-time Digital Earth, State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China., Yang MF; Frontiers Science Center for Deep-time Digital Earth, State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China., Deng J; Frontiers Science Center for Deep-time Digital Earth, State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China.; Geological Research Institute of Shandong Gold Group Co., Ltd., Jinan 250013, China.

Publikováno v: Proceedings of the National Academy of Sciences of the United States of America [Proc Natl Acad Sci U S A] 2024 Dec 24; Vol. 121 (52), pp. e2404731121. Date of Electronic Publication: 2024 Dec 19.

Author Correction: Geophysical evidence for an enriched molten silicate layer above Mars's core.

Autor: Samuel H; Université Paris Cité, Institut de physique du globe de Paris, CNRS, Paris, France. samuel@ipgp.fr., Drilleau M; Institut Supérieur de l'Aéronautique et de l'Espace ISAE-SUPAERO, Toulouse, France., Rivoldini A; Royal Observatory of Belgium, Brussels, Belgium., Xu Z; Université Paris Cité, Institut de physique du globe de Paris, CNRS, Paris, France., Huang Q; Department of Geophysics, Colorado School of Mines, Golden, CO, USA.; University of Maryland, College Park, MD, USA., Garcia RF; Institut Supérieur de l'Aéronautique et de l'Espace ISAE-SUPAERO, Toulouse, France., Lekić V; University of Maryland, College Park, MD, USA., Irving JCE; School of Earth Sciences, University of Bristol, Bristol, UK., Badro J; Université Paris Cité, Institut de physique du globe de Paris, CNRS, Paris, France., Lognonné PH; Université Paris Cité, Institut de physique du globe de Paris, CNRS, Paris, France., Connolly JAD; ETH Zurich, Zurich, Switzerland., Kawamura T; Université Paris Cité, Institut de physique du globe de Paris, CNRS, Paris, France., Gudkova T; Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia., Banerdt WB; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA.

Publikováno v: Nature [Nature] 2024 Jan; Vol. 625 (7995), pp. E13.

Marsquake Locations and 1-D Seismic Models for Mars From InSight Data.

Autor: Drilleau M; Institut Supérieur de l'Aéronautique et de l'Espace ISAE-SUPAERO Toulouse France., Samuel H; Institut de Physique du Globe de Paris CNRS Université de Paris Paris France., Garcia RF; Institut Supérieur de l'Aéronautique et de l'Espace ISAE-SUPAERO Toulouse France., Rivoldini A; Royal Observatory of Belgium Brussels Belgium., Perrin C; Nantes Université Université d'Angers Le Mans Université CNRS UMR 6112 Laboratoire de Planétologie et Géosciences UAR 3281 Observatoire des Sciences de l'Univers de Nantes Atlantique Nantes France., Michaut C; Université de Lyon Ecole Normale Supérieure de Lyon Université Claude Bernard Lyon 1 CNRS Laboratoire de Géologie de Lyon : Terre Planètes Environnement Villeurbanne France., Wieczorek M; Université Côte d'Azur Observatoire de la Côte d'Azur CNRS Laboratoire Lagrange Nice France., Tauzin B; Université de Lyon Ecole Normale Supérieure de Lyon Université Claude Bernard Lyon 1 CNRS Laboratoire de Géologie de Lyon : Terre Planètes Environnement Villeurbanne France.; Research School of Earth Sciences The Australian National University Canberra ACT Australia., Connolly JAD; Institute of Geophysics ETH Zürich Zürich Switzerland., Meyer P; Institut Supérieur de l'Aéronautique et de l'Espace ISAE-SUPAERO Toulouse France.; Ecole et Observatoire des Sciences de la Terre Université de Strasbourg Strasbourg France., Lognonné P; Institut de Physique du Globe de Paris CNRS Université de Paris Paris France., Banerdt WB; Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA.

Publikováno v: Journal of geophysical research. Planets [J Geophys Res Planets] 2022 Sep; Vol. 127 (9), pp. e2021JE007067. Date of Electronic Publication: 2022 Sep 07.

Juxtaposed slab dehydration, decarbonation and seismotectonic variation beneath the Philippine subduction zone based on 3-D modeling.

Autor: Zhu, Ye^1,2 (AUTHOR), Ji, Yingfeng^1,2 (AUTHOR) yingfengji@itpcas.ac.cn, Zhu, Weiling^1,2 (AUTHOR), Qu, Rui^1,2 (AUTHOR), Faheem, Haris^1,2 (AUTHOR), Xie, Chaodi³ (AUTHOR)

Publikováno v: Scientific Reports. 11/9/2024, p1-14. 14p.

Subducting serpentinites release reduced, not oxidized, aqueous fluids.

Autor: Piccoli F; University of Bern, Institute of Geological Sciences, Balzerstrasse 1+3, 3012, Bern, Switzerland. francesca.piccoli@geo.unibe.ch., Hermann J; University of Bern, Institute of Geological Sciences, Balzerstrasse 1+3, 3012, Bern, Switzerland., Pettke T; University of Bern, Institute of Geological Sciences, Balzerstrasse 1+3, 3012, Bern, Switzerland., Connolly JAD; Department of Earth Science, Swiss Federal Institute of Technology, Zurich, Switzerland., Kempf ED; University of Bern, Institute of Geological Sciences, Balzerstrasse 1+3, 3012, Bern, Switzerland., Vieira Duarte JF; University of Bern, Institute of Geological Sciences, Balzerstrasse 1+3, 3012, Bern, Switzerland.

Publikováno v: Scientific reports [Sci Rep] 2019 Dec 20; Vol. 9 (1), pp. 19573. Date of Electronic Publication: 2019 Dec 20.