Inhaltsbereich
Publications
(Co) Author: Yan, J.
| Paper (ISI journals) [11] |
Paper (further journals) [1] |
Chapter in Book [3] |
Conference Paper [8] |
All [23] |
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(2010): High pressure equation of state studies using methanol-ethanol-water and argon as pressure media. Journal of Physics and Chemistry of Solids, 71, 8, 1059-1064.
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(2010): Formation of scandium carbides and scandium oxycarbide from the elements at high-(P, T) conditions. Journal of Solid State Chemistry, 183, 5, 975-983.
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(2010): Nanosims studies of ∂ 15N and ∂ 13C in nitrides inclusions in coesite from a Tibetan massive cromitite ore. Geochimica et Cosmochimica Acta, 74, 12, Suppl. 1, 680.| EDOC: 15295 |
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(2009): High-pressure highly reduced nitrides and oxides from chromitite of a Tibetan ophiolite. Proceedings of the National Academy of Sciences of the United States of America (PNAS), 106, 46, 19233-19238.
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(2009): High-pressure Raman and x-ray diffraction studies on LaB6. Physical Review B, 80, 17, 172104.
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(2009): The carbon isotope composition of natural SiC (moissanite) from the Earth´s mantle. New discoveries from ophiolites.. Lithos, 113, 3-4, 612-620.
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(2009): Carbon isotope composition of natural SiC (moissanite) from the Earth's mantle: New discoveries from ophiolites. Geochimica et Cosmochimica Acta, 73, 13, Suppl. 1, A1349.| EDOC: 14476 |
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(2008): Boron and Nitrogen in ultrahigh-pressure terrestrial rocks. Geochimica et Cosmochimica Acta, 72, 12, Suppl. 1, A221.| EDOC: 12643 |
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(2008): Electronic phase transition and amorphization in AuIn2 at high pressure. Physical Review B, 78, 9.
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(2007): Diamond- and coesite-bearing chromitites from the Luobusa ophiolite, Tibet. Geology, 35, 10, 875-878.| EDOC: 10257 | 10.1130/G23766A.1 |
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(2001): Melt/mantle interaction and melt evolution in the Sartohay high-Al chromite deposits of the Dalabute ophiolite (NW China). Journal of Asian Earth Sciences, 19, 4, 517-534.
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(1999): Origin of Podiform Chromitites, diamonds and associated mineral assemblage in the Luobusa Ophilite, Tibet. Bulletin of the Chinese Academy of Sciences, 98 p..| EDOC: 1765 |
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(2010): Gravity modelling of the crust and upper mantle for understanding of tectonic processes: A case study for Europe. - In: Wang, X.; Xia, J.; Yan, J.; Xu, Y. (Eds.), Proceedings, Near-Surface Geophysics and Geohazards; Vol. 2, Science Press USA Inc., 748-752.| EDOC: 15333 |
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(2009): Towards Process Models for Disaster Response. - In: Ardagna, D.; Mecella, M.; Yang, J. (Eds.), Business Process Management Workshops, Springer, 254-265.
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(2007): Convergent Plate Boundaries and Collision Zones. - In: Harms, U.; Koeberl, C.; Zoback, M. D. (Eds.), Continental Scientific Drilling. A Decade of Progress, and Challenges for the Future, Springer, 289-335.| EDOC: 9717 |
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(2010): SIMS Analyses of Carbon Isotopes in Moissanite (SiC) from Ophiolites: A Light Carbon Reservoir in the Earth’s Lower Mantle?. 88. Jahrestagung der Deutschen Mineralogischen Gesellschaft - From Dust to Dust - (Münster 2010), 168.| EDOC: 15784 |
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(2010): Diamond and moissanite in ophiolitic mantle rocks and podiform chromitites: A deep carbon source?. AGU 2010 Fall Meeting (San Francisco 2010).| EDOC: 16509 |
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(2009): New geological settings for ultra-high pressure rocks. AGU 2009 Joint Assembly (Toronto, Canada 2009), V04.| EDOC: 13767 |
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(2008): From nanometric inclusions of osbornite (TiN) in terrestrial coesite to mantle convection and storage of nitrogen in Earth's interior. 33rd International Geological Congress (Oslo, Norway 2008).| EDOC: 12012 |
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(2008): Crust-Mantle recycling recorded In Tibetan Ophiolites. Geological Society of America - 2008 Joint Annual Meeting (Houston, USA 2008).| EDOC: 12982 |
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(2007): Unusal mineral assemblage of titanium and boron nitrides in podiform chromitite of Tibet: are they from Earth's deep interior?. Frontiers in Mineral Sciences 2007 (Cambridge, UK 2007), 189.| EDOC: 9937 |
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(2007): Osbornite (TiN) and boron nitride nanoinclusions in coesite from Tibet: a first record of nitrogen in a terrestrial ultrahigh pressure environment. AGU 2007 Fall Meeting (San Francisco 2007).| EDOC: 10553 |
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(2006): Diamond and coesite after former stishovite in Tibet ophiolites: Is that myth or reality?. AGU Fall Meeting (San Francisco, USA 2006).| EDOC: 9428 |